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other provinces and regions in Vietnam and other country.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Address\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Headquarters of Can Tho Journal of Medicine and Pharmacy, located Scientific Research and International Cooperation Office: 179 Nguyen Van Cu Street, An Khanh Ward, Ninh Kieu District, Can Tho City, Vietnam.\u003C\u002Fspan>\u003C\u002Fp>","\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Ngày 16\u002F7\u002F2015, Tạp chí Y Dược học Cần Thơ được cấp chỉ số quốc tế: ISSN 2354-1210.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 4\u002F2016, Tạp chí đã được Hội đồng Giáo sư ngành Y đưa vào danh sách các tạp chí khoa học Y học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Năm 2020 Tạp chí Y Dược học Cần Thơ đã được phê duyệt vào danh mục của các Hội đồng Giáo sư ngành Dược học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ ra 12 số\u002Fnăm, 180-200 trang\u002Fsố.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 12\u002F2022 Tạp chí Y Dược học Cần Thơ là thành viên của hệ thống Crossref và từ tháng 01\u002F2023 tạp chí thực hiện bình duyệt online kín 2 chiều nhằm tăng tính minh bạch, tin cậy của các công trình nghiên cứu khoa học và đảm bảo tốt nhất chất lượng khoa học của bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ, mục đích và phạm vi của tạp chí\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ và mục đích hoạt động của tạp chí: xuất bản nhằm mục đích phổ biến kết quả từ các đề tài nghiên cứu khoa học; giao lưu trao đổi khoa học, chia sẻ kinh nghiệm, học tập, đồng thời cập nhật thông tin khoa học mới trong các lĩnh vực y, sinh, dược học trong và ngoài nước.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phạm vi của tạp chí: Tạp chí xuất bản được chia thành 3 chuyên mục: (i) Bài báo nghiên cứu khoa học là kết quả công trình nghiên cứu khoa học có giá trị đã được triển khai nghiên cứu, (ii) Bài tổng quan y, sinh, dược học: phục vụ mục tiêu đào tạo liên tục trong lĩnh vực y, sinh, dược học; nhằm hệ thống hóa những kiến thức kinh điển và hiện đại; (iii) Thông tin cập nhật kiến thức mới về y, sinh, dược học trong nước và trên thế giới.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Chính sách truy cập mở\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ áp dụng chính sách truy cập mở đối với các bài báo đã xuất bản đến với độc giả, nhằm mở rộng cơ hội tiếp cận các kết quả nghiên cứu chất lượng cao và tăng cường trao đổi kiến thức. Tạp chí đăng tải trực tuyến (miễn phí) toàn văn các bài báo được công bố trên website của Tạp chí (https:\u002F\u002Ftapchi.ctump.edu.vn).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đạo đức xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ cam kết tuân thủ đạo đức xuất bản phù hợp với các hướng dẫn và tiêu chuẩn của the Committee on Publication Ethics (COPE), tuân thủ các nguyên tắc của COPE’s Core Practices, Best Practices Guidelines for Journal Editors và Guidelines on Good Publication Practices.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Bản thảo bài báo chỉ được chấp nhận khi được tác giả chịu trách nhiệm chính cam kết các nội dung sau: Các nội dung của bản thảo chưa được đăng tải toàn bộ hoặc một phần ở các tạp chí khác; Tất cả các tác giả đều có đóng góp một cách đáng kể vào quá trình nghiên cứu hoặc chuẩn bị bản thảo và cùng chịu trách nhiệm về các nội dung của bản thảo; Tuân thủ các biện pháp đảm bảo đạo đức nghiên cứu (ví dụ thỏa thuận đồng ý tham gia nghiên cứu).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Cam kết bảo mật\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí cam kết thực hiện và tuân thủ các quy định của luật và các văn bản hướng dẫn liên quan đến bảo mật thông tin cá nhân trên không gian mạng. Các thông tin mà người dùng (tác giả, độc giả, biên tập viên, người phản biện) nhập vào các biểu mẫu trên Hệ thống Quản lý xuất bản trực tuyến của tạp chí chỉ được sử dụng vào các mục đích đã được tuyên bố rõ ràng và sẽ không được cung cấp cho bất kỳ bên thứ ba nào khác, hay dùng vào bất kỳ mục đích nào khác.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phí gửi bài\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng bài: 1.000.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng nhanh: 1.500.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với tác giả là cán bộ viên chức thuộc Trường Đại học Y Dược Cần Thơ thì được hỗ trợ 50% lệ phí gửi đăng bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với sinh viên thực hiện đề tài nghiên cứu khoa học cấp trường được hỗ trợ 100% lệ phí đăng bài ( Tác giả gửi đính kèm “ Quyết định về việc giao tổ chức thực hiện đề tài nghiên cứu khoa học cấp Trường của sinh viên”).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Hình thức nộp lệ phí:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Tiền mặt:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Nộp trực tiếp tại Phòng Tài chính - Kế toán, Trường Đại học Y Dược Cần Thơ, số 179 Nguyễn Văn Cừ, P. An Khánh, Q. Ninh Kiều, thành phố Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Chuyển khoản:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tên Tài khoản: Trường ĐHYD Cần Thơ, Số TK: 0111000115668, tại ngân hàng Vietcombank chi nhánh Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Thời gian: Áp dụng từ ngày 01\u002F02\u002F2023.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">* Phí gửi bài không được hoàn trả khi bài viết bị từ chối hoặc tác giả xin rút bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Quy trình phản biện bài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ thực hiện quy trình phản biện kín hai chiều nghiêm ngặt. Danh tính của những người phản biện không được tiết lộ cho các tác giả và ngược lại. Quy trình thẩm định bài báo đăng gồm các bước sau:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tiếp nhận bản thảo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tác giả liên hệ gửi bản thảo đến Tạp chí qua hệ thống trực tuyến tại website: https:\u002F\u002Ftapchi.ctump.edu.vn. Hướng dẫn về cách đăng ký, gửi bài và chuẩn bị bản thảo được cung cấp trên website của Tạp chí.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sàng lọc sơ bộ\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sau khi Tòa soạn nhận được bài báo của tác giả, Ban Thư ký sẽ tiến hành kiểm tra sơ bộ bài báo (các yêu cầu về nội dung và hình thức). Những bài báo không đúng quy cách hoặc có nội dung không phù hợp hoặc vi phạm bản quyền sẽ bị từ chối (Ban Thư ký thông báo phản hồi đến tác giả trong vòng 1 tuần). Những bài báo đủ điều kiện, được Ban Thư ký tòa soạn chuyển đến Ban Biên tập có cùng chuyên môn với nội dung bài báo để đề xuất người phản biện. Thời gian kể từ khi Ban Biên tập nhận bài báo đến khi đề xuất người phản biện bài báo chậm nhất là 5 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Vòng phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký gửi bài và yêu cầu phản biện đến 02 phản biện độc lập.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Các phản biện gởi nhận xét cho Ban Thư ký. Thời gian từ khi gửi bài cho phản biện đến khi nhận ý kiến của phản biện tối đa là 20 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xử ký kết quả phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Nếu ý kiến đồng ý cho đăng và không cần chỉnh sửa, Ban Thư ký tiếp tục đăng bài theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Nếu ý kiến đồng ý đăng và cần chỉnh sửa, Ban Thư ký sẽ thông tin đến tác giả chỉnh sửa theo yêu cầu của người phản biện. Thời gian chỉnh sửa và gửi lại kéo dài không quá 2 tuần, từ khi tác giả bài báo nhận được thông tin (Quá trình này có thể lặp lại tối đa 2 lần\u002F1 bài báo). Khi có sự thống nhất, đồng ý của người phản biện; bài báo được tiếp tục đăng theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Những bài báo có chất lượng không đạt yêu cầu, cả 2 phản biện không đồng ý cho đăng sẽ bị Tòa soạn từ chối đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký tổng hợp các bản thảo đã được tác giả hoàn thiện sau thẩm định trình Ban Biên tập xem xét, Tổng Biên tập phê duyệt, quyết định bài đăng theo các tiêu chí: sự phù hợp nội dung với tôn chỉ và mục đích, thể loại bài viết (ưu tiên các bài có bài có nghiên cứu chuyên sâu, hàm lượng khoa học cao), đóng góp mới bài báo, bài báo được ưu tiên đăng trong số gần nhất của Tạp chí theo thứ tự: tính thời sự, chất lượng bài báo và thời gian gửi bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Ban Biên tập và Ban Thư ký biên tập bản thảo, chế bản, đọc rà soát lỗi. Thời gian hoàn thành từ 10-15 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Ban Thư ký có trách nhiệm thông báo cho tác giả bài báo (bằng e-mail) về tình hình phê duyệt bài báo, thời gian, số kỳ, tập xuất bản bài báo theo qui định.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">4. 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the concept of “orbital tuning”, a continuous, high-resolution deep-sea chronostratigraphy has been developed spanning the last 300,000 yr. The chronology is developed using a stacked oxygen-isotope stratigraphy and four different orbital tuning approaches, each of which is based upon a different assumption concerning the response of the orbital signal recorded in the data. Each approach yields a separate chronology. The error measured by the standard deviation about the average of these four results (which represents the “best” chronology) has an average magnitude of only 2500 yr. This small value indicates that the chronology produced is insensitive to the specific orbital tuning technique used. Excellent convergence between chronologies developed using each of five different paleoclimatological indicators (from a single core) is also obtained. The resultant chronology is also insensitive to the specific indicator used. The error associated with each tuning approach is estimated independently and propagated through to the average result. The resulting error estimate is independent of that associated with the degree of convergence and has an average magnitude of 3500 yr, in excellent agreement with the 2500-yr estimate. Transfer of the final chronology to the stacked record leads to an estimated error of ±1500 yr. Thus the final chronology has an average error of ±5000 yr.\u003C\u002Fjats:p>",{"EN":775},"Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy",{"VOID":777},"10.1016\u002F0033-5894(87)90046-9","PUBLICATION","2024-09-30T20:53:42.513+00:00","Auto Verify",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400017889\u002Ftype\u002Fjournal_article",[784,804,823,845,862,882],{"id":785,"sortIndex":114,"researcher":26,"roles":786,"affiliations":787,"properties":799},"60316d3f-735a-447d-84cf-37958da3ee9e",[],[788],{"id":789,"sortIndex":36,"affiliation":790,"properties":26},"28566d3a-d849-400c-875b-d7f7013ca1ed",{"id":791,"createTime":792,"updateTime":793,"relativeEntities":794,"slug":795,"properties":796,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"2c8ffaf3-8301-4cb5-83fd-27f0b1c2779e","2023-12-04T03:38:32.998+00:00","2024-09-30T20:53:42.531+00:00",[],"Department-of-Geological-Sciences-Columbia-University-New-York-New-York-10027-USA",{"title":797},{"VI":798},"Department of Geological Sciences, Columbia University, New York, New York 10027 USA",{"openalex":800,"title":802},{"VOID":801},"A5043596819",{"EN":803},"James D Hays",{"id":805,"sortIndex":162,"researcher":26,"roles":806,"affiliations":807,"properties":818},"e2d85644-cee7-493b-b59a-036c04cf89ee",[],[808],{"id":809,"sortIndex":36,"affiliation":810,"properties":26},"28cd6e6f-cae6-42d9-be80-61c0de7c405f",{"id":811,"createTime":812,"updateTime":812,"relativeEntities":813,"slug":814,"properties":815,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"bd8c7dd3-9fdd-4126-b467-8969d622ce7d","2024-09-30T20:53:42.582+00:00",[],"Sub-Department-of-Quaternary-Research-The-Godwin-Laboratory-Free-School-Lane-Cambridge-England-CB2-3RS",{"title":816},{"EN":817},"Sub-Department of Quaternary Research, The Godwin Laboratory, Free School Lane, Cambridge, England CB2 3RS",{"openalex":819,"title":821},{"VOID":820},"A5026246029",{"EN":822},"Nicholas J Shackleton",{"id":824,"sortIndex":59,"researcher":26,"roles":825,"affiliations":826,"properties":838},"fd71e10b-f8f0-4a6b-8fb0-73e43699d687",[],[827],{"id":828,"sortIndex":36,"affiliation":829,"properties":26},"580ead83-df4c-45f2-bc6c-6a1a8c29fc1f",{"id":830,"createTime":831,"updateTime":832,"relativeEntities":833,"slug":834,"properties":835,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"a9967bb5-79f0-4354-8c5d-8ab5d21a7a14","2024-01-05T09:15:04.447+00:00","2024-10-14T19:59:40.271+00:00",[],"Department-of-Geological-Sciences-Brown-University-Providence-Rhode-Island-02912-USA",{"title":836},{"VI":837},"Department of Geological Sciences, Brown University, Providence, Rhode Island 02912 USA",{"openalex":839,"orcid":841,"title":843},{"VOID":840},"A5052168264",{"VOID":842},"https:\u002F\u002Forcid.org\u002F0000-0001-9170-7949",{"EN":844},"John Imbrie",{"id":846,"sortIndex":36,"researcher":26,"roles":847,"affiliations":848,"properties":855},"80b9dcb0-9722-4fe7-888b-6405ccf0cec1",[],[849],{"id":850,"sortIndex":36,"affiliation":851,"properties":26},"8f9c8733-7a13-4956-9d8b-d064fad6acbf",{"id":791,"createTime":792,"updateTime":793,"relativeEntities":852,"slug":795,"properties":853,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":854},{"VI":798},{"openalex":856,"orcid":858,"title":860},{"VOID":857},"A5014022885",{"VOID":859},"https:\u002F\u002Forcid.org\u002F0000-0002-3673-778X",{"EN":861},"Douglas G. 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measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of <2 μm\u002F>10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming periods, eolian dust accumulation was still substantial and, hence, loess deposition can be regarded as a nearly continuous process during the Quaternary period. In this study we compared the Baoji grain-size time series with the SPECMAP marine isotope record with the objective of elucidating the dynamic linkage between changes in global ice volume and the winter monsoon circulation. Both records show good agreement at both time and frequency domains. In particular, the winter monsoon variations are also dominated by a 100,000 yr period over the past 800,000 yr. 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1984, Synoptic-climatic studies of dust fall in China since historical times., 825",{},{"id":26,"text":1201,"url":26,"identifiers":1202},"Denton, 1981, The Arctic ice sheet: An outrageous hypothesis., “The Last Great Ice Sheet”, 440",{},{"id":26,"text":1204,"url":26,"identifiers":1205},"Berger, 1984, Accuracy and frequency stability of the Earth’s orbital elements during the Quaternary., “Milankovitch and Climate”, 3",{},{"id":26,"text":1207,"url":26,"identifiers":1208},"Liu, 1981, The dust fall in Beijing, China on April 18, 1980., 149",{},{"id":26,"text":1210,"url":26,"identifiers":1211},"Tao, 1957, The atmospheric structure over the Asian continent in summer., 234",{},{"id":26,"text":1213,"url":26,"identifiers":1214},"10.1016\u002F0277-3791(93)90024-G",{"doi":1213},{"id":26,"text":1216,"url":26,"identifiers":1217},"Duplessy, 1988, Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation., 343",{},{"id":26,"text":1219,"url":26,"identifiers":1220},"1984, The last interglacial ocean., 123",{},{"id":26,"text":1222,"url":26,"identifiers":1223},"Berger, 1978, Long-term variations of caloric insolation resulting from the Earth’s orbital elements., 139",{},{"id":26,"text":1225,"url":26,"identifiers":1226},"Liu, 1982, A satellite images study on the dust storm at Beijing on April 17-21, 1980., “Quaternary Geology and Environment of China”, 49",{},{"id":26,"text":1228,"url":26,"identifiers":1229},"Shackleton, 1990, An alternative astronomical calibration of the lower Pleistocene time scale based on ODP site 677., 251",{},{"id":26,"text":1231,"url":26,"identifiers":1232},"Kukla, 1987, Loess stratigraphy in central China., 191",{},{"id":26,"text":1234,"url":26,"identifiers":1235},"Berger, 1991, Insolation values for the climate of the last 10 million years., 297",{},{"id":26,"text":1237,"url":26,"identifiers":1238},"Howard, 1984, Comparison of radiolarian and foraminiferal 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Pleistocene evolution: Northern Hemisphere ice sheets and the North Atlantic Ocean., 353",{},{"id":26,"text":1261,"url":26,"identifiers":1262},"Ding, 1994, Towards an orbital time scale for Chinese loess deposits., 39",{},{"id":26,"text":1264,"url":26,"identifiers":1265},"Chen, 1991, “Monsoons over East Asia.”",{},{"id":26,"text":1267,"url":26,"identifiers":1268},"Ruddiman, 1991, Informal reflections on some unsolved problems in orbital-scale climate cycles., “Global Change of the Past”, 357",{},{"id":26,"text":1270,"url":26,"identifiers":1271},"Liu, 1965, “The Loess Deposits in China.”",{},{"id":26,"text":1273,"url":26,"identifiers":1274},"Zhang, 1982, An analysis on dust storms in historical time, 294",{},{"id":26,"text":1276,"url":26,"identifiers":1277},"Chu, 1984, Regional circulation characteristics associated with a cold surge event over East Asia during winter MONEX., 955",{},{"id":26,"text":1279,"url":26,"identifiers":1280},"Imbrie, 1992, On the structure and origin of major glaciation cycles, 1: Linear response to Milankovitch forcing., 701",{},{"id":26,"text":1282,"url":26,"identifiers":1283},"10.1007\u002F978-94-017-4841-4_14",{"doi":1282},{"id":26,"text":1285,"url":26,"identifiers":1286},"1988, Climatic changes of the last 18,000 years: Observations and model simulations., 1043",{},{"id":26,"text":1288,"url":26,"identifiers":1289},"Liu, 1989, The global surface energy system and the geological role of wind stress., 43",{},{"id":26,"text":1291,"url":26,"identifiers":1292},"Thierstein, 1977, Global synchroneity of late Quaternary coccolith datum levels: Validation by oxygen isotope., 400",{},{"id":26,"text":1294,"url":26,"identifiers":1295},"Tauxe, 1992, Pinning down the Brunhes\u002FMatuyama and upper Jaramitlo boundaries: A reconciliation of orbital and isotopic time scales., 561",{},{"id":26,"text":1297,"url":26,"identifiers":1298},"Kukla, 1989, Loess stratigraphy in central China., 203",{},{"id":26,"text":1300,"url":26,"identifiers":1301},"Zhang, 1987, “Climate in China.”",{},{"id":26,"text":1303,"url":26,"identifiers":1304},"Xiao, 1995, Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during the last 130,000 yr., 22",{},{"id":26,"text":1306,"url":26,"identifiers":1307},"Kutzbach, 1985, Simulation of the climate of 18,000 years B.P.: Results for the North American\u002FNorth Atlantic\u002FEuropean sector and comparison with the geologic record of North America., 147",{},{"id":26,"text":1309,"url":26,"identifiers":1310},"Bartholomew, 1980, “The Times Atlas of the World, Comprehensive Edition.”",{},{"id":26,"text":1312,"url":26,"identifiers":1313},"Liu, 1985, “Loess and the Environment.”",{},{"id":26,"text":1315,"url":26,"identifiers":1316},"Hays, 1976, Variations in the earth’s orbit: Pacemaker of the ice age., 1121",{},{"id":26,"text":1318,"url":26,"identifiers":1319},"Trewartha, 1980, “An Introduction to Climate.”",{},{"id":26,"text":1321,"url":26,"identifiers":1322},"Milankovitch, 1941, “Kanon der Erdestrahlung.” Beogard, Koninglich Serbische Akademie., (English translation: “Canon of Insolation and the Ice Age Problem,” by the Israel Program for Scientific Translation and published for the U.S. Department of Commerce and the National Science Foundation.), 157",{},{"id":26,"text":1324,"url":26,"identifiers":1325},"Ding, 1993, Pedostratigraphy of Chinese loess deposits and climatic cycles in the last 2.5 Ma., 73",{},{"id":26,"text":1327,"url":26,"identifiers":1328},"1976, The surface of the ice-age earth., 1131",{},{"id":26,"text":1330,"url":26,"identifiers":1331},"Hays, 1978, A review of the late Quaternary climatic history of the Antarctic seas., “Antarctic Glacial History and World Palaeoenvironments”, 57",{},{"id":26,"text":1333,"url":26,"identifiers":1334},"Rutter, 1990, Baoji-type pedostratigraphic section, Loess Plateau, north-central China., 1",{},{"id":26,"text":1336,"url":26,"identifiers":1337},"Lambeck, 1995, Constraints on the late Weichselian ice sheet over the Barents sea from observations of raised shorelines., 1",{},{"id":26,"text":1339,"url":26,"identifiers":1340},"Trewartha, 1981, “The Earth’s Problem Climate.”",{},{"id":26,"text":1342,"url":26,"identifiers":1343},"Liu, 1966, “Composition and Texture of Loess.”",{},{"id":26,"text":1345,"url":26,"identifiers":1346},"Baksi, 1992, 40Ar\u002F30-Ar dating of the Brunhes-Matuyama geomagnetic reversal., 356",{},{"id":26,"text":1348,"url":26,"identifiers":1349},"An, 1991a, Late Quaternary dust flow on the Chinese Loess Plateau., 125",{},{"id":26,"text":1351,"url":26,"identifiers":1352},"Imbrie, 1984, The orbital theory of Pleistocene climate: Support from a revised chronology of the marine delta 18O record., “Milankovitch and Climate”, 269",{},{"id":26,"text":1354,"url":26,"identifiers":1355},"Ruddiman, 1989b, Late Miocene to Pleistocene evolution of climate in Africa and the low-latitude Atlantic: Overview of Leg 108 results., 463",{},{"id":26,"text":1357,"url":26,"identifiers":1358},"Chang, 1980, Northeasterly cold surges and near- equatorial disturbances over the winter MONEX during December 1974, Part II: Planetary scale aspects., 298",{},{"id":26,"text":1360,"url":26,"identifiers":1361},"Ding, 1992, A coupled environmental system formed at about 2.5 Ma over eastern Asia., 223",{},{"id":26,"text":1363,"url":26,"identifiers":1364},"Stuiver, 1981, History of marine ice sheet in West Antarctica: A working hypothesis., “The Last Great Ice Sheets”, 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history across northern Russia (including Siberia). Boreal forest development in this region commenced by 10,000 yr B.P. Over most of Russia, forest advanced to or near the current arctic coastline between 9000 and 7000 yr B.P. and retreated to its present position by between 4000 and 3000 yr B.P. Forest establishment and retreat was roughly synchronous across most of northern Russia. Treeline advance on the Kola Peninsula, however, appears to have occurred later than in other regions. During the period of maximum forest extension, the mean July temperatures along the northern coastline of Russia may have been 2.5° to 7.0°C warmer than modern. The development of forest and expansion of treeline likely reflects a number of complimentary environmental conditions, including heightened summer insolation, the demise of Eurasian ice sheets, reduced sea-ice cover, greater continentality with eustatically lower sea level, and extreme Arctic penetration of warm North Atlantic waters. The late Holocene retreat of Eurasian treeline coincides with declining summer insolation, cooling arctic waters, and neoglaciation.\u003C\u002Fjats:p>",{"EN":1379},"Holocene Treeline History and Climate Change Across Northern Eurasia",{"VOID":1381},"10.1006\u002Fqres.1999.2123",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400030787\u002Ftype\u002Fjournal_article",[1385,1406,1425,1445,1466,1486,1503,1522,1537,1559,1579,1594,1611,1626],{"id":1386,"sortIndex":36,"researcher":26,"roles":1387,"affiliations":1388,"properties":1399},"8ce83e73-8287-44e7-a582-ffbca098f6b7",[],[1389],{"id":1390,"sortIndex":36,"affiliation":1391,"properties":26},"0eb6c8fd-29bf-4c75-a0b8-179aef014032",{"id":1392,"createTime":1393,"updateTime":1393,"relativeEntities":1394,"slug":1395,"properties":1396,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"128c7c55-a998-49f7-a573-baa3c373e7ee","2024-10-11T04:48:08.763+00:00",[],"Departments-of-Geography-and-Biology-UCLA-Los-Angeles-California-90095-1524",{"title":1397},{"EN":1398},"Departments of Geography and Biology, UCLA, Los Angeles, California, 90095-1524",{"openalex":1400,"orcid":1402,"title":1404},{"VOID":1401},"A5051888588",{"VOID":1403},"https:\u002F\u002Forcid.org\u002F0000-0002-0267-9825",{"EN":1405},"Glen M. 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Edwards",{"id":1446,"sortIndex":50,"researcher":26,"roles":1447,"affiliations":1448,"properties":1459},"fa354b65-bc87-4914-a0d1-82d745054d11",[],[1449],{"id":1450,"sortIndex":36,"affiliation":1451,"properties":26},"7e627f91-bcc5-4ba3-b8ee-0cd60c504cc2",{"id":1452,"createTime":1453,"updateTime":1453,"relativeEntities":1454,"slug":1455,"properties":1456,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"8f2daf24-7c8c-48e7-b858-f0d7765fb578","2024-10-11T04:48:08.860+00:00",[],"Department-of-Earth-and-Environmental-Sciences-University-of-Illinois-at-Chicago-Chicago-Illinois-60607-7059",{"title":1457},{"EN":1458},"Department of Earth and Environmental Sciences, University of Illinois at Chicago, Chicago, Illinois, 60607-7059",{"openalex":1460,"orcid":1462,"title":1464},{"VOID":1461},"A5069340527",{"VOID":1463},"https:\u002F\u002Forcid.org\u002F0000-0002-2080-7915",{"EN":1465},"Steven L. 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reef-crest coral \u003Cjats:italic>Acropora palmata\u003C\u002Fjats:italic> from late Pleistocene reefs on Barbados has recorded the same global variations in oxygen isotopes as planktonic and benthonic foraminifera. Although the record of oxygen isotopes in \u003Cjats:italic>Acropora palmata\u003C\u002Fjats:italic> is discontinuous, it offers several advantages over the isotope records from deep-sea sediments: (1) the coral grows at water depths of less than 5 m; (2) the samples are unmixed; (3) specimens may be sampled from various elevations of paleo-sea level; and (4) aragonitic corals are suitable for \u003Cjats:sup>230\u003C\u002Fjats:sup>Th\u002F\u003Cjats:sup>234\u003C\u002Fjats:sup>U and He\u002FU dating techniques. The latter advantage means that direct dating of the marine oxygen isotope record is possible. Oxygen isotope stage 5e corresponds to Barbados III, dated at 125,000 ± 6000 yr BP. Petrographic and geochemical evidence from five boreholes drilled into the south coast of Barbados indicates a major eustatic lowering (greater than 100 m below present sea level) occurred between 180,000 and 125,000 yr BP. The age and isotopic data suggest correlation of this change in sea level to Emiliani's oxygen isotope stage 6. \u003Cjats:italic>Acropora palmata\u003C\u002Fjats:italic> deposited at various elevations of sea level during oxygen isotope stage 6 vary by 0.11 ‰ δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O for each 10 m of change in sea level. We further hypothesize a minimum drop of 2°C in the average temperature occurred during the regressive phase of oxygen isotope stage 6. These data indicate that temperature lowering of surface water near Barbados lagged behind a major glacial buildup during this time period. Using the δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O vs sea level calibration herein derived, we estimate the relative height of sea stands responsible for Barbados coral reef terraces in the time range 80,000 to 220,000 yr BP.\u003C\u002Fjats:p>",{"EN":1804},"The Marine Oxygen Isotope Record in Pleistocene Coral, Barbados, West Indies",{"VOID":1806},"10.1016\u002F0033-5894(78)90100-x",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400029653\u002Ftype\u002Fjournal_article",[1810,1830],{"id":1811,"sortIndex":36,"researcher":26,"roles":1812,"affiliations":1813,"properties":1825},"8a559bdc-42a3-4619-838a-0925195c12cc",[],[1814],{"id":1815,"sortIndex":36,"affiliation":1816,"properties":26},"f84a54de-34be-4193-bf20-fbc1beed2387",{"id":1817,"createTime":1818,"updateTime":1819,"relativeEntities":1820,"slug":1821,"properties":1822,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"776ad9a1-19ef-4d1e-809f-5c27f5e99cda","2024-01-08T23:54:53.564+00:00","2024-10-09T13:24:50.400+00:00",[],"Lamont-Doherty-Geological-Observatory-of-Columbia-University-Palisades-New-York-10964-USA",{"title":1823},{"VI":1824},"Lamont-Doherty Geological Observatory of Columbia University, Palisades, New York 10964, USA",{"openalex":1826,"title":1828},{"VOID":1827},"A5034499424",{"EN":1829},"Richard G. 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Matthews",{"url":26,"publisher":1846,"properties":1868},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":1847,"slug":663,"properties":1848,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":1851,"manageAffiliations":1852,"indexDatabases":1853,"url":26,"thumbnailPath":26,"statistic":26,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"issn":1849,"title":1850},{"VOID":666},{"EN":668},[],[],[1854,1861],{"id":738,"indexDatabase":1855,"url":753,"indexYears":26,"academicFieldIds":1860,"indexDatabaseRanking":26},{"id":740,"createTime":741,"updateTime":742,"relativeEntities":1856,"label":1857,"description":1858,"key":749,"publicationTags":1859,"standard":26},[],{"EN":745,"VI":745},{"VI":747,"EN":748},[751,752],[755,756],{"id":717,"indexDatabase":1862,"url":730,"indexYears":731,"academicFieldIds":1867,"indexDatabaseRanking":736},{"id":719,"createTime":720,"updateTime":721,"relativeEntities":1863,"label":1864,"description":1865,"key":727,"publicationTags":1866,"standard":26},[],{"EN":724,"VI":724},{"EN":724,"VI":726},[729],[733,734,735],{"volume":1869,"pages":1871,"issue":1873},{"VOID":1870},"10",{"VOID":1872},"181-196",{"VOID":1190},380,{"total":1874,"publishYear":26,"statisticByYear":1876},{"2012":116,"2013":298,"2014":116,"2015":52,"2016":59,"2017":114,"2018":111,"2019":234,"2020":59,"2021":158,"2022":135,"2023":115,"2024":114},"1978-09-01",1978,[1880,1883,1886,1889,1892,1895,1897,1900,1903,1906,1909,1912,1915,1918,1921,1924,1927,1930,1933,1936,1939,1942,1945,1948,1951,1954,1957,1960,1963,1965,1968,1971,1974,1977,1980,1983,1986,1989,1992,1995],{"id":26,"text":1881,"url":26,"identifiers":1882},"10.1130\u002FMEM145-p43",{"doi":1881},{"id":26,"text":1884,"url":26,"identifiers":1885},"Fairbanks, 1977, The Geochemistry of Marine Skeletal Carbonate for Use in Paleoenvironmental Reconstructions, Ph.D. Thesis",{},{"id":26,"text":1887,"url":26,"identifiers":1888},"10.1130\u002F0016-7606(1971)82[2011:AEWRTA]2.0.CO;2",{"doi":1887},{"id":26,"text":1890,"url":26,"identifiers":1891},"10.1063\u002F1.1747785",{"doi":1890},{"id":26,"text":1893,"url":26,"identifiers":1894},"Milliman, 1974, Marine Carbonates",{},{"id":26,"text":1004,"url":26,"identifiers":1896},{"doi":1004},{"id":26,"text":1898,"url":26,"identifiers":1899},"10.1016\u002F0016-7037(57)90024-8",{"doi":1898},{"id":26,"text":1901,"url":26,"identifiers":1902},"10.1016\u002F0033-5894(73)90061-6",{"doi":1901},{"id":26,"text":1904,"url":26,"identifiers":1905},"Cross, Mg, Sr and U in Recent and fossil Acropora palmata and Montastrea annularis",{},{"id":26,"text":1907,"url":26,"identifiers":1908},"Imbrie, 1971, A new micropaleonto-logical method for quantitative paleoclimatology: Application to a late Pleistocene Caribbean core, Late Cenozoic Glacial Ages, 71",{},{"id":26,"text":1910,"url":26,"identifiers":1911},"10.1038\u002F268618a0",{"doi":1910},{"id":26,"text":1913,"url":26,"identifiers":1914},"Bé, é et al., 1976, Late Quaternary climatic record in western equatorial Atlantic sediments, Investigation of Late Quaternary Paleoceanography and Paleoclimatology, 165",{},{"id":26,"text":1916,"url":26,"identifiers":1917},"10.1016\u002F0033-5894(73)90060-4",{"doi":1916},{"id":26,"text":1919,"url":26,"identifiers":1920},"10.1086\u002F626504",{"doi":1919},{"id":26,"text":1922,"url":26,"identifiers":1923},"10.1130\u002FMEM145-p147",{"doi":1922},{"id":26,"text":1925,"url":26,"identifiers":1926},"10.1016\u002F0033-5894(67)90007-5",{"doi":1925},{"id":26,"text":1928,"url":26,"identifiers":1929},"10.1130\u002F0091-7613(1977)5\u003C16:CAOIAD>2.0.CO;2",{"doi":1928},{"id":26,"text":1931,"url":26,"identifiers":1932},"10.1016\u002F0033-5894(73)90051-3",{"doi":1931},{"id":26,"text":1934,"url":26,"identifiers":1935},"10.1029\u002FRG008i001p00169",{"doi":1934},{"id":26,"text":1937,"url":26,"identifiers":1938},"Harrison, 1973, Near-Surface Diagenesis of Subaerially Exposed Pleistocene Carbonates, Barbados, Ph.D. Thesis",{},{"id":26,"text":1940,"url":26,"identifiers":1941},"James, 1971, Late Pleistocene Reef Limestones, Northern Barbados, W.I., Ph.D. Thesis",{},{"id":26,"text":1943,"url":26,"identifiers":1944},"10.1126\u002Fscience.188.4193.1116",{"doi":1943},{"id":26,"text":1946,"url":26,"identifiers":1947},"Bender, 1978, Uranium series dating of the Pleistocene reef tracts of Barbados, West Indies, Geological Society of America Bulletin",{},{"id":26,"text":1949,"url":26,"identifiers":1950},"10.1126\u002Fscience.183.4128.959",{"doi":1949},{"id":26,"text":1952,"url":26,"identifiers":1953},"Goreau, 1973, The ecology of Jamaican coral reefs. II. Geomorphology, zonation and sedimentary phases, Bulletin of Marine Science, 23, 399",{},{"id":26,"text":1955,"url":26,"identifiers":1956},"10.1029\u002FJB073i006p02271",{"doi":1955},{"id":26,"text":1958,"url":26,"identifiers":1959},"10.1029\u002FJC077i003p00463",{"doi":1958},{"id":26,"text":1961,"url":26,"identifiers":1962},"10.1016\u002F0033-5894(75)90024-1",{"doi":1961},{"id":26,"text":965,"url":26,"identifiers":1964},{"doi":965},{"id":26,"text":1966,"url":26,"identifiers":1967},"10.1130\u002F0016-7606(1953)64[1315:RCITS]2.0.CO;2",{"doi":1966},{"id":26,"text":1969,"url":26,"identifiers":1970},"Mesolella, 1968, The Uplifted Reefs of Barbardos: Physical Stratigraphy, Facies Relationships, and Absolute Chronology, Ph.D. Thesis",{},{"id":26,"text":1972,"url":26,"identifiers":1973},"10.1038\u002F215015a0",{"doi":1972},{"id":26,"text":1975,"url":26,"identifiers":1976},"10.1016\u002F0079-6611(65)90020-0",{"doi":1975},{"id":26,"text":1978,"url":26,"identifiers":1979},"10.1086\u002F627434",{"doi":1978},{"id":26,"text":1981,"url":26,"identifiers":1982},"Savin, 1974, Interpretation of oxygen isotope paleotemperature measurements: effect of the 018\u002F016 ratio of sea water, depth stratification of foraminifera and selective solution, Colloques Internationaux du C.N.R.S., 219, 183",{},{"id":26,"text":1984,"url":26,"identifiers":1985},"10.1126\u002Fscience.168.3933.822",{"doi":1984},{"id":26,"text":1987,"url":26,"identifiers":1988},"10.1126\u002Fscience.178.4059.398",{"doi":1987},{"id":26,"text":1990,"url":26,"identifiers":1991},"Fairbanks, 1976, Oxygen isotope record in Pleistocene coral skeletons, Barbados, W. I., Geological Society of America 89th Ann. Meeting. Abstr., 8, 859",{},{"id":26,"text":1993,"url":26,"identifiers":1994},"Matthews, 1974, A process approach to diagenesis of reefs and reef-associated limestones, Society of Economic Paleontologists and Mineralogists Special Publication, 18, 234",{},{"id":26,"text":1996,"url":26,"identifiers":1997},"10.1126\u002Fscience.166.3904.499",{"doi":1996},{"id":1999,"createTime":2000,"updateTime":2000,"relativeEntities":2001,"slug":2002,"properties":2003,"entityType":778,"verifyStatus":25,"verifyTime":2000,"verifyNote":780,"syncStatus":28,"languages":2015,"translateLanguages":26,"viewCount":36,"primaryUrl":2016,"fullTextUrl":26,"authors":2017,"publicationType":903,"publisherRelationship":2107,"citationCount":2136,"citationInfo":2137,"publishDate":2139,"publishYear":2140,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":2141,"isForceReanalyzing":1024},"effbfaa7-c642-4e13-ae43-d1e108133065","2024-10-09T15:22:24.644+00:00",[],"Lake-Levels-and-Sequence-Stratigraphy-of-Lake-Lisan-the-Late-Pleistocene-Precursor-of-the-Dead-Sea",{"mag":2004,"keywords":2006,"openalex":2007,"abstract":2009,"title":2011,"doi":2013},{"VOID":2005},"2165741265",{},{"VOID":2008},"W2165741265",{"EN":2010},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Lake Lisan, the late Pleistocene precursor of the Dead Sea, existed from ∼70,000 to 15,000 yr B.P. It evolved through frequent water-level fluctuations, which reflected the regional hydrological and climatic conditions. We determined the water level of the lake for the time interval ∼55,000–15,000 cal yr B.P. by mapping offshore, nearshore, and fan-delta sediments; by application of sequence stratigraphy methods; and by dating with radiocarbon and U-series methods. During the studied time interval the lake-level fluctuated between ∼340 and 160 m below mean sea level (msl). Between 55,000 and 30,000 cal yr B.P. the lake evolved through short-term fluctuations around 280–290 m below msl, punctuated (at 48,000–43,000 cal yr B.P.) by a drop event to at least 340 m below msl. At ∼27,000 cal yr B.P. the lake began to rise sharply, reaching its maximum elevation of about 164 m below msl between 26,000 and 23,000 cal yr B.P., then it began dropping and reached 300 m below msl at ∼15,000 cal yr B.P. During the Holocene the lake, corresponding to the present Dead Sea, stabilized at ca. 400 m below msl with minor fluctuations. The hypsometric curve of the basin indicates that large changes in lake area are expected at above 403 and 385 m below msl. At these elevations the lake level is buffered. Lake Lisan was always higher than 380 m below msl, indicating a significantly large water contribution to the basin. The long and repetitious periods of stabilization at 280–290 m below msl during Lake Lisan time indicate hydrological control combined with the existence of a physical sill at this elevation. Crossing this sill could not have been achieved without a dramatic increase in the total water input to the lake, as occurred during the fast and intense lake rise from ∼280 to 160 m below msl at ∼27,000 cal yr B.P.\u003C\u002Fjats:p>",{"EN":2012},"Lake Levels and Sequence Stratigraphy of Lake Lisan, the Late Pleistocene Precursor of the Dead Sea",{"VOID":2014},"10.1006\u002Fqres.2001.2284",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400010528\u002Ftype\u002Fjournal_article",[2018,2039,2056,2073,2090],{"id":2019,"sortIndex":114,"researcher":26,"roles":2020,"affiliations":2021,"properties":2032},"56bc8de9-ae5a-4706-8607-bc780fa143b6",[],[2022],{"id":2023,"sortIndex":36,"affiliation":2024,"properties":26},"f5240053-4fbd-497f-9ae1-f682390672fb",{"id":2025,"createTime":2026,"updateTime":2026,"relativeEntities":2027,"slug":2028,"properties":2029,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"51a52b93-0dcb-446b-91b2-f33e2d1dc53c","2024-10-09T15:22:24.653+00:00",[],"The-Institute-of-Earth-Sciences-The-Hebrew-University-of-Jerusalem-Givat-Ram-91904-Israel",{"title":2030},{"EN":2031},"The Institute of Earth Sciences, The Hebrew University of Jerusalem, Givat Ram, 91904, Israel",{"openalex":2033,"orcid":2035,"title":2037},{"VOID":2034},"A5044847857",{"VOID":2036},"https:\u002F\u002Forcid.org\u002F0000-0001-8367-9255",{"EN":2038},"Yehouda Enzel",{"id":2040,"sortIndex":36,"researcher":26,"roles":2041,"affiliations":2042,"properties":2049},"dbe560cf-e314-4c0e-a1d8-bd8b00d846f9",[],[2043],{"id":2044,"sortIndex":36,"affiliation":2045,"properties":26},"13059621-130e-43aa-8afd-0ad7e9c430ce",{"id":2025,"createTime":2026,"updateTime":2026,"relativeEntities":2046,"slug":2028,"properties":2047,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2048},{"EN":2031},{"openalex":2050,"orcid":2052,"title":2054},{"VOID":2051},"A5015028581",{"VOID":2053},"https:\u002F\u002Forcid.org\u002F0000-0003-0172-3553",{"EN":2055},"Y. 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1992, The highest stand of Lake Lisan: ∼150 meter below MSL, Israel Journal of Earth Sciences, 41, 233",{},{"id":26,"text":2146,"url":26,"identifiers":2147},"10.1002\u002F9781444303919.ch9",{"doi":2146},{"id":26,"text":2149,"url":26,"identifiers":2150},"Neev, 1967, The Dead Sea; Depositional processes and environments of evaporites, Israel Geological Survey Bulletin, 41",{},{"id":26,"text":2152,"url":26,"identifiers":2153},"10.1130\u002F0016-7606(1998)110\u003C1318:SPATAO>2.3.CO;2",{"doi":2152},{"id":26,"text":2155,"url":26,"identifiers":2156},"Bartov, 1999, The Geology of the Lisan Formation at the Massada Plain and the Lisan Peninsula",{},{"id":26,"text":2158,"url":26,"identifiers":2159},"10.1016\u002F0016-7037(71)90115-3",{"doi":2158},{"id":26,"text":2161,"url":26,"identifiers":2162},"10.1006\u002Fqres.1999.2096",{"doi":2161},{"id":26,"text":2164,"url":26,"identifiers":2165},"Bowman, 1997, Geomorphology of the Dead Sea western margins, 217",{},{"id":26,"text":2167,"url":26,"identifiers":2168},"Street-Perrott, 1985, Lake-level and climate reconstruction, 291",{},{"id":26,"text":2170,"url":26,"identifiers":2171},"10.1016\u002F0033-5894(92)90039-L",{"doi":2170},{"id":26,"text":2173,"url":26,"identifiers":2174},"10.1016\u002FS1040-6182(00)00070-7",{"doi":2173},{"id":26,"text":2176,"url":26,"identifiers":2177},"10.1016\u002FS0016-7037(97)00191-9",{"doi":2176},{"id":26,"text":2179,"url":26,"identifiers":2180},"10.1029\u002F2000JB900313",{"doi":2179},{"id":26,"text":2182,"url":26,"identifiers":2183},"Wohl, 1995, Data For Paleohydrology., Continental Paleohydrology, 23",{},{"id":26,"text":2185,"url":26,"identifiers":2186},"Schramm, 1997, Uranium series and 14C dating of Lake Lisan (Paleo-Dead Sea) sediments: Implications for 14C time scale calibration and relation to global paleoclimate",{},{"id":26,"text":2188,"url":26,"identifiers":2189},"Posamentier, 1992, Forced regression in a sequence stratigraphic framework: Concepts, examples and exploration significance, Bulletin of American Association of Petroleum Geologists, 76, 1687",{},{"id":26,"text":2191,"url":26,"identifiers":2192},"Sneh, 1979, Late Pleistocene fan-deltas along the Dead Sea Rift, Journal of Sedimentary Petrology, 49, 541",{},{"id":26,"text":2194,"url":26,"identifiers":2195},"10.1016\u002FS0012-821X(99)00279-4",{"doi":2194},{"id":26,"text":2197,"url":26,"identifiers":2198},"Stein, 2000, The Late Pleistocene and Holocene sediments and tectonics of the Dead Sea Basin., Professional field trip guide book, 41",{},{"id":26,"text":2200,"url":26,"identifiers":2201},"Nemec, 1988, What is a fan-delta and how do we recognize it?, 3",{},{"id":26,"text":2203,"url":26,"identifiers":2204},"Begin, 1974, Lake Lisan—The Pleistocene precursor of the Dead Sea, Geological Survey of Israel Bulletin, 63",{},{"id":26,"text":2206,"url":26,"identifiers":2207},"10.1130\u002F0091-7613(1995)023\u003C0695:PEDNMD>2.3.CO;2",{"doi":2206},{"id":26,"text":2209,"url":26,"identifiers":2210},"10.1144\u002Fgsjgs.146.3.0527",{"doi":2209},{"id":26,"text":2212,"url":26,"identifiers":2213},"Kadan, 1997, Evidence for Dead Sea Lake-Level Fluctuations and Recent Tectonism from the Holocene Fan-Delta of Nahal Darga, Israel",{},{"id":26,"text":2215,"url":26,"identifiers":2216},"Waldman, 2000, Limnological changes in Lake Samra from geochemical and mineralogical evidence of the sedimentary section of Peratzim Valley, 126",{},{"id":26,"text":2218,"url":26,"identifiers":2219},"Klein, 1984, Morphological evidence of lake-level changes, western shore of the Dead Sea, Israel Journal of Earth Sciences, 31, 67",{},{"id":26,"text":2221,"url":26,"identifiers":2222},"Nemec, 1984, Alluvial and coastal conglomerates: Their significant features and comments of gravelly mass-flow deposits, 1",{},{"id":26,"text":2224,"url":26,"identifiers":2225},"Hall, 1997, Topography and bathymetry of the Dead Sea Depression, 11",{},{"id":26,"text":2227,"url":26,"identifiers":2228},"10.1029\u002F95JB01587",{"doi":2227},{"id":26,"text":2230,"url":26,"identifiers":2231},"Ethridge, 1984, Tectonic setting, recognition and hydrocarbon reservoir potential of fan-delta deposits, 217",{},{"id":26,"text":2233,"url":26,"identifiers":2234},"Oviatt, 2000, Lacustrine features and global climate change, 470",{},{"id":26,"text":2236,"url":26,"identifiers":2237},"Ben-David, 1998, Modern and Holocene Debris Flows over the Western Escarpment of the Dead Sea",{},{"id":26,"text":2239,"url":26,"identifiers":2240},"10.1016\u002FS0037-0738(98)00138-9",{"doi":2239},{"id":26,"text":2242,"url":26,"identifiers":2243},"10.1016\u002F0040-1951(81)90143-8",{"doi":2242},{"id":26,"text":2245,"url":26,"identifiers":2246},"Manspeizer, 1985, The Dead Sea Rift: Impact of climate and tectonism on Pleistocene and Holocene sedimentation, 143",{},{"id":2248,"createTime":2249,"updateTime":2249,"relativeEntities":2250,"slug":2251,"properties":2252,"entityType":778,"verifyStatus":25,"verifyTime":2249,"verifyNote":780,"syncStatus":28,"languages":2264,"translateLanguages":26,"viewCount":36,"primaryUrl":2265,"fullTextUrl":26,"authors":2266,"publicationType":903,"publisherRelationship":2311,"citationCount":122,"citationInfo":2340,"publishDate":2342,"publishYear":2343,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":2344,"isForceReanalyzing":1024},"d9c9f5f0-e620-4be2-b8d8-229f083f780c","2024-09-17T21:53:41.273+00:00",[],"Paleoclimatic-Significance-of-the-Mineral-Magnetic-Record-of-the-Chinese-Loess-and-Paleosols",{"mag":2253,"keywords":2255,"openalex":2256,"abstract":2258,"title":2260,"doi":2262},{"VOID":2254},"2037933879",{},{"VOID":2257},"W2037933879",{"EN":2259},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>The origins of the magnetic susceptibility variations of the Chinese loess and paleosols are explored by scanning and transmission electron microscopy of magnetic extracts, and by magnetic modeling of magnetic hysteresis data, to provide quantified estimates of the major magnetic components. Microscopy identifies several distinct size and shape characteristics in the magnetic carriers. Lithogenic magnetites, intact and abraded, dominate the coarse-grained magnetic fraction. The smallest of the coarse grains is ∼ 2 μm. The remaining magnetic materal is ultrafine in size, with two types of magnetite particles present. Type A particles strongly resemble soil magnetites produced by inorganic precipitation. Type B particles, which occur rarely, are probably bacterial in origin. Quantitative modeling of these magnetic assemblages shows that over 90% of the susceptibility variations is accounted for by the superparamagnetic magnetite component. Compared to the loess units, the paleosols are richer in magnetite, particularly of superparamagnetic size, and have a threefold higher ratio of magnetite to hematite. We identify pedogenic formation of magnetite as the major contributor to the loess magnetic record. Matching this record against other paleoclimatic records, we find an extremely high correlation with the standard \u003Cjats:sup>18\u003C\u002Fjats:sup>O record. The Chinese loess sequences record a very high resolution magnetic stratigraphy directly related to changing climate.\u003C\u002Fjats:p>",{"EN":2261},"Paleoclimatic Significance of the Mineral Magnetic Record of the Chinese Loess and Paleosols",{"VOID":2263},"10.1016\u002F0033-5894(92)90079-x",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400023644\u002Ftype\u002Fjournal_article",[2267,2289],{"id":2268,"sortIndex":36,"researcher":26,"roles":2269,"affiliations":2270,"properties":2282},"e66aa530-1483-473b-91e7-7a976ef8b064",[],[2271],{"id":2272,"sortIndex":36,"affiliation":2273,"properties":26},"c4c3817e-0c42-457a-bfd9-2b75c117106e",{"id":2274,"createTime":2275,"updateTime":2276,"relativeEntities":2277,"slug":2278,"properties":2279,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"7d86923d-7d57-4a42-8d20-d6090b9006b2","2023-11-25T19:35:32.331+00:00","2024-12-24T07:14:01.541+00:00",[],"School-of-Environmental-Sciences-University-of-East-Anglia-Norwich-United-Kingdom",{"title":2280},{"VI":2281},"School of Environmental Sciences, University of East Anglia, Norwich, United Kingdom",{"openalex":2283,"orcid":2285,"title":2287},{"VOID":2284},"A5068665443",{"VOID":2286},"https:\u002F\u002Forcid.org\u002F0000-0002-8759-8214",{"EN":2288},"Barbara A. Maher",{"id":2290,"sortIndex":115,"researcher":26,"roles":2291,"affiliations":2292,"properties":2304},"d2a625ba-7829-4762-9820-45fd6b84c187",[],[2293],{"id":2294,"sortIndex":36,"affiliation":2295,"properties":26},"19f7d745-a58a-4363-a25e-f7a9b253d1c0",{"id":2296,"createTime":2297,"updateTime":2298,"relativeEntities":2299,"slug":2300,"properties":2301,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"a3ecc83a-80fd-4274-9558-4fc9bbed0b99","2024-01-05T00:45:04.859+00:00","2024-09-17T21:53:41.308+00:00",[],"Department-of-Geology-and-Geophysics-University-of-Edinburgh-United-Kingdom",{"title":2302},{"VI":2303},"Department of Geology and Geophysics, University of Edinburgh, United Kingdom",{"openalex":2305,"orcid":2307,"title":2309},{"VOID":2306},"A5069821453",{"VOID":2308},"https:\u002F\u002Forcid.org\u002F0000-0003-3877-4370",{"EN":2310},"Roy Thompson",{"url":26,"publisher":2312,"properties":2334},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":2313,"slug":663,"properties":2314,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":2317,"manageAffiliations":2318,"indexDatabases":2319,"url":26,"thumbnailPath":26,"statistic":26,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"issn":2315,"title":2316},{"VOID":666},{"EN":668},[],[],[2320,2327],{"id":738,"indexDatabase":2321,"url":753,"indexYears":26,"academicFieldIds":2326,"indexDatabaseRanking":26},{"id":740,"createTime":741,"updateTime":742,"relativeEntities":2322,"label":2323,"description":2324,"key":749,"publicationTags":2325,"standard":26},[],{"EN":745,"VI":745},{"VI":747,"EN":748},[751,752],[755,756],{"id":717,"indexDatabase":2328,"url":730,"indexYears":731,"academicFieldIds":2333,"indexDatabaseRanking":736},{"id":719,"createTime":720,"updateTime":721,"relativeEntities":2329,"label":2330,"description":2331,"key":727,"publicationTags":2332,"standard":26},[],{"EN":724,"VI":724},{"EN":724,"VI":726},[729],[733,734,735],{"volume":2335,"pages":2337,"issue":2339},{"VOID":2336},"37",{"VOID":2338},"155-170",{"VOID":1190},{"total":122,"publishYear":26,"statisticByYear":2341},{"2012":52,"2013":53,"2014":116,"2015":103,"2016":50,"2017":162,"2018":50,"2019":51,"2020":162,"2021":59,"2022":50,"2023":50,"2024":162},"1992-03-01",1992,[2345,2348,2351,2354,2357,2360,2363,2366,2369,2372,2376,2379,2382,2385,2388,2391,2394,2397,2400,2403,2406,2409,2412,2415,2418,2421,2424,2427,2430,2433,2436,2439,2442,2445],{"id":26,"text":2346,"url":26,"identifiers":2347},"10.1016\u002F0277-3791(87)90004-7",{"doi":2346},{"id":26,"text":2349,"url":26,"identifiers":2350},"10.1080\u002F00018736300101263",{"doi":2349},{"id":26,"text":2352,"url":26,"identifiers":2353},"10.1016\u002F0012-821X(91)90168-H",{"doi":2352},{"id":26,"text":2355,"url":26,"identifiers":2356},"10.1038\u002F300431a0",{"doi":2355},{"id":26,"text":2358,"url":26,"identifiers":2359},"10.1016\u002F0012-821X(82)90141-8",{"doi":2358},{"id":26,"text":2361,"url":26,"identifiers":2362},"10.1016\u002FS0031-9201(86)80013-9",{"doi":2361},{"id":26,"text":2364,"url":26,"identifiers":2365},"10.1130\u002F0091-7613(1988)016\u003C0811:PCICDB>2.3.CO;2",{"doi":2364},{"id":26,"text":2367,"url":26,"identifiers":2368},"10.1038\u002F346737a0",{"doi":2367},{"id":26,"text":2370,"url":26,"identifiers":2371},"10.1130\u002F0091-7613(1991)019\u003C0003:MMROTC>2.3.CO;2",{"doi":2370},{"id":26,"text":2373,"url":26,"identifiers":2374},"Thompson, 1986, Environmental Magnetism, 10.1007\u002F978-94-011-8036-8",{"doi":2375},"10.1007\u002F978-94-011-8036-8",{"id":26,"text":2377,"url":26,"identifiers":2378},"10.1111\u002Fj.1365-246X.1988.tb03429.x",{"doi":2377},{"id":26,"text":2380,"url":26,"identifiers":2381},"Imbrie, 1984, The orbital theory of Pleistocene climate: Support from a revised chronology of the marine delta 18O record, 169",{},{"id":26,"text":2383,"url":26,"identifiers":2384},"10.1130\u002F0091-7613(1990)018\u003C0040:PFOMSV>2.3.CO;2",{"doi":2383},{"id":26,"text":2386,"url":26,"identifiers":2387},"10.1029\u002FGL013i011p01169",{"doi":2386},{"id":26,"text":2389,"url":26,"identifiers":2390},"10.1017\u002FS0370164600032181",{"doi":2389},{"id":26,"text":2392,"url":26,"identifiers":2393},"10.1007\u002FBF00202045",{"doi":2392},{"id":26,"text":2395,"url":26,"identifiers":2396},"10.1038\u002F336368a0",{"doi":2395},{"id":26,"text":2398,"url":26,"identifiers":2399},"10.1016\u002FS0031-9201(86)80006-1",{"doi":2398},{"id":26,"text":2401,"url":26,"identifiers":2402},"10.1038\u002F343161a0",{"doi":2401},{"id":26,"text":2404,"url":26,"identifiers":2405},"10.1038\u002F330252a0",{"doi":2404},{"id":26,"text":2407,"url":26,"identifiers":2408},"Radhakrishnamurty, 1974, Magnetic techniques for ascertaining the nature of iron oxide grains in basalts, Journal of Geophysics, 40, 453",{},{"id":26,"text":2410,"url":26,"identifiers":2411},"10.1029\u002FRG010i001p00213",{"doi":2410},{"id":26,"text":2413,"url":26,"identifiers":2414},"10.1038\u002F263490a0",{"doi":2413},{"id":26,"text":2416,"url":26,"identifiers":2417},"10.1111\u002Fj.1365-246X.1984.tb01928.x",{"doi":2416},{"id":26,"text":2419,"url":26,"identifiers":2420},"10.1029\u002FPA005i002p00109",{"doi":2419},{"id":26,"text":2422,"url":26,"identifiers":2423},"10.1038\u002F256565a0",{"doi":2422},{"id":26,"text":2425,"url":26,"identifiers":2426},"10.1111\u002Fj.1365-246X.1986.tb04522.x",{"doi":2425},{"id":26,"text":2428,"url":26,"identifiers":2429},"10.1038\u002F340296a0",{"doi":2428},{"id":26,"text":2431,"url":26,"identifiers":2432},"10.1180\u002Fclaymin.1987.022.4.05",{"doi":2431},{"id":26,"text":2434,"url":26,"identifiers":2435},"10.1038\u002F299538a0",{"doi":2434},{"id":26,"text":2437,"url":26,"identifiers":2438},"Prell, 1991, One Million Year Record of Summer Monsoon Winds and Continental Aridity from the Owen Ridge (Site 722), Northwest Arabian Sea, 365",{},{"id":26,"text":2440,"url":26,"identifiers":2441},"10.1146\u002Fannurev.mi.36.100182.001245",{"doi":2440},{"id":26,"text":2443,"url":26,"identifiers":2444},"10.1038\u002F342897a0",{"doi":2443},{"id":26,"text":2446,"url":26,"identifiers":2447},"10.1038\u002F320611a0",{"doi":2446},{"id":2449,"createTime":2450,"updateTime":2451,"relativeEntities":2452,"slug":2453,"properties":2454,"entityType":778,"verifyStatus":25,"verifyTime":2465,"verifyNote":780,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"primaryUrl":2466,"fullTextUrl":26,"authors":2467,"publicationType":903,"publisherRelationship":2496,"citationCount":149,"citationInfo":2524,"publishDate":2526,"publishYear":1195,"citationAnalyzeStatus":2527,"lastCitationAnalyze":2528,"indexDatabases":26,"openAccess":26,"references":26,"isForceReanalyzing":1024},"99c0cceb-0c44-4da4-8125-c43c2e8d842d","2024-01-08T08:11:44.290+00:00","2026-06-18T12:43:39.773+00:00",[],"Evidence-of-Active-Dune-Sand-on-the-Great-Plains-in-the-19th-Century-from-Accounts-of-Early-Explorers",{"references":2455,"abstract":2457,"title":2459,"doi":2461,"gsPaper":2463},{"VOID":2456},"Warren, 1856, “Explorations in the Dacota Country, in the Year 1855,”\n10.1130\u002F0091-7613(1994)022\u003C0483:SEODIT>2.3.CO;2\nMaljn, 1946, Dust storms part two, 1861-1880., The Kansas Historical Quarterly, 14, 265\nMorrison, 1969, Photointerpretive mapping from space photographs of Quaternary geomorphic features and soil associations in northern Chihuahua and adjoining New Mexico and Texas., In“Guidebook of the Border Region”, 116\nHitchcock, 1898, Ecological plant geography of Kansas., Transactions of (he Academy of Science of St. Louis, 8, 55\n10.1130\u002F0091-7613(1990)018\u003C0745:SEFLQD>2.3.CO;2\n10.2134\u002Fjeq1993.00472425002200010002x\nSchumm, 1963, “Channel Widening and Flood-Plain Construction Along Cimarron River in Southwestern Kansas,”, 10.3133\u002Fpp352D\nHolliday, 1987, Eolian processes and sediments of the Great Plains., In “Geomorphic Systems of North America”, 195\nWestin, 1971, “Soil Associations of South Dakota,”\nThorp, 1952, “Pleistocene Eolian Deposits of the United States, Alaska, and Parts of Canada.”\nSharps, 1980, “Geologic Map of the Limon 1° x 2° Quadrangle, Colorado and Kansas.”\nHartman, 1992, “Geologic Map of Texas.”\nHolliday, 1985, Holocene soil-geomorphological relations in a semi-arid environment: The Southern High Plains of Texas., In “Soils and Quaternary Landscape Evolution”, 325\n10.1016\u002FS0070-4571(08)70806-9\n10.1130\u002F0091-7613(1992)020\u003C0145:LSSDOT>2.3.CO;2\nCoues, 1895, “The Expeditions of Zebulon Montgomery Pike, Headwaters of the Mississippi River, Through Louisiana Territory and in New Spain, During the Years 1805-6-7.”\n10.1086\u002F624871\nJaco, 1971, “Soil Survey of El Paso County, Texas.”\nSwinehart, 1990, Wind-blown deposits., Jn “An Atlas of the Sand Hills”, 43\nMachenberg, 1984, “Geology of Monahans Sandhills State Park, Texas.”\nMichler, 1850, In “Reports of the Secretary of War, with Reconnaissances of Routes from San Antonio to El Paso,”, 30\nLancaster, 1988, Development of linear dunes in the southwestern Kalahari, southern Africa., Journal of Arid Environments, 14, 233, 10.1016\u002FS0140-1963(18)31070-X\nFremont, 1845, “Report of the Exploring Expedition to the Rocky Mountains in the Year 1842 and to Oregon and North California in the Years 1843-44,”\nHadley, 1987, Fluvial processes and river atftustments on the Great Plains, In “Geomorphic Systems of North America”, 182\nScott, 1968, “Geologic and Structure Contour Map of the La Junta Quadrangle, Colorado and Kansas.”\nBerg, 1969, Geology of Sierra de Samalayuca, Chihuahua, Mexico., In “Guidebook of the Border Region”, 176\nScott, 1975, “Historic Trail Maps of the Pueblo 1° x V Quadrangle, Colorado.”\nEschner, 1983, “Hydrologic and Morphologic Changes in Channels of the Platte River Basin in Colorado, Wyoming, and Nebraska: A Historical Perspective,”, A1\nGilbert, 1896, “The Underground Water of the Arkansas Valley in Eastern Colorado,”, 551\nHall, 1857, Palaeontology and geology of the boundary., In “Report on the United States and Mexican Boundary Survey”\nKuzila, 1990, “General Soil Map of Nebraska.”\n10.1016\u002F0277-3791(95)00005-A\nDiller, 1955, James Mackay’s journey in Nebraska in 1796., Nebraska History Magazine, 36, 123\nDodge, 1877, “The Plains of the Great West and Their Inhabitants being a Description of the Plains, Game, Indians, and c. of the Great North American Desert.”\nNadler, 1981, Metamorphosis of South Platte and Arkansas Rivers, eastern Colorado., Physical Geography, 2, 95, 10.1080\u002F02723646.1981.10642207\nMuhs, 1995b, Origin of the late Quaternary dune fields of northeastern Colorado., Geomorphology,\nThompson, 1993, Climatic changes in the western United States since 18,000 yr B.P., In “Global Climates Since the Last Glacial Maximum”, 468\nMiller, 1990, Land development and use., In “An atlas of the Sand Hills”, 207\nTucker, 1963, Major Long’s route from the Arkansas to the Canadian River, 1820., New Mexico Historical Review, 38, 185\n10.1175\u002F1520-0493(1978)106\u003C0142:TCBTAP>2.0.CO;2\nMeko, 1992, Dendroclimatic evidence from the Great Plains of the United States., In “Climate Since A.D. 1500”, 312\n\nScott, 1978, “Map Showing Geology, Structure, and Oil and Gas Fields in the Sterling 1° x 2° Quadrangle, Colorado, Nebraska, and Kansas.”\n10.1006\u002Fjare.1993.1068\nWeakly, 1962, History of drought in Nebraska., 271\n10.1016\u002F0033-5894(89)90086-0\nRoss, 1991, “Geologic Map of Kansas.”\nLove, 1985, “Geological Map of Wyoming.”\n10.1111\u002Fj.1467-8306.1985.tb00094.x\n10.1007\u002F978-94-009-0067-7_3\nDane, 1965, “Geologic Map of New Mexico.”\nSettle, 1970, “The Journal of Jacob Fowler Edited, with Notes, by Elliott Coues.”\nWilliams, 1978, “The Case of the Shrinking Channels—The North Platte and Platte Rivers in Nebraska,”, 10.3133\u002Fcir781\nJohnson, 1992, Buried soil surfaces beneath the Great Bend Prairie of central Kansas and archaeological implications., Current Research in the Pleistocene, 8, 108\nMarcy, 1850, In “Reports of the Secretary of War, with Reconnaissances of Routes from San Antonio to El Paso,”\nJames, 1823, “Account of an Expedition from Pittsburgh to the Rocky Mountains.”\nKing, 1948, “Geology of the Southern Guadalupe Mountains Texas,”, 10.3133\u002Fpp215\nSharps, 1976, “Geologic Map of the Lamar Quadrangle, Colorado and Kansas.”\nNace, 1965, “Drought of the 1950’s with Special Reference to the Midcontinent,”\nMcKee, 1971, “Growth and movement of dunes at White Sands National Monument, New Mexico,”, 108\nChepil, 1957, Dust Bowl: Causes and effects., Journal of Soil and Water Conservation, 12, 108\nScott, 1989, “Historic Trail Maps of the Sterling 1° x 2° Quadrangle, Northeastern Colorado.”\nPope, 1855, “Report of Exploration of a Route for the Pacific Railroad, Near the Thirty-second Parallel of North Latitude from the Red River to the Rio Grande.”\nSchumm, 1977, “The Fluvial System.”",{"EN":2458},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Eolian sand is extensive over the Great Plains of North America, but is at present mostly stabilized by vegetation. Accounts published by early explorers, however, indicate that at least parts of dune fields in Nebraska, Colorado, Kansas, New Mexico, and Texas were active in the 19th century. Based on an index of dune mobility and a regional tree-ring record, the probable causes for these periods of greater eolian activity are droughts, accompanied by higher temperatures, which greatly lowered the precipitation-to-evapotranspiration ratio and diminished the cover of stabilizing vegetation. In addition, observations by several explorers, and previous historical studies, indicate that rivers upwind of Great Plains dune fields had shallow, braided, sandy channels, as well as intermittent flow in the 19th century. Wide, braided, sandy rivers that were frequently dry would have increased sand supplies to active dune fields. We conclude that dune fields in the Great Plains are extremely sensitive to climate change and that the potential for reactivation of stabilized dunes in the future is high, with or without greenhouse warming.\u003C\u002Fjats:p>",{"EN":2460},"Evidence of Active Dune Sand on the Great Plains in the 19th Century from Accounts of Early Explorers",{"VOID":2462},"10.1006\u002Fqres.1995.1020",{"VOID":2464},"[\"4152324713072217511\"]","2024-05-27T06:57:11.354+00:00","https:\u002F\u002Fwww.sciencedirect.com\u002Fscience\u002Farticle\u002Fpii\u002FS0033589485710204",[2468,2484],{"id":2469,"sortIndex":115,"researcher":26,"roles":2470,"affiliations":2472,"properties":2481},"5baa83ef-3162-4070-8920-e49259141295",[2471],"AUTHOR",[2473],{"id":26,"sortIndex":36,"affiliation":2474,"properties":26},{"id":2475,"createTime":2476,"updateTime":2476,"relativeEntities":2477,"slug":26,"properties":2478,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"186868db-0851-4564-91ba-800dc8ec4d24","2024-01-08T08:11:44.300+00:00",[],{"title":2479},{"VI":2480},"U.S. Geological Survey, MS 974, Box 25046, Federal Center, Denver, Colorado 80225 and Department of Geography, Science Hall, 550 North Park Street, University of Wisconsin, Madison, Wisconsin 53706",{"title":2482},{"VI":2483},"Vance T. Holliday",{"id":2485,"sortIndex":36,"researcher":26,"roles":2486,"affiliations":2487,"properties":2493},"74f52789-699e-4395-adf5-c2657ed72084",[2471],[2488],{"id":26,"sortIndex":36,"affiliation":2489,"properties":26},{"id":2475,"createTime":2476,"updateTime":2476,"relativeEntities":2490,"slug":26,"properties":2491,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2492},{"VI":2480},{"title":2494},{"VI":2495},"Daniel R. Muhs",{"url":2466,"publisher":2497,"properties":2519},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":2498,"slug":663,"properties":2499,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":2502,"manageAffiliations":2503,"indexDatabases":2504,"url":26,"thumbnailPath":26,"statistic":26,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"issn":2500,"title":2501},{"VOID":666},{"EN":668},[],[],[2505,2512],{"id":738,"indexDatabase":2506,"url":753,"indexYears":26,"academicFieldIds":2511,"indexDatabaseRanking":26},{"id":740,"createTime":741,"updateTime":742,"relativeEntities":2507,"label":2508,"description":2509,"key":749,"publicationTags":2510,"standard":26},[],{"EN":745,"VI":745},{"VI":747,"EN":748},[751,752],[755,756],{"id":717,"indexDatabase":2513,"url":730,"indexYears":731,"academicFieldIds":2518,"indexDatabaseRanking":736},{"id":719,"createTime":720,"updateTime":721,"relativeEntities":2514,"label":2515,"description":2516,"key":727,"publicationTags":2517,"standard":26},[],{"EN":724,"VI":724},{"EN":724,"VI":726},[729],[733,734,735],{"volume":2520,"pages":2522},{"VOID":2521},"43",{"VOID":2523},"198-208",{"total":149,"publishYear":1195,"statisticByYear":2525},{"1995":115,"1996":162,"1997":116,"1998":59,"1999":50,"2000":103,"2001":162,"2002":173,"2003":53,"2004":50,"2005":356,"2006":50,"2007":103,"2008":162,"2009":356,"2010":158,"2011":103,"2012":53,"2013":516,"2014":50,"2015":116,"2016":116,"2017":50,"2018":53,"2019":298,"2020":103,"2021":114,"2022":50,"2023":135,"2024":59,"2025":111,"2026":115},"1995-03-01","DONE_ANALYZE_CITATION","2026-06-18T12:43:39.772+00:00",{"id":2530,"createTime":2531,"updateTime":2532,"relativeEntities":2533,"slug":2534,"properties":2535,"entityType":778,"verifyStatus":25,"verifyTime":2544,"verifyNote":780,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"primaryUrl":2545,"fullTextUrl":26,"authors":2546,"publicationType":903,"publisherRelationship":2659,"citationCount":2687,"citationInfo":2688,"publishDate":2691,"publishYear":2689,"citationAnalyzeStatus":28,"lastCitationAnalyze":2532,"indexDatabases":26,"openAccess":26,"references":2692,"isForceReanalyzing":1024},"fa4e3ded-a113-4844-804a-fe312be8de6b","2023-11-25T12:34:14.178+00:00","2026-02-05T20:11:53.088+00:00",[],"Episode-of-Strengthened-Summer-Monsoon-Climate-of-Younger-Dryas-Age-on-the-Loess-Plateau-of-Central-China",{"abstract":2536,"title":2538,"doi":2540,"gsPaper":2542},{"EN":2537},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>The Baxie loess section, just east of the Tibetan Plateau, contains evidence showing that the Asian monsoon climate experienced an abrupt reversal near the end of the last glacial age. Rapid deposition of dust under cool, dry full-glacial conditions gave way to an interval of soil development and reduced dust influx attributed to a strengthening of the warm, moist summer monsoon. A subsequent abrupt increase in dust deposition, a response to a weakening of the summer monsoon, was later followed by renewed soil formation as summer monsoon circulation again intensified during the early Holocene. By one interpretation, the thin upper loess is a manifestation of the European Younger Dryas oscillation; however, in this case the available \u003Cjats:sup>14\u003C\u002Fjats:sup>C ages require either that (1) onset of loess deposition lagged the beginning of the Younger Dryas event in Europe by as much as 2000 calibrated \u003Cjats:sup>14\u003C\u002Fjats:sup>C years or (2) all the \u003Cjats:sup>14\u003C\u002Fjats:sup>C ages are too young, possibly due to contamination. Alternatively, the late-glacial paleosol, the top of which is synchronous with the abrupt end of the late-glacial δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O anomaly in the Dye 3 Greenland ice core, records the Younger Dryas event. Such an interpretation is consistent with general circulation model simulations of Younger Dryas climate that show strong seasonality and a strengthened summer monsoon, and with marine cores from the western Pacific Ocean that contain evidence of pronounced cooling of surface waters during Younger Dryas time.\u003C\u002Fjats:p>",{"EN":2539},"Episode of Strengthened Summer Monsoon Climate of Younger Dryas Age on the Loess Plateau of Central China",{"VOID":2541},"10.1006\u002Fqres.1993.1005",{"VOID":2543},"[\"12473676804436884924\"]","2024-04-30T11:39:40.282+00:00","https:\u002F\u002Fwww.sciencedirect.com\u002Fscience\u002Farticle\u002Fpii\u002FS0033589483710057",[2547,2563,2575,2587,2599,2611,2623,2635,2647],{"id":2548,"sortIndex":114,"researcher":26,"roles":2549,"affiliations":2550,"properties":2560},"e7b92d07-4cde-4da4-bb6b-4c5da07c906b",[2471],[2551],{"id":26,"sortIndex":36,"affiliation":2552,"properties":26},{"id":2553,"createTime":2554,"updateTime":2554,"relativeEntities":2555,"slug":2556,"properties":2557,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"22e8c6f8-0052-4a17-a23c-e9d039432f1b","2023-11-25T12:34:14.284+00:00",[],"Xi-an-Laboratory-of-Loess-and-Quaternary-Geology-Academia-Sinica-Xi-an-710061-People-s-Republic-of-China-Quaternary-Research-Center-University-of-Washington-Seattle-Washington-98195-Department-of-Physics-University-of-Arizona-Tucson-Arizona-85721-and-Radiocarbon-Research-Unit-ANU-Canberra-ACT-2601-Australia",{"title":2558},{"VI":2559},"Xi'an Laboratory of Loess and Quaternary Geology, Academia Sinica, Xi'an 710061, People's Republic of China; Quaternary Research Center, University of Washington, Seattle, Washington 98195; Department of Physics, University of Arizona, Tucson, Arizona 85721; and Radiocarbon Research Unit, ANU, Canberra, ACT 2601, Australia",{"title":2561},{"VI":2562},"Zhou Weijian",{"id":2564,"sortIndex":135,"researcher":26,"roles":2565,"affiliations":2566,"properties":2572},"5066319a-7180-4746-bc4c-04e03688a1e2",[2471],[2567],{"id":26,"sortIndex":36,"affiliation":2568,"properties":26},{"id":2553,"createTime":2554,"updateTime":2554,"relativeEntities":2569,"slug":2556,"properties":2570,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2571},{"VI":2559},{"title":2573},{"VI":2574},"Wu Xihuo",{"id":2576,"sortIndex":158,"researcher":26,"roles":2577,"affiliations":2578,"properties":2584},"84668d13-2c67-45a5-8ef1-9f03e788d81c",[2471],[2579],{"id":26,"sortIndex":36,"affiliation":2580,"properties":26},{"id":2553,"createTime":2554,"updateTime":2554,"relativeEntities":2581,"slug":2556,"properties":2582,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2583},{"VI":2559},{"title":2585},{"VI":2586},"Ren Jianzhang",{"id":2588,"sortIndex":36,"researcher":26,"roles":2589,"affiliations":2590,"properties":2596},"ab9e53eb-afd8-4dca-bfb2-15289446f4e8",[2471],[2591],{"id":26,"sortIndex":36,"affiliation":2592,"properties":26},{"id":2553,"createTime":2554,"updateTime":2554,"relativeEntities":2593,"slug":2556,"properties":2594,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2595},{"VI":2559},{"title":2597},{"VI":2598},"An Zhisheng",{"id":2600,"sortIndex":115,"researcher":26,"roles":2601,"affiliations":2602,"properties":2608},"df7d3dd0-bb61-42b2-a5c0-297b520c6c17",[2471],[2603],{"id":26,"sortIndex":36,"affiliation":2604,"properties":26},{"id":2553,"createTime":2554,"updateTime":2554,"relativeEntities":2605,"slug":2556,"properties":2606,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},[],{"title":2607},{"VI":2559},{"title":2609},{"VI":2610},"Stephen C. 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Donahue",{"url":2545,"publisher":2660,"properties":2682},{"id":659,"createTime":660,"updateTime":661,"relativeEntities":2661,"slug":663,"properties":2662,"entityType":24,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36,"subjectFields":2665,"manageAffiliations":2666,"indexDatabases":2667,"url":26,"thumbnailPath":26,"statistic":26,"gsStatistic":26,"type":26,"analyzePriority":26},[],{"issn":2663,"title":2664},{"VOID":666},{"EN":668},[],[],[2668,2675],{"id":738,"indexDatabase":2669,"url":753,"indexYears":26,"academicFieldIds":2674,"indexDatabaseRanking":26},{"id":740,"createTime":741,"updateTime":742,"relativeEntities":2670,"label":2671,"description":2672,"key":749,"publicationTags":2673,"standard":26},[],{"EN":745,"VI":745},{"VI":747,"EN":748},[751,752],[755,756],{"id":717,"indexDatabase":2676,"url":730,"indexYears":731,"academicFieldIds":2681,"indexDatabaseRanking":736},{"id":719,"createTime":720,"updateTime":721,"relativeEntities":2677,"label":2678,"description":2679,"key":727,"publicationTags":2680,"standard":26},[],{"EN":724,"VI":724},{"EN":724,"VI":726},[729],[733,734,735],{"volume":2683,"pages":2685},{"VOID":2684},"39",{"VOID":2686},"45-54",282,{"total":2687,"publishYear":2689,"statisticByYear":2690},1993,{},"1993-01-01",[2693,2696,2703,2706,2709,2715,2718,2720,2723,2726,2729,2732,2737,2740,2743,2746,2749,2752,2755,2758,2761,2764,2767,2773,2780,2783,2787,2790,2793,2796,2799,2804,2806,2809,2812,2815,2818,2822,2825,2827],{"id":26,"text":2694,"url":26,"identifiers":2695},"10.1038\u002F317130a0",{"doi":2694},{"id":26,"text":2697,"url":2698,"identifiers":2699},"Lu, 1987, Thermoluminescence dating of the Malan loess at Zhaitang, China., Geology, 15, 603, 10.1130\u002F0091-7613(1987)15\u003C603:TDOTML>2.0.CO;2","https:\u002F\u002Fdoi.org\u002F10.1130\u002F0091-7613(1987)15\u003C603:tdotml>2.0.co;2",{"mag":2700,"openalex":2701,"doi":2702},"2068911809","W2068911809","10.1130\u002F0091-7613(1987)15",{"id":26,"text":2704,"url":26,"identifiers":2705},"10.1038\u002F349406a0",{"doi":2704},{"id":26,"text":2707,"url":26,"identifiers":2708},"1981, “Seasonal Reconstructions of the Earth’s Surface at the Last Glacial Maximum.”",{},{"id":2710,"text":2711,"url":2712,"identifiers":2713},"4c68646b-0035-4279-8000-0006b275d4fa","Paterson, 1987, Ice core and other gla-ciological data., 91","https:\u002F\u002Flink.springer.com\u002F10.1007\u002Fs10440-022-00541-7",{"doi":2714},"10.1007\u002Fs10440-022-00541-7",{"id":26,"text":2716,"url":26,"identifiers":2717},"Kelts, 1989, Geological fingerprints of climate history: A cooper-ative study of Qinghai Lake, China., Eclogae Geol. Heiv., 82, 167",{},{"id":26,"text":1312,"url":26,"identifiers":2719},{},{"id":26,"text":2721,"url":26,"identifiers":2722},"10.1017\u002FS0033822200012285",{"doi":2721},{"id":26,"text":2724,"url":26,"identifiers":2725},"Guao, 1962, Regional monsoon climate and subdivision of monsoon area in China., In “Some questions about East Asian Monsoon”, 49",{},{"id":26,"text":2727,"url":26,"identifiers":2728},"An, 1990b, A preliminary study of the paleoenvironmental change of China during the last 20,000 years., In “Loess, Quaternary Geology and Global Change”, 1",{},{"id":26,"text":2730,"url":26,"identifiers":2731},"10.1126\u002Fscience.227.4688.721",{"doi":2730},{"id":2733,"text":2734,"url":2735,"identifiers":2736},"efc38a7c-7e40-4eaf-8df9-c22461d50eb1","10.1016\u002F0031-0182(88)90076-4","https:\u002F\u002Fwww.sciencedirect.com\u002Fscience\u002Farticle\u002Fpii\u002F0031018288900764",{"doi":2734},{"id":2710,"text":2738,"url":2712,"identifiers":2739},"Margart, 1971, Variation in the 13C\u002F12C ratios of plants in relations to the pathway of photosynthetic carbon dioxide fixation., Pho-tochemistry, 10, 1239",{"doi":2714},{"id":26,"text":2741,"url":26,"identifiers":2742},"10.1016\u002F0033-5894(92)90079-X",{"doi":2741},{"id":26,"text":2744,"url":26,"identifiers":2745},"10.1126\u002Fscience.246.4929.474",{"doi":2744},{"id":26,"text":2747,"url":26,"identifiers":2748},"10.1016\u002F0033-5894(91)90015-W",{"doi":2747},{"id":26,"text":2750,"url":26,"identifiers":2751},"10.1029\u002FPA005i001p00077",{"doi":2750},{"id":26,"text":2753,"url":26,"identifiers":2754},"Huang, 1992, The effects of the arctic sea ice on the variations of atmospheric general circulation and climate., Acta Meteorologica Sinica, 6, 1",{},{"id":26,"text":2756,"url":26,"identifiers":2757},"Stuiver, Extended 14C data base and revised CALIB radiocarbon age calibration program., Radiocarbon,",{},{"id":26,"text":2759,"url":26,"identifiers":2760},"10.1038\u002F295313a0",{"doi":2759},{"id":26,"text":2762,"url":26,"identifiers":2763},"10.1016\u002F0031-0182(89)90143-0",{"doi":2762},{"id":26,"text":2765,"url":26,"identifiers":2766},"10.1017\u002FS0033822200007384",{"doi":2765},{"id":2768,"text":2769,"url":2770,"identifiers":2771},"89f56e7c-6630-43a7-98b7-d2174a3861a3","An, 1990a, The long-term paleomonsoon variation re-corded by the loess-paleosol sequence in central China., Quaternary International, 7\u002F8, 91, 10.1016\u002F1040-6182(90)90042-3","https:\u002F\u002Fwww.sciencedirect.com\u002Fscience\u002Farticle\u002Fpii\u002F1040618290900423",{"doi":2772},"10.1016\u002F1040-6182(90)90042-3",{"id":26,"text":2774,"url":2775,"identifiers":2776},"Beijing, 1988, The chronology of the last deglaciation: Implications to the cause of the Younger Dryas event., Paleoceanography, 3, 1, 10.1029\u002FPA003i001p00001","https:\u002F\u002Fdoi.org\u002F10.1029\u002Fpa003i001p00001",{"mag":2777,"openalex":2778,"doi":2779},"2064444973","W2064444973","10.1029\u002Fpa003i001p00001",{"id":26,"text":2781,"url":26,"identifiers":2782},"10.1016\u002F0277-3791(89)90033-4",{"doi":2781},{"id":26,"text":2784,"url":26,"identifiers":2785},"Lu, 1988, Thermoluminescence dating of loess and palaeosols from the Lantian section, Shaanxi Province, China., Quaternary Science Reviews, 7, 245, 10.1016\u002F0277-3791(88)90011-X",{"doi":2786},"10.1016\u002F0277-3791(88)90011-X",{"id":26,"text":2788,"url":26,"identifiers":2789},"Zhang, 1989, Landslide history and late Cenozoic environmental factors in the Sa Le Shan area, Dongxian County, Gansu Province, China., Journal of Lanzhou University, 81",{},{"id":26,"text":2791,"url":26,"identifiers":2792},"Readhead, 1982, Extending thermoluminescence dating to geological sediments., In “Archeaometry: An Australian Perspective”, 276",{},{"id":26,"text":2794,"url":26,"identifiers":2795},"10.1111\u002Fj.1502-3885.1985.tb00896.x",{"doi":2794},{"id":26,"text":2797,"url":26,"identifiers":2798},"10.1038\u002F356757a0",{"doi":2797},{"id":2800,"text":2801,"url":2802,"identifiers":2803},"2c99fc9b-d3a9-41c3-8239-923e91783438","10.1007\u002FBF01277044","https:\u002F\u002Flink.springer.com\u002Farticle\u002F10.1007\u002FBF01277044",{"doi":2801},{"id":26,"text":2364,"url":26,"identifiers":2805},{"doi":2364},{"id":26,"text":2807,"url":26,"identifiers":2808},"10.1038\u002F339532a0",{"doi":2807},{"id":26,"text":2810,"url":26,"identifiers":2811},"10.1029\u002FPA005i006p01025",{"doi":2810},{"id":2710,"text":2813,"url":2712,"identifiers":2814},"Kallel, 1988, Evidence of cooling during the Younger Dryas in the western North Pacific., Oceanologica Acta, 11, 369",{"doi":2714},{"id":26,"text":2816,"url":26,"identifiers":2817},"10.1038\u002F279710a0",{"doi":2816},{"id":2819,"text":2346,"url":2820,"identifiers":2821},"9b221807-8113-4f3f-906a-c36931dc3f1f","https:\u002F\u002Fwww.sciencedirect.com\u002Fscience\u002Farticle\u002Fpii\u002F0277379187900047",{"doi":2346},{"id":26,"text":2823,"url":26,"identifiers":2824},"10.1038\u002F359311a0",{"doi":2823},{"id":26,"text":2826,"url":26,"identifiers":26},"Zhou, 1990, Discussion of the reliability of organisms from paleosols and lacustrine deposits for ",{"id":26,"text":2828,"url":26,"identifiers":26},"                  14C dating., In “Loess, Quaternary Geology and Global Change”, 58",{"id":2830,"createTime":2831,"updateTime":2831,"relativeEntities":2832,"slug":2833,"properties":2834,"entityType":778,"verifyStatus":25,"verifyTime":2831,"verifyNote":780,"syncStatus":28,"languages":2846,"translateLanguages":26,"viewCount":36,"primaryUrl":2847,"fullTextUrl":26,"authors":2848,"publicationType":903,"publisherRelationship":2989,"citationCount":3018,"citationInfo":3019,"publishDate":3021,"publishYear":3022,"citationAnalyzeStatus":28,"lastCitationAnalyze":26,"indexDatabases":26,"openAccess":26,"references":3023,"isForceReanalyzing":1024},"6082900b-de51-4069-b462-6a112634b78d","2024-10-10T23:57:42.244+00:00",[],"A-Record-of-Holocene-Climate-Change-from-Lake-Geochemical-Analyses-in-Southeastern-Arabia",{"mag":2835,"keywords":2837,"openalex":2838,"abstract":2840,"title":2842,"doi":2844},{"VOID":2836},"2001609029",{},{"VOID":2839},"W2001609029",{"EN":2841},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Lacustrine sediments from southeastern Arabia reveal variations in lake level corresponding to changes in the strength and duration of Indian Ocean Monsoon (IOM) summer rainfall and winter cyclonic rainfall. The late glacial\u002FHolocene transition of the region was characterised by the development of mega-linear dunes. These dunes became stabilised and vegetated during the early Holocene and interdunal lakes formed in response to the incursion of the IOM at approximately 8500 cal yr BP with the development of C3 dominated savanna grasslands. The IOM weakened ca. 6000 cal yr BP with the onset of regional aridity, aeolian sedimentation and dune reactivation and accretion. Despite this reduction in precipitation, the lake was maintained by winter dominated rainfall. There was a shift to drier adapted C4 grasslands across the dune field. Lake sediment geochemical analyses record precipitation minima at 8200, 5000 and 4200 cal yr BP that coincide with Bond events in the North Atlantic. A number of these events correspond with changes in cultural periods, suggesting that climate was a key mechanism affecting human occupation and exploitation of this region.\u003C\u002Fjats:p>",{"EN":2843},"A Record of Holocene Climate Change from Lake Geochemical Analyses in Southeastern Arabia",{"VOID":2845},"10.1016\u002Fj.yqres.2006.07.001",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400004634\u002Ftype\u002Fjournal_article",[2849,2870,2892,2909,2931,2946,2968],{"id":2850,"sortIndex":36,"researcher":26,"roles":2851,"affiliations":2852,"properties":2863},"8ce53a0e-6202-4c8c-afc0-c1aa8705d4e3",[],[2853],{"id":2854,"sortIndex":36,"affiliation":2855,"properties":26},"47137b83-894f-4c15-bdec-91e7954bdfcc",{"id":2856,"createTime":2857,"updateTime":2857,"relativeEntities":2858,"slug":2859,"properties":2860,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"1b557aac-e594-46dd-a3cf-b1c20d183b61","2024-10-10T23:57:42.265+00:00",[],"Department-of-Geography-Oxford-Brookes-University-Headington-Oxford-OX3-0BP-UK",{"title":2861},{"EN":2862},"Department of Geography, Oxford Brookes University, Headington, Oxford, OX3 0BP, UK",{"openalex":2864,"orcid":2866,"title":2868},{"VOID":2865},"A5027333066",{"VOID":2867},"https:\u002F\u002Forcid.org\u002F0000-0003-2989-7344",{"EN":2869},"Adrian G. 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We identified ∼850 volcanic signals (700 of these from 110,000 to 9000 yr ago) with sulfate concentrations greater than that associated with historical eruptions from either equatorial or mid-latitude regions that are known to have perturbed global or Northern Hemisphere climate, respectively. This number is a minimum because decreasing sampling resolution with depth, source volcano location, variable circulation patterns at the time of the eruption, and post-depositional modification of the signal can result in an incomplete record. The largest and most abundant volcanic signals over the past 110,000 yr, even after accounting for lower sampling resolution in the earlier part of the record, occur between 17,000 and 6000 yr ago, during and following the last deglaciation. A second period of enhanced volcanism occurs 35,000–22,000 yr ago, leading up to and during the last glacial maximum. These findings further support a possible climate-forcing component in volcanism. Increased volcanism often occurs during stadial\u002Finterstadial transitions within the last glaciation, but this is not consistent over the entire cycle. Ages for some of the largest known eruptions 100,000–9000 yr ago closely correspond to individual sulfate peaks or groups of peaks in our record.\u003C\u002Fjats:p>",{"EN":3238},"A 110,000-Yr Record of Explosive Volcanism from the GISP2 (Greenland) Ice Core",{"VOID":3240},"10.1006\u002Fqres.1996.0013","2024-09-28T07:22:05.081+00:00",[102],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0033589400024637\u002Ftype\u002Fjournal_article",[3245,3265,3280,3295,3310],{"id":3246,"sortIndex":114,"researcher":26,"roles":3247,"affiliations":3248,"properties":3260},"7c8b1931-3745-4891-bccf-8f313509121c",[],[3249],{"id":3250,"sortIndex":36,"affiliation":3251,"properties":26},"800e60c7-e794-438c-8915-b96aae7b5668",{"id":3252,"createTime":3253,"updateTime":3254,"relativeEntities":3255,"slug":3256,"properties":3257,"entityType":98,"verifyStatus":28,"verifyTime":26,"verifyNote":26,"syncStatus":28,"languages":26,"translateLanguages":26,"viewCount":36},"0aecabf7-2295-4015-bd02-4b9a1687e1ec","2024-09-28T07:22:05.101+00:00","2025-06-11T23:49:06.857+00:00",[],"Climate-Change-Research-Center-Institute-for-the-Study-of-Earth-Oceans-and-Space-University-of-New-Hampshire-Durham-New-Hampshire-03824",{"title":3258},{"EN":3259},"Climate Change Research Center, Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham, New Hampshire, 03824",{"openalex":3261,"title":3263},{"VOID":3262},"A5012766175",{"EN":3264},"L. 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