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Journal of Medicine and Pharmacy","Tạp chí Y Dược học Cần Thơ",{"EN":487,"VI":488},"\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">04\u002F10\u002F2015 Ministry of Information and Communications allowed Can Tho journal of medicine and pharmacy to operate (102 \u002FGP-BTTTT)\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">07\u002F16\u002F2015 Can Tho journal of medicine and pharmacy is internationally recognized: ISSN 2354-1210\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">In 2016, The journal has been included in the list of medical science journals by The State Council for professorship which is awarded a work score of 0-0.5 points for a published article.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Can Tho Journal of Medicine and Pharmacy welcome original works that haven’t been submitted or published in other medical journals. Posts must contain content related to one of the journal’s categories.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The content published\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The journal is divided into 3 categories:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Scientific research article: are valuable scientific works, which have been researched and accepted.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Overview of medicine, biology and pharmacy: serving the objective of continuing training in the fields of medicine, biology and pharmacy; to systematize classical and modern knowledge.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Update information on new knowledge about medicine, biology, pharmacy in the country and in the world.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Scope\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Publication and introduction of scientific research in the fields:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Medicine (internal medicine, surgery, pediatrics, obstetrics and gynecology, odonto-stomatology, laboratory, oncology, traditional medicine, nursing).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Biology (genetics, biotechnology).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Pharmacology (pharmaceutics, drug quality analysis-control, synthetic pharmaceutical chemistry, biochemistry, pharmacognosy, botany, clinical pharmacy).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- To enhance the quality of undergraduate, postgraduate education, scientifically researching and meet the necessary treatment in hospital.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Introducing the updated domestic and oversea information about science technology to promote scientific research and exchanging technology in local, other universities.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Exchanging pharmaceutical and medical information for social health developing in the Mekong Delta and Vietnam.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The object\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Postgraduate students, student of Can Tho University of Medicine and Pharmacy, scientists from schools, research institutes, hospitals, health centers, pharmaceutical companies of the Mekong Delta; 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. Danh sách bài báo theo số Tạp chí được in ấn và phát hành trong năm định kỳ được công bố chính thức trên website: https:\u002F\u002Ftapchi.ctump.edu.vn\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>",{"VOID":490},"wcQ1uqwAAAAJ","2023-05-30T08:17:21.868+00:00",[],[494],{"id":495,"createTime":28,"updateTime":28,"relativeEntities":496,"slug":28,"properties":497,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":507,"parentIds":508,"statistic":28},"6413896b-eca9-442b-a73f-182a58a0ce40",[],{"title":498,"address":501,"country":504,"abbreviation":505},{"EN":499,"VI":500},"Can Tho University of Medicine and Pharmacy","Trường Đại học Y Dược Cần Thơ",{"EN":502,"VI":503},"No 179, Nguyen Van Cu street, An Khanh ward, Ninh Kieu district, Can Tho city, Vietnam","Số 179, đường Nguyễn Văn Cừ, phường An Khánh, quận Ninh Kiều, thành phố Cần Thơ, Việt Nam",{"VOID":15},{"VOID":506},"ctump","http:\u002F\u002Fwww.ctump.edu.vn\u002F",[],[],"https:\u002F\u002Ftapchi.ctump.edu.vn\u002Findex.php\u002Fctump",{"impactFactor":32,"impactFactorByYear":512,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":514,"totalPublicationByYear":515,"totalCitation":520,"totalCitationByYear":521,"totalCitationPerPublication":108,"totalCitationPerPublicationByYear":523,"hindexLast5Year":45,"hindex":45},{"2022":513,"2023":111,"2024":106},0.01,1556,{"2020":47,"2021":516,"2022":517,"2023":518,"2024":519,"2025":122},57,306,801,358,161,{"2021":146,"2022":280,"2023":522},99,{"2021":524,"2022":318,"2023":104},0.23,{"impactFactor":28,"impactFactorByYear":28,"i10Index":123,"i10IndexLast5Year":123,"totalPublication":526,"totalPublicationByYear":527,"totalCitation":526,"totalCitationByYear":528,"totalCitationPerPublication":40,"totalCitationPerPublicationByYear":531,"hindexLast5Year":49,"hindex":49},476,{"0":205,"2019":123,"2021":139,"2022":459,"2023":451,"2024":357,"2025":49,"2026":48},{"2021":42,"2022":123,"2023":161,"2024":529,"2025":360,"2026":530},136,83,{"2021":105,"2022":513,"2023":532,"2024":127,"2025":533,"2026":534},0.62,25.43,13.83,{"id":536,"createTime":537,"updateTime":382,"relativeEntities":538,"slug":539,"properties":540,"entityType":25,"verifyStatus":26,"verifyTime":28,"verifyNote":28,"languages":552,"translateLanguages":28,"viewCount":133,"subjectFields":553,"manageAffiliations":554,"indexDatabases":555,"url":556,"thumbnailPath":557,"statistic":558,"gsStatistic":594,"type":55,"analyzePriority":28},"6984a56a-db70-403b-9cc4-4013e1ceaffa","2023-05-09T06:47:40.346+00:00",[],"T%E1%BA%A1p%20ch%C3%AD%20Nghi%C3%AAn%20c%E1%BB%A9u%20n%C6%B0%E1%BB%9Bc%20ngo%C3%A0i",{"country":541,"issn":542,"title":544,"introduce":547,"gsId":550},{"VOID":15},{"VOID":543},"25252445",{"EN":545,"VI":546},"VNU Journal of Foreign Studies","Tạp chí Nghiên cứu nước ngoài",{"EN":548,"VI":549},"{\"ops\":[{\"insert\":\"\\n\\nThe \\n\"},{\"attributes\":{\"italic\":true},\"insert\":\"VNU Journal of Science\"},{\"insert\":\"\\n was established in 1985 for the publication of national and international research papers in all fields of natural sciences and technology, social sciences and humanities. 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This is the first benthic δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O stack composed of more than three records to extend beyond 850 ka, and we use its improved signal quality to identify 24 new marine isotope stages in the early Pliocene. We also present a new LR04 age model for the Pliocene‐Pleistocene derived from tuning the δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O stack to a simple ice model based on 21 June insolation at 65°N. Stacked sedimentation rates provide additional age model constraints to prevent overtuning. Despite a conservative tuning strategy, the LR04 benthic stack exhibits significant coherency with insolation in the obliquity band throughout the entire 5.3 Myr and in the precession band for more than half of the record. The LR04 stack contains significantly more variance in benthic δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O than previously published stacks of the late Pleistocene as the result of higher‐resolution records, a better alignment technique, and a greater percentage of records from the Atlantic. Finally, the relative phases of the stack's 41‐ and 23‐kyr components suggest that the precession component of δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O from 2.7–1.6 Ma is primarily a deep‐water temperature signal and that the phase of δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O precession response changed suddenly at 1.6 Ma.\u003C\u002Fjats:p>",{"EN":952,"VI":953},"A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ\u003Csup>18\u003C\u002Fsup>O records","Chuỗi xếp chồng Pliocen–Pleistocen từ 57 bản ghi δ18O sinh vật đáy phân bố toàn cầu",{"VOID":955},"10.1029\u002F2004pa001071","Auto Verify",[31],[30],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2004PA001071",[961,980],{"id":962,"sortIndex":32,"researcher":28,"roles":963,"affiliations":964,"properties":973,"displayName":977,"givenName":28,"familyName":28},"87ff27dd-cc36-4d18-9968-cd450f17902a",[],[965],{"id":966,"sortIndex":32,"affiliation":967,"properties":28},"b0ca18c1-37d5-4524-a216-c12998d0c139",{"id":966,"createTime":28,"updateTime":28,"relativeEntities":968,"slug":28,"properties":969,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":972,"statistic":28},[],{"title":970},{"VI":971},"Department of Geological Sciences, Brown University, Providence, Rhode Island, USA",[],{"orcid":974,"title":976,"openalex":978},{"VOID":975},"https:\u002F\u002Forcid.org\u002F0000-0001-7859-0096",{"EN":977},"L. 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Project, 81, 599",{},{"id":28,"text":1230,"url":28,"identifiers":1231},"10.1029\u002FGM032p0303",{"doi":1230},{"id":28,"text":1233,"url":28,"identifiers":1234},"10.1017\u002FS0263593300020782",{"doi":1233},{"id":28,"text":1236,"url":28,"identifiers":1237},"Shackleton N. J., 1995, Pliocene stable isotope stratigraphy of ODP Site 846, Proc. Ocean Drill. Program Sci. Results, 138, 337",{},{"id":28,"text":1239,"url":28,"identifiers":1240},"Shackleton N. J., 1995, A new late Neogene time scale: Application to Leg 138 sites, Proc. Ocean Drill. Program Sci. Results, 138, 73",{},{"id":28,"text":1242,"url":28,"identifiers":1243},"10.1029\u002F2000PA000513",{"doi":1242},{"id":28,"text":1245,"url":28,"identifiers":1246},"10.1016\u002FS0025-3227(03)00127-0",{"doi":1245},{"id":28,"text":1248,"url":28,"identifiers":1249},"10.1016\u002F0016-7037(93)90416-T",{"doi":1248},{"id":28,"text":1251,"url":28,"identifiers":1252},"10.1016\u002FS0012-821X(02)00923-8",{"doi":1251},{"id":28,"text":1254,"url":28,"identifiers":1255},"Tiedemann R.(1991) Acht Millionen Jahre Klimageschichte von Nordwest Afrika und Paläo‐Ozeanographie des angrenzenden Atlantiks Ber. Rep. 46 190 pp. Geol.‐Paläontol. Inst. und Mus. Christian‐Albrechts‐Univ. Kiel Germany.",{},{"id":28,"text":1257,"url":28,"identifiers":1258},"Tiedemann R., 1997, Deep‐water cicurlation, chemistry, and terrigenous sediment supply in the equatorial Atlantic during the Pliocene, 3.3–2.6 Ma and 5–4.5 Ma, Proc. Ocean Drill. Program Sci. Results, 154, 299",{},{"id":28,"text":1260,"url":28,"identifiers":1261},"10.1029\u002F94PA00208",{"doi":1260},{"id":28,"text":1263,"url":28,"identifiers":1264},"10.1016\u002FS0031-0182(01)00496-5",{"doi":1263},{"id":28,"text":1266,"url":28,"identifiers":1267},"10.1029\u002F1998PA900013",{"doi":1266},{"id":28,"text":1269,"url":28,"identifiers":1270},"10.1038\u002F35089060",{"doi":1269},{"id":28,"text":1272,"url":28,"identifiers":1273},"10.1016\u002F0031-0182(88)90008-9",{"doi":1272},{"id":28,"text":1275,"url":28,"identifiers":1276},"10.1029\u002F1999PA900027",{"doi":1275},{"id":1278,"createTime":1279,"updateTime":1279,"relativeEntities":1280,"slug":1281,"properties":1282,"entityType":895,"verifyStatus":877,"verifyTime":1293,"verifyNote":897,"languages":1294,"translateLanguages":28,"viewCount":32,"primaryUrl":1295,"fullTextUrl":28,"authors":1296,"publicationType":916,"publisherRelationship":1308,"citationCount":1322,"citationInfo":1323,"publishDate":1327,"publishYear":1324,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":1328,"openAccess":28,"references":1329,"isForceReanalyzing":937},"261dafb8-05c2-49c8-aa20-fc6fd91d6cb8","2024-10-07T09:38:37.443+00:00",[],"Glacial-interglacial-CO-sub-2-sub-change-The-Iron-Hypothesis",{"openalex":1283,"mag":1285,"abstract":1287,"title":1289,"doi":1291},{"VOID":1284},"W1993013648",{"VOID":1286},"1993013648",{"EN":1288},"\u003Cjats:p>Several explanations for the 200 to 280 ppm glacial\u002Finterglacial change in atmospheric CO\u003Cjats:sub>2\u003C\u002Fjats:sub> concentrations deal with variations in southern ocean phytoplankton productivity and the related use or nonuse of major plant nutrients. An hypothesis is presented herein in which arguments are made that new productivity in today's southern ocean (7.4 × 10\u003Cjats:sup>13\u003C\u002Fjats:sup>g yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>) is limited by iron deficiency, and hence the phytoplankton are unable to take advantage of the excess surface nitrate\u002Fphosphate that, if used, could result in total southern ocean new production of 2−3 × 10\u003Cjats:sup>15\u003C\u002Fjats:sup> g C yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>. As a consequence of Fe‐limited new productivity, Holocene interglacial CO\u003Cjats:sub>2\u003C\u002Fjats:sub> levels (preindustrial) are as high as they were during the last interglacial (≈ 280 ppm). In contrast, atmospheric dust Fe supplies were 50 times higher during the last glacial maximum (LGM). Because of this Fe enrichment, phytoplankton growth may have been greatly enhanced, larger amounts of upwelled nutrients may have been used, and the resulting stimulation of new productivity may have contributed to the LGM drawdown of atmospheric CO\u003Cjats:sub>2\u003C\u002Fjats:sub> to levels of less than 200 ppm. Background information and arguments in support of this hypothesis are presented.\u003C\u002Fjats:p>",{"EN":1290},"Glacial‐interglacial CO\u003Csub>2\u003C\u002Fsub> change: The Iron Hypothesis",{"VOID":1292},"10.1029\u002Fpa005i001p00001","2024-10-07T09:38:37.442+00:00",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002FPA005i001p00001",[1297],{"id":1298,"sortIndex":32,"researcher":28,"roles":1299,"affiliations":1300,"properties":1301,"displayName":1305,"givenName":28,"familyName":28},"a7345c1a-5a1d-4f6e-a6d8-7839334bbcfe",[],[],{"orcid":1302,"title":1304,"openalex":1306},{"VOID":1303},"https:\u002F\u002Forcid.org\u002F0000-0002-8670-8469",{"EN":1305},"John H. Martin",{"VOID":1307},"A5068402271",{"url":28,"publisher":1309,"properties":1317},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1310,"slug":872,"properties":1311,"entityType":25,"verifyStatus":877,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1314,"manageAffiliations":1315,"indexDatabases":1316,"url":28,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":1312,"title":1313},{"VOID":875},{"VOID":872},[],[],[],{"issue":1318,"pages":1319,"volume":1321},{"VOID":1010},{"VOID":1320},"1-13",{"VOID":928},1904,{"total":1322,"publishYear":1324,"statisticByYear":1325},1990,{"2012":826,"2013":428,"2014":155,"2015":1326,"2016":161,"2017":159,"2018":208,"2019":567,"2020":358,"2021":601,"2022":829,"2023":599,"2024":560},81,"1990-02-01",[],[1330,1333,1336,1339,1342,1345,1348,1351,1354,1357,1360,1363,1366,1369,1372,1375,1378,1381,1384,1387,1390,1393,1396,1399,1402,1405,1408,1411,1414,1417,1420,1423,1426,1429,1432,1435,1438,1441,1444,1447,1450,1453,1456,1459,1462,1465,1468,1471,1474,1478,1481,1484,1487,1490,1493,1496,1499,1502,1505,1508,1511,1514,1517,1520,1523,1526,1529,1532,1535,1538,1541],{"id":28,"text":1331,"url":28,"identifiers":1332},"10.4319\u002Flo.1982.27.5.0789",{"doi":1331},{"id":28,"text":1334,"url":28,"identifiers":1335},"Bainbridge A. E., 1981, CEOSECS Atlantic Expedition: HydrographLc Data, 1972–73",{},{"id":28,"text":1337,"url":28,"identifiers":1338},"10.1038\u002F329408a0",{"doi":1337},{"id":28,"text":1340,"url":28,"identifiers":1341},"10.1029\u002FGM029p0337",{"doi":1340},{"id":28,"text":1343,"url":28,"identifiers":1344},"10.1017\u002FS0033822200009498",{"doi":1343},{"id":28,"text":1346,"url":28,"identifiers":1347},"10.1038\u002F302520a0",{"doi":1346},{"id":28,"text":1349,"url":28,"identifiers":1350},"10.1029\u002FGD015p0049",{"doi":1349},{"id":28,"text":1352,"url":28,"identifiers":1353},"10.1016\u002F0016-7037(86)90175-4",{"doi":1352},{"id":28,"text":1355,"url":28,"identifiers":1356},"10.1038\u002F331055a0",{"doi":1355},{"id":28,"text":1358,"url":28,"identifiers":1359},"10.1007\u002F978-94-009-8514-8_5",{"doi":1358},{"id":28,"text":1361,"url":28,"identifiers":1362},"10.1016\u002F0079-6611(82)90007-6",{"doi":1361},{"id":28,"text":1364,"url":28,"identifiers":1365},"10.1016\u002F0016-7037(82)90110-7",{"doi":1364},{"id":28,"text":1367,"url":28,"identifiers":1368},"10.1029\u002FGB003i003p00215",{"doi":1367},{"id":28,"text":1370,"url":28,"identifiers":1371},"Broecker W. S., 1982, GEOSECS Pacific Expedition: Hydrographie Data, 1973–1974",{},{"id":28,"text":1373,"url":28,"identifiers":1374},"10.1029\u002FJC090iC04p06925",{"doi":1373},{"id":28,"text":1376,"url":28,"identifiers":1377},"10.1016\u002F0198-0149(87)90073-2",{"doi":1376},{"id":28,"text":1379,"url":28,"identifiers":1380},"Cooke D. W., 1982, Antarctic Geoscience, 1017",{},{"id":28,"text":1382,"url":28,"identifiers":1383},"10.1029\u002FPA003i003p00317",{"doi":1382},{"id":28,"text":1385,"url":28,"identifiers":1386},"10.1038\u002F325318a0",{"doi":1385},{"id":28,"text":1388,"url":28,"identifiers":1389},"10.1038\u002F284155a0",{"doi":1388},{"id":28,"text":1391,"url":28,"identifiers":1392},"10.1007\u002F978-94-009-4738-2_19",{"doi":1391},{"id":28,"text":1394,"url":28,"identifiers":1395},"10.1007\u002F978-94-009-4738-2_10",{"doi":1394},{"id":28,"text":1397,"url":28,"identifiers":1398},"El‐Sayed S. Z., 1988, Productivity of the southern ocean: A closer look, Comp. Biochem. Physiol., 9, 489",{},{"id":28,"text":1400,"url":28,"identifiers":1401},"10.1016\u002FB978-0-08-028881-9.50016-9",{"doi":1400},{"id":28,"text":1403,"url":28,"identifiers":1404},"10.1016\u002F0198-0149(81)90015-7",{"doi":1403},{"id":28,"text":1406,"url":28,"identifiers":1407},"10.1029\u002FGM032p0154",{"doi":1406},{"id":28,"text":1409,"url":28,"identifiers":1410},"10.1038\u002F282677a0",{"doi":1409},{"id":28,"text":1412,"url":28,"identifiers":1413},"10.1038\u002F335426a0",{"doi":1412},{"id":28,"text":1415,"url":28,"identifiers":1416},"10.1111\u002Fj.1529-8817.1977.tb02917.x",{"doi":1415},{"id":28,"text":1418,"url":28,"identifiers":1419},"10.1029\u002FAR015p0169",{"doi":1418},{"id":28,"text":1421,"url":28,"identifiers":1422},"Hardy A. C., 1967, Great Waters",{},{"id":28,"text":1424,"url":28,"identifiers":1425},"Hart T. J., 1934, On the phytoplankton of the south‐west Atlantic and the Bellingshausen Sea, 1929–31, Discovery Rep., 1",{},{"id":28,"text":1427,"url":28,"identifiers":1428},"Hart T. J., 1942, Phytoplankton periodicity in Antarctic surface waters, Discovery Rep., 261",{},{"id":28,"text":1430,"url":28,"identifiers":1431},"10.1029\u002FPA003i004p00413",{"doi":1430},{"id":28,"text":1433,"url":28,"identifiers":1434},"10.1029\u002FJD089iD03p04629",{"doi":1433},{"id":28,"text":1436,"url":28,"identifiers":1437},"10.1016\u002F0198-0149(85)90034-2",{"doi":1436},{"id":28,"text":1439,"url":28,"identifiers":1440},"10.1016\u002F0016-7037(87)90004-4",{"doi":1439},{"id":28,"text":1442,"url":28,"identifiers":1443},"10.1038\u002F334418a0",{"doi":1442},{"id":28,"text":1445,"url":28,"identifiers":1446},"Liebig J., 1847, Chemistry in Its Application to Agriculture and Physiology",{},{"id":28,"text":1448,"url":28,"identifiers":1449},"10.1038\u002F316591a0",{"doi":1448},{"id":28,"text":1451,"url":28,"identifiers":1452},"10.3354\u002Fmeps019197",{"doi":1451},{"id":28,"text":1454,"url":28,"identifiers":1455},"10.1038\u002F331341a0",{"doi":1454},{"id":28,"text":1457,"url":28,"identifiers":1458},"10.1016\u002F0198-0149(88)90035-0",{"doi":1457},{"id":28,"text":1460,"url":28,"identifiers":1461},"10.1016\u002F0198-0149(87)90086-0",{"doi":1460},{"id":28,"text":1463,"url":28,"identifiers":1464},"10.1016\u002F0198-0149(89)90144-1",{"doi":1463},{"id":28,"text":1466,"url":28,"identifiers":1467},"Morel F. M. M., 1985, Chemical Processes in Lakes, 251",{},{"id":28,"text":1469,"url":28,"identifiers":1470},"10.1016\u002F0011-7471(66)90602-4",{"doi":1469},{"id":28,"text":1472,"url":28,"identifiers":1473},"10.1016\u002F0198-0149(89)90052-6",{"doi":1472},{"id":28,"text":1475,"url":28,"identifiers":1476},"Neftel A., 1982, Ice core sample measurements give atmospheric C02 content during the past 40,000 years, Nature, 295, 220, 10.1038\u002F295220a0",{"doi":1477},"10.1038\u002F295220a0",{"id":28,"text":1479,"url":28,"identifiers":1480},"10.1016\u002F0198-0149(89)90133-7",{"doi":1479},{"id":28,"text":1482,"url":28,"identifiers":1483},"10.1029\u002FPA003i002p00157",{"doi":1482},{"id":28,"text":1485,"url":28,"identifiers":1486},"10.1038\u002F293391a0",{"doi":1485},{"id":28,"text":1488,"url":28,"identifiers":1489},"10.1016\u002F0004-6981(88)90508-2",{"doi":1488},{"id":28,"text":1491,"url":28,"identifiers":1492},"10.1111\u002Fj.1529-8817.1987.tb02531.x",{"doi":1491},{"id":28,"text":1494,"url":28,"identifiers":1495},"10.1038\u002F308621a0",{"doi":1494},{"id":28,"text":1497,"url":28,"identifiers":1498},"10.1038\u002F272043a0",{"doi":1497},{"id":28,"text":1500,"url":28,"identifiers":1501},"10.1007\u002F978-94-009-3993-6_27",{"doi":1500},{"id":28,"text":1503,"url":28,"identifiers":1504},"10.1029\u002FPA003i003p00361",{"doi":1503},{"id":28,"text":1506,"url":28,"identifiers":1507},"10.1029\u002FJC094iC02p01979",{"doi":1506},{"id":28,"text":1509,"url":28,"identifiers":1510},"10.1038\u002F308624a0",{"doi":1509},{"id":28,"text":1512,"url":28,"identifiers":1513},"10.4319\u002Flo.1972.17.2.0293",{"doi":1512},{"id":28,"text":1515,"url":28,"identifiers":1516},"10.1126\u002Fscience.227.4683.163",{"doi":1515},{"id":28,"text":1518,"url":28,"identifiers":1519},"10.1007\u002F978-3-642-82275-9_10",{"doi":1518},{"id":28,"text":1521,"url":28,"identifiers":1522},"10.1029\u002FGM032p0005",{"doi":1521},{"id":28,"text":1524,"url":28,"identifiers":1525},"10.1021\u002Fes60165a006",{"doi":1524},{"id":28,"text":1527,"url":28,"identifiers":1528},"10.1016\u002F0016-7037(64)90129-2",{"doi":1527},{"id":28,"text":1530,"url":28,"identifiers":1531},"10.1029\u002FGM032p0163",{"doi":1530},{"id":28,"text":1533,"url":28,"identifiers":1534},"10.1038\u002F299145a0",{"doi":1533},{"id":28,"text":1536,"url":28,"identifiers":1537},"10.1016\u002F0198-0149(88)90066-0",{"doi":1536},{"id":28,"text":1539,"url":28,"identifiers":1540},"Weiss R. F., 1983, GEOSECS Indian Ocean Expedition: Hydrographie Data, 1977–1978",{},{"id":28,"text":1542,"url":28,"identifiers":1543},"Whitworth T., 1988, The Antarctic Circumpolar Current, Oceanus, 31, 53",{},{"id":1545,"createTime":1546,"updateTime":1546,"relativeEntities":1547,"slug":1548,"properties":1549,"entityType":895,"verifyStatus":877,"verifyTime":1546,"verifyNote":897,"languages":1560,"translateLanguages":28,"viewCount":32,"primaryUrl":1561,"fullTextUrl":28,"authors":1562,"publicationType":916,"publisherRelationship":1655,"citationCount":1670,"citationInfo":1671,"publishDate":1674,"publishYear":1672,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":1675,"openAccess":28,"references":1676,"isForceReanalyzing":937},"45a51dc1-94a5-49c8-ad81-a3b0b58e8092","2024-10-11T15:10:23.765+00:00",[],"Deepwater-source-variations-during-the-last-climatic-cycle-and-their-impact-on-the-global-deepwater-circulation",{"openalex":1550,"mag":1552,"abstract":1554,"title":1556,"doi":1558},{"VOID":1551},"W2090767277",{"VOID":1553},"2090767277",{"EN":1555},"\u003Cjats:p>The degree of similarity of the ∂\u003Cjats:sup>13\u003C\u002Fjats:sup>C records of the planktonic foraminiferal species\u003Cjats:italic>N. pachyderma\u003C\u002Fjats:italic>and of the benthic foraminiferal genus\u003Cjats:italic>Cibicides\u003C\u002Fjats:italic>in the high‐latitude basins of the world ocean is used as an indicator of the presence of deepwater sources during the last climatic cycle. Whereas continuous formation of deep water is recognized in the southern ocean, the Norwegian Sea stopped acting as a sink for surface water during isotope stage 4 and the remainder of the last glaciation. However, deep water formed in the north Atlantic south of the Norwegian Sea during the last climatic cycle as early as isotope substage 5d, and this area was also the only active northern source during stages 4–2. A detailed reconstruction of the geographic distribution of ∂\u003Cjats:sup>13\u003C\u002Fjats:sup>C in benthic foraminifera in the Atlantic Ocean during the last glacial maximum shows that the most important deepwater mass originated from the southern ocean, whereas the Glacial North Atlantic Deep Water cannot be traced south of 40°N. At shallower depth an oxygenated\u003Cjats:sup>13\u003C\u002Fjats:sup>C rich Intermediate Water mass extended from 45°N to 15°S. In the Pacific Ocean a ventilation higher than the modern one was also found in open ocean in the depth range 700–2600 m and is best explained by stronger formation of Intermediate Water in high northern latitudes.\u003C\u002Fjats:p>",{"EN":1557},"Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation",{"VOID":1559},"10.1029\u002Fpa003i003p00343",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002FPA003i003p00343",[1563,1580,1597,1606,1623,1640],{"id":1564,"sortIndex":32,"researcher":28,"roles":1565,"affiliations":1566,"properties":1575,"displayName":1577,"givenName":28,"familyName":28},"4ccd5beb-e111-4dd5-8064-19984c0a0945",[],[1567],{"id":1568,"sortIndex":32,"affiliation":1569,"properties":28},"3b2d0ed6-29b4-419a-9483-d81643e49671",{"id":1568,"createTime":28,"updateTime":28,"relativeEntities":1570,"slug":28,"properties":1571,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1574,"statistic":28},[],{"title":1572},{"EN":1573},"CFR - Centre des Faibles Radioactivités (91190 Gif sur Yvette - France)",[],{"title":1576,"openalex":1578},{"EN":1577},"Jean‐Claude Duplessy",{"VOID":1579},"A5008755241",{"id":1581,"sortIndex":40,"researcher":28,"roles":1582,"affiliations":1583,"properties":1592,"displayName":1594,"givenName":28,"familyName":28},"5952c37c-1109-4cb9-bed5-b26a7f41c797",[],[1584],{"id":1585,"sortIndex":32,"affiliation":1586,"properties":28},"fe0bd4bd-767e-4b26-b288-e0b955f3b274",{"id":1585,"createTime":28,"updateTime":28,"relativeEntities":1587,"slug":28,"properties":1588,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1591,"statistic":28},[],{"title":1589},{"EN":1590},"Godwin Laboratory (Department of Earth Sciences, University of Cambridge, CB2 3EQ, UK - United Kingdom)",[],{"title":1593,"openalex":1595},{"EN":1594},"Nicholas J Shackleton",{"VOID":1596},"A5026246029",{"id":1598,"sortIndex":123,"researcher":28,"roles":1599,"affiliations":1600,"properties":1601,"displayName":1603,"givenName":28,"familyName":28},"ae507e63-4907-4091-ac39-7b154dac8ab9",[],[],{"title":1602,"openalex":1604},{"EN":1603},"Richard G. 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L., 1965, Intermediate waters of the Pacific Ocean, The Tohns Hopkins Océanographie Studies Number 2",{},{"id":28,"text":1804,"url":28,"identifiers":1805},"10.2307\u002F1485696",{"doi":1804},{"id":28,"text":1807,"url":28,"identifiers":1808},"Sarnthein M., Global variations of surface ocean productivity in low and mid latitudes: Influence on CO2 reservoirs of the deep ocean and atmosphere during the last 21,000 years, Paleoceanography",{},{"id":28,"text":1810,"url":28,"identifiers":1811},"10.1021\u002Fac60214a047",{"doi":1810},{"id":28,"text":1813,"url":28,"identifiers":1814},"10.1007\u002F978-1-4899-5016-1_22",{"doi":1813},{"id":28,"text":1816,"url":28,"identifiers":1817},"10.1016\u002F0012-821X(83)90162-0",{"doi":1816},{"id":28,"text":1819,"url":28,"identifiers":1820},"Streeter S. 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Oppo Lamont Doherty Geological Observatory Palisades N.Y. 10964.",{},{"id":1843,"createTime":1844,"updateTime":1844,"relativeEntities":1845,"slug":1846,"properties":1847,"entityType":895,"verifyStatus":26,"verifyTime":1858,"verifyNote":956,"languages":1859,"translateLanguages":28,"viewCount":32,"primaryUrl":1860,"fullTextUrl":28,"authors":1861,"publicationType":916,"publisherRelationship":1951,"citationCount":1966,"citationInfo":1967,"publishDate":1969,"publishYear":934,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":1970,"openAccess":28,"references":1971,"isForceReanalyzing":937},"e6669ffc-d4b8-4a33-8b2e-12415359f44b","2024-10-10T10:21:38.875+00:00",[],"Astronomic-timescale-for-the-Pliocene-Atlantic-%CE%B4-sup-18-sup-O-and-dust-flux-records-of-Ocean-Drilling-Program-Site-659",{"openalex":1848,"mag":1850,"abstract":1852,"title":1854,"doi":1856},{"VOID":1849},"W2136923855",{"VOID":1851},"2136923855",{"EN":1853},"\u003Cjats:p>High‐resolution benthic oxygen isotope and dust flux records from Ocean Drilling Program site 659 have been analyzed to extend the astronomically calibrated isotope timescale for the Atlantic from 2.85 Ma back to 5 Ma. Spectral analysis of the δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O record indicates that the 41‐kyr period of Earth's orbital obliquity dominates the Pliocene record. This is shown to be true regardless of fundamental changes in the Earth's climate during the Pliocene. However, the cycles of Sahelian aridity fluctuations indicate a shift in spectral character near 3 Ma. From the early Pliocene to 3 Ma, the periodicities were dominantly precessional (19 and 23 kyr) and remained strong until 1.5 Ma. Subsequent to 3 Ma, the variance at the obliquity period (41 kyr) increased. The timescale tuned to precession suggests that the Pliocene was longer than previously estimated by more than 0.5 m.y. The tuned ages for the magnetic boundaries Gauss\u002FGilbert and Top Cochiti are about 6–8% older than the ages of the conventional timescale. A major phase of Pliocene northern hemisphere ice growth occurred between 3.15 Ma and 2.5 Ma. 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Results, 108, 167",{},{"id":28,"text":2099,"url":28,"identifiers":2100},"10.1038\u002F293193a0",{"doi":2099},{"id":28,"text":2102,"url":28,"identifiers":2103},"10.1007\u002F978-3-642-68409-8_24",{"doi":2102},{"id":28,"text":2105,"url":28,"identifiers":2106},"Schulz H. Hochauflösende Sauerstoff‐ und Kohlenstoffisotopenstratigraphie im frühen Pliozän vor 3.4 bis 4.6 Millionen Jahren: ODP Site 659 Subtropischer Ostatlantik Masters thesis 34pp. Univ. Kiel Hiel Germany 1988.",{},{"id":28,"text":2108,"url":28,"identifiers":2109},"Shackleton N. J., 1984, Oxygen and carbon isotope stratigraphy of Deep Sea Drilling Project hole 552A: Plio‐Pleistocene glacial history, Initial Rep. Deep Sea Drill. Proj., 81, 599",{},{"id":28,"text":1233,"url":28,"identifiers":2111},{"doi":1233},{"id":28,"text":2113,"url":28,"identifiers":2114},"Shackleton N. J., 1994, Pliocene stable isotope stratigraphy of ODP site 846, Proc. Ocean Drill. Program Sci. Results",{},{"id":28,"text":2116,"url":28,"identifiers":2117},"Shackleton N. J., 1994, A new late Neogene time scale: Application to leg 138 sites, Proc. Ocean Drill. Program Sci. Results",{},{"id":28,"text":2119,"url":28,"identifiers":2120},"10.1007\u002FBF01770183",{"doi":2119},{"id":28,"text":2122,"url":28,"identifiers":2123},"Stein R., 1989, Accumulation of marine and terrigenous organic carbon at upwelling site 658 and nonupwelling sites 657 and 659: Implications for the reconstruction of paleoenvironments in the eastern subtropical Atlantic through late Cenozoic times, Proc. Ocean Drill. Program Sci. 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Results, 108, 455",{},{"id":28,"text":1831,"url":28,"identifiers":2149},{"doi":1831},{"id":2151,"createTime":2152,"updateTime":2152,"relativeEntities":2153,"slug":2154,"properties":2155,"entityType":895,"verifyStatus":877,"verifyTime":2152,"verifyNote":897,"languages":2166,"translateLanguages":28,"viewCount":32,"primaryUrl":2167,"fullTextUrl":28,"authors":2168,"publicationType":916,"publisherRelationship":2189,"citationCount":858,"citationInfo":2203,"publishDate":2205,"publishYear":1324,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":2206,"openAccess":28,"references":2207,"isForceReanalyzing":937},"f7e4053f-8698-4d73-9453-c32cc82e74a4","2024-10-11T09:20:33.668+00:00",[],"Application-of-the-Ce-anomaly-as-a-paleoredox-indicator-The-ground-rules",{"openalex":2156,"mag":2158,"abstract":2160,"title":2162,"doi":2164},{"VOID":2157},"W2057482300",{"VOID":2159},"2057482300",{"EN":2161},"\u003Cjats:p>Much attention has been paid, in recent years, to the potential application of the Ce anomaly, measured in various marine phases, as a paleoceanographic indicator of widespread marine anoxia. In this paper we present and discuss results from recent studies of present‐day rare earth element (REE) distributions (and hence Ce anomaly distributions) in the marine environment which are particularly pertinent to paleoceanography. Subsequently, we review and discuss the validity of the recent literature in which Ce anomalies have been employed as paleoredox indicators.\u003C\u002Fjats:p>",{"EN":2163},"Application of the Ce anomaly as a paleoredox indicator: The ground rules",{"VOID":2165},"10.1029\u002Fpa005i005p00823",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002FPA005i005p00823",[2169,2180],{"id":2170,"sortIndex":32,"researcher":28,"roles":2171,"affiliations":2172,"properties":2173,"displayName":2177,"givenName":28,"familyName":28},"306a5d11-0d51-4ef7-9352-3b3d5f22fac6",[],[],{"orcid":2174,"title":2176,"openalex":2178},{"VOID":2175},"https:\u002F\u002Forcid.org\u002F0000-0002-3417-6413",{"EN":2177},"Christopher R. 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ORSTOM Ser. Geol., 7, 65",{},{"id":28,"text":2215,"url":28,"identifiers":2216},"10.1038\u002F301324a0",{"doi":2215},{"id":28,"text":2218,"url":28,"identifiers":2219},"10.1016\u002F0016-7037(85)90089-4",{"doi":2218},{"id":28,"text":2221,"url":28,"identifiers":2222},"10.1016\u002F0016-7037(88)90275-X",{"doi":2221},{"id":28,"text":2224,"url":28,"identifiers":2225},"Elderfield H., 1988, The oceanic chemistry of the rare earth elements, Philos. Trans. R. Soc. London, Ser. A, 325, 105",{},{"id":28,"text":2227,"url":28,"identifiers":2228},"10.1016\u002F0012-821X(81)90095-9",{"doi":2227},{"id":28,"text":2230,"url":28,"identifiers":2231},"10.1038\u002F296214a0",{"doi":2230},{"id":28,"text":2233,"url":28,"identifiers":2234},"10.1016\u002F0048-9697(86)90239-1",{"doi":2233},{"id":28,"text":2236,"url":28,"identifiers":2237},"10.1016\u002F0012-821X(87)90202-0",{"doi":2236},{"id":28,"text":2239,"url":28,"identifiers":2240},"10.1016\u002F0016-7037(81)90184-8",{"doi":2239},{"id":28,"text":2242,"url":28,"identifiers":2243},"10.1016\u002F0016-7037(81)90146-0",{"doi":2242},{"id":28,"text":2245,"url":28,"identifiers":2246},"Elderfield H. H.Kennedy R.Pagett P.Ridout A preliminary study of rare earth elements in pore waters of deep‐sea sediments report Dep. of the Environ. 1986.",{},{"id":28,"text":2248,"url":28,"identifiers":2249},"10.1016\u002F0016-7037(89)90128-2",{"doi":2248},{"id":28,"text":2251,"url":28,"identifiers":2252},"10.1016\u002F0016-7037(90)90262-J",{"doi":2251},{"id":28,"text":2254,"url":28,"identifiers":2255},"10.1038\u002F345516a0",{"doi":2254},{"id":28,"text":2257,"url":28,"identifiers":2258},"10.1016\u002F0304-4203(73)90010-8",{"doi":2257},{"id":28,"text":2260,"url":28,"identifiers":2261},"10.1016\u002F0016-7037(89)90097-5",{"doi":2260},{"id":28,"text":2263,"url":28,"identifiers":2264},"10.1016\u002F0012-821X(87)90084-7",{"doi":2263},{"id":28,"text":2266,"url":28,"identifiers":2267},"10.1029\u002FGL015i004p00389",{"doi":2266},{"id":28,"text":2269,"url":28,"identifiers":2270},"10.1016\u002F0016-7037(88)90068-3",{"doi":2269},{"id":28,"text":2272,"url":28,"identifiers":2273},"10.1038\u002F305185a0",{"doi":2272},{"id":28,"text":2275,"url":28,"identifiers":2276},"Liu Y.‐G., 1984, Chemical profiles in sediment and basalt samples from Deep Sea Drilling Project Leg 74, Hole 525A, Walvis Ridge, Initial Rep. Deep Sea Drill. Pro]., 39, 1047",{},{"id":28,"text":2278,"url":28,"identifiers":2279},"10.1016\u002F0016-7037(88)90207-4",{"doi":2278},{"id":28,"text":2281,"url":28,"identifiers":2282},"10.1016\u002F0016-7037(89)90019-7",{"doi":2281},{"id":28,"text":2284,"url":28,"identifiers":2285},"10.1016\u002F0304-4203(88)90063-1",{"doi":2284},{"id":28,"text":2287,"url":28,"identifiers":2288},"10.1016\u002F0012-821X(85)90077-9",{"doi":2287},{"id":28,"text":2290,"url":28,"identifiers":2291},"10.1016\u002F0016-7037(74)90002-7",{"doi":2290},{"id":28,"text":2293,"url":28,"identifiers":2294},"10.1016\u002F0016-7037(86)90192-4",{"doi":2293},{"id":28,"text":2296,"url":28,"identifiers":2297},"Shannon R. D., 1976, Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcedonides, Acta Crystallogr., Sect. 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In particular, the present study independently confirms the link between major deglaciations (terminations) and increases in northern hemisphere summer radiation at high latitudes and shows that this correlation is not an artifact of orbital tuning. In addition, the excess ice characteristic of late Quaternary “100‐kyr” climate cycles typically accumulates when July insolation at 65°N has been unusually low for more than a full precessional cycle, or >21 kyr, and once established does not last beyond the next increase in summer insolation. Thus, the timing of the growth and decay of large 100‐kyr ice sheets, as depicted in the deep sea δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O record, is strongly (and semipredictably) influenced by eccentricity through its modulation of the orbital precession component of northern hemisphere summer insolation.\u003C\u002Fjats:p>",{"EN":2329},"The timing of major climate terminations",{"VOID":2331},"10.1029\u002F97pa01169",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F97PA01169",[2335],{"id":2336,"sortIndex":32,"researcher":28,"roles":2337,"affiliations":2338,"properties":2347,"displayName":996,"givenName":28,"familyName":28},"53d73f14-a54a-4bda-8578-cf0a948fcdd9",[],[2339],{"id":2340,"sortIndex":32,"affiliation":2341,"properties":28},"e7e06415-febf-42fe-99cc-94783669b2c1",{"id":2340,"createTime":28,"updateTime":28,"relativeEntities":2342,"slug":28,"properties":2343,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2346,"statistic":28},[],{"title":2344},{"VI":2345},"Department of Earth Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge",[],{"orcid":2348,"title":2349,"openalex":2350},{"VOID":994},{"EN":996},{"VOID":998},{"url":28,"publisher":2352,"properties":2360},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2353,"slug":872,"properties":2354,"entityType":25,"verifyStatus":877,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2357,"manageAffiliations":2358,"indexDatabases":2359,"url":28,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":2355,"title":2356},{"VOID":875},{"VOID":872},[],[],[],{"issue":2361,"pages":2362,"volume":2364},{"VOID":1962},{"VOID":2363},"577-585",{"VOID":2365},"12",480,{"total":2366,"publishYear":2368,"statisticByYear":2369},1997,{"2012":127,"2013":146,"2014":130,"2015":136,"2016":129,"2017":126,"2018":323,"2019":357,"2020":199,"2021":352,"2022":152,"2023":136,"2024":127},"1997-08-01",[],[2373,2376,2379,2382,2385,2389,2392,2395,2398,2401,2404,2407,2410,2413,2416,2419,2422,2424,2426,2428,2430,2433,2436,2439,2442,2445,2448,2451,2454,2457,2460,2462,2465,2468,2470,2473,2475,2478,2481],{"id":28,"text":2374,"url":28,"identifiers":2375},"10.1029\u002F94PA00860",{"doi":2374},{"id":28,"text":2377,"url":28,"identifiers":2378},"Berger A., Palaeoclimate sensitivity to CO2 and insolation, Ambio, 26, 32",{},{"id":28,"text":2380,"url":28,"identifiers":2381},"Berger W. H., 1996, The Polar Oceans and Their Role in Shaping the Global Environment, Geophys. Monogr. Ser., 295",{},{"id":28,"text":2383,"url":28,"identifiers":2384},"10.1130\u002F0091-7613(1994)022\u003C0463:QTSFTO>2.3.CO;2",{"doi":2383},{"id":28,"text":2386,"url":28,"identifiers":2387},"Bickert T. W. B.Curry G.Wefer Late Pliocene to Holocene (2.6 – O Ma) western equatorial Atlantic deep water circulation: Inferences from benthic stable isotopes ODP Leg Proc. Ocean Drill. Program Sci. Results 154 154 edited byN. J.Shackleton et al. 1997.",{"doi":2388},"10.2973\u002Fodp.proc.sr.154.110.1997",{"id":28,"text":2390,"url":28,"identifiers":2391},"10.1007\u002F978-94-017-4841-4_14",{"doi":2390},{"id":28,"text":2393,"url":28,"identifiers":2394},"Cheng H., 1996, Pa‐231 dating of carbonates using TIMS techniques (abstract), EOS Trans. AGU, 77, S168",{},{"id":28,"text":2396,"url":28,"identifiers":2397},"Curry W. B., 1995, Proceedings of the Ocean Drilling Program, series‐numbered Initial Reports",{},{"id":28,"text":2399,"url":28,"identifiers":2400},"10.1175\u002F1520-0442(1991)004\u003C0318:AODMOC>2.0.CO;2",{"doi":2399},{"id":28,"text":2402,"url":28,"identifiers":2403},"10.1016\u002F0012-821X(90)90066-7",{"doi":2402},{"id":28,"text":2405,"url":28,"identifiers":2406},"10.1029\u002F91PA00877",{"doi":2405},{"id":28,"text":2408,"url":28,"identifiers":2409},"10.1130\u002F0091-7613(1995)023\u003C0403:ICRCOL>2.3.CO;2",{"doi":2408},{"id":28,"text":2411,"url":28,"identifiers":2412},"10.1126\u002Fscience.263.5148.796",{"doi":2411},{"id":28,"text":2414,"url":28,"identifiers":2415},"10.1126\u002Fscience.194.4270.1121",{"doi":2414},{"id":28,"text":2417,"url":28,"identifiers":2418},"Henderson G., 1996, Direct U\u002FTh dating of marine oxygenisotope substage‐5e in Bahamian sediments (abstract), Eos Trans. AGU, 77, S168",{},{"id":28,"text":2420,"url":28,"identifiers":2421},"10.1130\u002FDNAG-GNA-K3.183",{"doi":2420},{"id":28,"text":1119,"url":28,"identifiers":2423},{"doi":1119},{"id":28,"text":1122,"url":28,"identifiers":2425},{},{"id":28,"text":1125,"url":28,"identifiers":2427},{"doi":1125},{"id":28,"text":2030,"url":28,"identifiers":2429},{"doi":2030},{"id":28,"text":2431,"url":28,"identifiers":2432},"Laskar J., 1993, Orbital, precessional and insolation quantities for the Earth from ‐20 Myrto +10 Myr, Astron. Astrophys., 270, 522",{},{"id":28,"text":2434,"url":28,"identifiers":2435},"10.1029\u002F95GL03027",{"doi":2434},{"id":28,"text":2437,"url":28,"identifiers":2438},"10.1038\u002F358397a0",{"doi":2437},{"id":28,"text":2440,"url":28,"identifiers":2441},"Mix A. C., 1995, Benthic foraminiferal stable isotope record form Site 849, 0–5 Ma: Local and global climate changes, Proc. Ocean Drill. Program. Sci. Results, 371",{},{"id":28,"text":2443,"url":28,"identifiers":2444},"Mix A. C., 1995, Benthic foraminiferal stable isotope stratigraphy of Site 846: 0–1.8 Ma, Proc. Ocean Drill. Program Sci. Results, 839",{},{"id":28,"text":2446,"url":28,"identifiers":2447},"10.1038\u002F377107b0",{"doi":2446},{"id":28,"text":2449,"url":28,"identifiers":2450},"10.1016\u002F0012-821X(81)90197-7",{"doi":2449},{"id":28,"text":2452,"url":28,"identifiers":2453},"10.1029\u002F94PA00289",{"doi":2452},{"id":28,"text":2455,"url":28,"identifiers":2456},"10.1130\u002F0091-7613(1988)016\u003C0649:IOLCMB>2.3.CO;2",{"doi":2455},{"id":28,"text":2458,"url":28,"identifiers":2459},"Ruddiman W. F., 1986, Sediment disturbance and correlation of offset holes drilled with the hydraulic piston corer, Initial Rep. Deep Sea Drill. Proj., 94, 615",{},{"id":28,"text":1218,"url":28,"identifiers":2461},{"doi":1218},{"id":28,"text":2463,"url":28,"identifiers":2464},"10.1029\u002F94PA02289",{"doi":2463},{"id":28,"text":2466,"url":28,"identifiers":2467},"10.1130\u002FMEM145-p449",{"doi":2466},{"id":28,"text":1233,"url":28,"identifiers":2469},{"doi":1233},{"id":28,"text":2471,"url":28,"identifiers":2472},"10.1016\u002F0012-821X(96)00030-1",{"doi":2471},{"id":28,"text":1260,"url":28,"identifiers":2474},{"doi":1260},{"id":28,"text":2476,"url":28,"identifiers":2477},"10.1017\u002FS0022143000023327",{"doi":2476},{"id":28,"text":2479,"url":28,"identifiers":2480},"10.1126\u002Fscience.258.5080.255",{"doi":2479},{"id":28,"text":2482,"url":28,"identifiers":2483},"Winograd I. J., 1996, High resolution δ18O record from Devil's Hole, Nevada, for the period 80 to 19 Ka (abstract), Eos Trans. 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Sea surface temperature, photosynthetic pigments, and a lithic proxy for El Niño flood events on the continent are used as paleo–El Niño–Southern Oscillation proxy data. The onset of stronger El Niño activity in Peru started around 17,000 calibrated years before the present, which is later than modeling experiments show but contemporaneous with the Heinrich event 1. Maximum El Niño activity occurred during the early and late Holocene, especially during the second and third millennium B.P. The recurrence period of very strong El Niño events is 60–80 years. El Niño events were weak before and during the beginning of the Younger Dryas, during the middle of the Holocene, and during medieval times. The strength of El Niño flood events during the last millennium has positive and negative relationships to global and Northern Hemisphere temperature reconstructions.\u003C\u002Fjats:p>",{"EN":2497},"El Niño variability off Peru during the last 20,000 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F., 1992, El Niño",{},{"id":28,"text":2698,"url":28,"identifiers":2699},"Diaz H. F., 2000, El Niño and the Southern Oscillation—Multiscale Variability and Global and Regional Impacts, 10.1017\u002FCBO9780511573125",{"doi":2700},"10.1017\u002FCBO9780511573125",{"id":28,"text":2702,"url":28,"identifiers":2703},"10.1029\u002F2000PA000511",{"doi":2702},{"id":28,"text":2705,"url":28,"identifiers":2706},"Dullo W. C., 2000, Cruise Report Sonne‐147—Peru Upwelling, 102",{},{"id":28,"text":2708,"url":28,"identifiers":2709},"10.1191\u002F0959683603hl622ed",{"doi":2708},{"id":28,"text":2711,"url":28,"identifiers":2712},"10.1126\u002Fscience.1066208",{"doi":2711},{"id":28,"text":2714,"url":28,"identifiers":2715},"Fairbanks R.(1992) Barbados sea level and Th\u002FU14C calibration inIGBP PAGES Data Contrib. Ser. 92–020 World Data Cent.‐A for Paleoclimatol. Boulder Colo. 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Florence Italy 20 – 27 Aug.",{},{"id":28,"text":2877,"url":28,"identifiers":2878},"10.1017\u002FS0033822200013904",{"doi":2877},{"id":28,"text":2880,"url":28,"identifiers":2881},"10.1017\u002FS0033822200019123",{"doi":2880},{"id":28,"text":2883,"url":28,"identifiers":2884},"Suess E., 1990, Scientific Results—Leg 112",{},{"id":28,"text":2886,"url":28,"identifiers":2887},"Suess E. L. D.Kulm andJ. S.Killingley(1987) Coastal upwelling and a history of organic rich mudstone deposition off Peru inMarine Petroleum Source Rocks edited byJ.Brooks andA. J.Fleet Geol. Soc. Spec. Publ. 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Hannover Germany.",{},{"id":28,"text":2914,"url":28,"identifiers":2915},"10.1175\u002F1520-0493(1987)115\u003C2262:AMENO>2.0.CO;2",{"doi":2914},{"id":2917,"createTime":2918,"updateTime":2918,"relativeEntities":2919,"slug":2920,"properties":2921,"entityType":895,"verifyStatus":877,"verifyTime":2918,"verifyNote":897,"languages":2932,"translateLanguages":28,"viewCount":32,"primaryUrl":2933,"fullTextUrl":28,"authors":2934,"publicationType":916,"publisherRelationship":2946,"citationCount":2960,"citationInfo":2961,"publishDate":2963,"publishYear":934,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":2964,"openAccess":28,"references":2965,"isForceReanalyzing":937},"258cae29-f079-4ac6-b3a5-8c715e4d2c98","2024-10-09T08:48:27.403+00:00",[],"Nannofossils-and-superplumes-The-Early-Aptian-nannoconid-crisis-",{"openalex":2922,"mag":2924,"abstract":2926,"title":2928,"doi":2930},{"VOID":2923},"W2058695708",{"VOID":2925},"2058695708",{"EN":2927},"\u003Cjats:p>A group of calcareous nannoplankton named nannoconids experienced a crisis in the early Aptian and recovered only later in the late Aptian after a period of virtual absence. Although no extinctions occurred, the widespread nature of the “nannoconid crisis” suggests a global causal factor. This crisis is recorded within the \u003Cjats:italic>Chiastozygus litterarius\u003C\u002Fjats:italic> nannofossil and \u003Cjats:italic>Globigerinelloides blowi\u003C\u002Fjats:italic> planktonic foraminiferal zones, postdates magnetic chronozone M0 by approximately 300 kyr, and precedes the oceanic anoxic subevent 1a and associated δ\u003Cjats:sup>13\u003C\u002Fjats:sup>C anomaly by some 40–100 kyr. Selective dissolution and anoxia cannot explain the crisis, because nannoconids are dissolution‐resistant forms and their crisis clearly precedes the deposition of anoxic sediments. At least 1 m.y. prior to the “nannoconid crisis,” the onset of a nannoplankton speciation event may be the response of nannofloras to a major rise in relative sea level. The “nannoconid crisis” seems to be synchronous with the early Aptian volcanic eruptions in the Pacific Ocean. Hence calcareous nannoplankton were severely affected by the “superplume” volcanic episode. The coccolithophorid bloom\u002Fnannoconid crisis was possibly induced by the excessive CO\u003Cjats:sub>2\u003C\u002Fjats:sub> levels in the atmosphere and\u002For caused by changes in nutrient content of oceanic surface waters. Fertility was enhanced by rapid turnover of nutrients due to the abnormal volcanic activity and accelerated transfer of nutrients from the continents into the oceans under warm and humid conditions of the mid‐Cretaceous greenhouse climate. The “nannoconid crisis” may represent a competition between phytoplankton groups for nutrients or, more likely, competition between different calcareous nannoplankton. The biologic affinity and mode of life of \u003Cjats:italic>Nannoconus\u003C\u002Fjats:italic> are unknown, because there is no modern analog of this genus. However, comparison of Lower Cretaceous nannofossil assemblages with modern nannoplankton cummunities suggests that nannoconids, like extant \u003Cjats:italic>Florisphaera profunda\u003C\u002Fjats:italic>, possibly inhabited the lower photic zone. Concentrations of nutrients in the upper euphotic zone may have triggered blooms of coccolithophorids and nannoconid depletion. This model implies that the “nannoconid crisis” is the result of an abrupt, major change in the structure of surface waters caused directly or indirectly by the “superplume.” The adjustments of the biosphere to the new paleoceanographic and climatic conditions required some 40–100 kyr before changing into abnormally high primary productivity and deposition of organic carbon‐rich sediments with dinoflagellates outcompeting nannoplankton.\u003C\u002Fjats:p>",{"EN":2929},"Nannofossils and superplumes: The Early Aptian “nannoconid crisis”",{"VOID":2931},"10.1029\u002F94pa00258",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F94PA00258",[2935],{"id":2936,"sortIndex":32,"researcher":28,"roles":2937,"affiliations":2938,"properties":2939,"displayName":2943,"givenName":28,"familyName":28},"a8b0bb63-6bf9-4743-97c6-1d60227561e3",[],[],{"orcid":2940,"title":2942,"openalex":2944},{"VOID":2941},"https:\u002F\u002Forcid.org\u002F0000-0001-6213-6550",{"EN":2943},"Elisabetta Erba",{"VOID":2945},"A5059153091",{"url":28,"publisher":2947,"properties":2955},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2948,"slug":872,"properties":2949,"entityType":25,"verifyStatus":877,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2952,"manageAffiliations":2953,"indexDatabases":2954,"url":28,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":55,"analyzePriority":28},[],{"issn":2950,"title":2951},{"VOID":875},{"VOID":872},[],[],[],{"issue":2956,"pages":2957,"volume":2959},{"VOID":1666},{"VOID":2958},"483-501",{"VOID":932},385,{"total":2960,"publishYear":934,"statisticByYear":2962},{"2012":128,"2013":51,"2014":51,"2015":130,"2016":47,"2017":145,"2018":146,"2019":135,"2020":130,"2021":135,"2022":127,"2023":51,"2024":48},"1994-06-01",[],[2966,2969,2972,2975,2978,2981,2984,2987,2990,2993,2996,2999,3002,3005,3008,3011,3014,3017,3020,3023,3026,3029,3032,3035,3038,3041,3044,3047,3050,3053,3056,3059,3062,3065,3068,3071,3074,3077,3080,3083,3086,3089,3092,3095,3098,3101,3104,3107,3110,3113,3116,3119,3122,3125,3128,3131,3134,3137,3140,3143,3146,3149,3152,3155,3158,3161,3164,3167,3170,3173,3176,3179,3182,3185,3188,3191,3194,3198,3201,3204,3207,3210,3213,3216,3219,3222,3225,3228,3231,3234,3237],{"id":28,"text":2967,"url":28,"identifiers":2968},"Applegate J. 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Ital., 44, 59",{},{"id":28,"text":3235,"url":28,"identifiers":3236},"Weissert H., 1991, Controversies in Modern Geology, 173",{},{"id":28,"text":3238,"url":28,"identifiers":3239},"10.1029\u002FGM032p0531",{"doi":3238},{"id":3241,"createTime":3242,"updateTime":3242,"relativeEntities":3243,"slug":3244,"properties":3245,"entityType":895,"verifyStatus":26,"verifyTime":3242,"verifyNote":956,"languages":3256,"translateLanguages":28,"viewCount":32,"primaryUrl":3257,"fullTextUrl":28,"authors":3258,"publicationType":916,"publisherRelationship":3292,"citationCount":577,"citationInfo":3305,"publishDate":3308,"publishYear":3306,"citationAnalyzeStatus":877,"lastCitationAnalyze":28,"indexDatabases":3309,"openAccess":28,"references":3310,"isForceReanalyzing":937},"2da3228d-0c71-44e3-840c-6f546acab737","2024-10-06T22:31:13.358+00:00",[],"The-41-kyr-world-Milankovitch-s-other-unsolved-mystery",{"openalex":3246,"mag":3248,"abstract":3250,"title":3252,"doi":3254},{"VOID":3247},"W2107030987",{"VOID":3249},"2107030987",{"EN":3251},"\u003Cjats:p>For most of the Northern Hemisphere Ice Ages, from ∼3.0 to 0.8 m.y., global ice volume varied predominantly at the 41,000 year period of Earth's orbital obliquity. However, summer (or summer caloric half year) insolation at high latitudes, which is widely believed to be the major influence on high‐latitude climate and ice volume, is dominated by the 23,000 year precessional period. Thus the geologic record poses a challenge to our understanding of climate dynamics. Here we propose that variations in the insolation gradient between high and low latitudes control high‐latitude climate and ice volume during the late Pliocene and early Pleistocene. The differential heating between high and low latitudes, driven by obliquity, controls the atmospheric meridional flux of heat, moisture, and latent energy, which may exert the dominant control on high‐latitude climate on Milankovitch timescales. In the two‐dimensional zonal energy balance models typically used to study the long‐term evolution of climate, the meridional atmospheric moisture flux is usually kept fixed. The hypothesis that insolation gradients control the poleward energy fluxes, precipitation, and ice volume at high latitudes has never been directly examined within the context of an ice sheet model. In light of what we know about modern energy fluxes and their relative influence on high‐latitude climate, this possibility should be examined.\u003C\u002Fjats:p>",{"EN":3253},"The 41 kyr world: Milankovitch's other unsolved mystery",{"VOID":3255},"10.1029\u002F2002pa000791",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F2002PA000791",[3259,3273],{"id":3260,"sortIndex":32,"researcher":28,"roles":3261,"affiliations":3262,"properties":3269,"displayName":996,"givenName":28,"familyName":28},"41c78efb-d9ae-4d81-88ac-ba8cfa916b15",[],[3263],{"id":985,"sortIndex":32,"affiliation":3264,"properties":28},{"id":985,"createTime":28,"updateTime":28,"relativeEntities":3265,"slug":28,"properties":3266,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3268,"statistic":28},[],{"title":3267},{"EN":990},[],{"orcid":3270,"title":3271,"openalex":3272},{"VOID":994},{"EN":996},{"VOID":998},{"id":3274,"sortIndex":40,"researcher":28,"roles":3275,"affiliations":3276,"properties":3285,"displayName":3289,"givenName":28,"familyName":28},"2d9e6ad5-a0ec-4f4a-92f9-a5eac6f20df6",[],[3277],{"id":3278,"sortIndex":32,"affiliation":3279,"properties":28},"c137d5c4-fdcc-4081-9e10-753deab475ee",{"id":3278,"createTime":28,"updateTime":28,"relativeEntities":3280,"slug":28,"properties":3281,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":3284,"statistic":28},[],{"title":3282},{"VI":3283},"Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA",[],{"orcid":3286,"title":3288,"openalex":3290},{"VOID":3287},"https:\u002F\u002Forcid.org\u002F0000-0002-5737-5765",{"EN":3289},"Kerim H. 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