Boreas
SCIE-ISI SCOPUS (1972-2023)
0300-9483
1502-3885
Mỹ
Cơ quản chủ quản: WILEY , Wiley-Blackwell
Lĩnh vực:
Ecology, Evolution, Behavior and SystematicsArcheology (arts and humanities)Geology
Các bài báo tiêu biểu
The last Eurasian ice sheets – a chronological database and time‐slice reconstruction, DATED‐1We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish, Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these interconnected ice sheets every 1000 years from 25 to 10 ka, and at four selected time periods back to 40 ka. The time‐slice maps of ice‐sheet extent are based on a new Geographical Information System (...
Tập 45 Số 1 - Trang 1-45 - 2016
Luminescence dating of glacial and associated sediments: review, recommendations and future directionsDating glacial and associated sediments is essential to provide a temporal framework for accurate reconstructions of past climatic conditions and for helping to determine the nature and magnitude of glaciation for landscape evolution studies. There are few widely applicable, accurate and precise methods available to date Quaternary landforms and sediments, despite the numerous numerical da... ...
Tập 37 Số 4 - Trang 636-659 - 2008
Palaeo-ice streams, trough mouth fans and high-latitude continental slope sedimentation
Tập 32 Số 1 - Trang 37-55 - 2003
Dynamics of the Late Weichselian ice sheet on Svalbard inferred from high‐resolution sea‐floor morphologyHigh‐resolution bathymetric mapping of the fjords and continental shelf around the Svalbard archipelago shows an extensive pattern of large‐ and medium‐scale submarine landforms formed by differences in ice‐flow regimes. Mega‐scale glacial lineations, lateral moraines, transverse ridges and glaciotectonic features are superimposed on the large‐scale fjord, shelf and cross‐shelf trough morp... ...
Tập 36 Số 3 - Trang 286-306 - 2007
Map and GIS database of glacial landforms and features related to the last British Ice Sheet
Tập 33 Số 4 - Trang 359-375 - 2004
Norwegian corals: radiocarbon and stable isotopes in Lophelia pertusaThe ahermatypic coral Lophelia pertusa which produces aragonitic skeletons is widely distributed along the Norwegian coast. Specimens from a number of localities have been analyzed for oxygen and stable carbon isotope composition and 14 C age. Stable isotope ratios of recent corals provide information on growth rate and seasonality of oceanogr... ...
Tập 11 Số 2 - Trang 163-171 - 1982
An alternative Weichselian glaciation model, with special reference to the glacial history of Skåne, South SwedenA revised lithostratigraphy of Skåne, South Sweden, constitutes the basis of an alternative Weichselian glaciation model for southern Scandinavia, progressively anchored to the stratigraphy. Skåne was not glaciated during the Weichselian until 21,000 B.P. The concepts, outlet surge and marginal dome (the main tools of the model) are defined. The palaeogeography o... ...
Tập 16 Số 4 - Trang 433-459 - 1987
Timing and pattern of the last deglaciation in the Kattegat region, southwest ScandinaviaThis paper presents evidence on the timing and pattern of the Late Weichselian deglaciation in SW Scandinavia, particularly in the Öresund–Kattegat region before the Allerød interstadial. New radiocarbon ages and evaluated older dates demonstrate that active glacier ice had left eastern Denmark, southern Halland and western Skåne before 14,000 BP. The deglaciation in the Öresund region too... ...
Tập 22 Số 4 - Trang 337-347 - 1993
A mountain icefield of Loch Lomond Stadial age, western Grampians, ScotlandThe extent of a large mountain icefield that existed in the western Grampians during the Loch Lomond stade has been mapped. The main types of evidence used in establishing the limits comprise moraines, thick drift, fluvioglacial landforms, erratics, ice‐smoothed bedrock, striae, friction cracks and relict periglacial forms. Trimlines on 198 spurs, and various forms of glacial and periglaci... ...
Tập 15 Số 1 - Trang 83-97 - 1986
Holocene vegetation and climate changes in Hoton-Nur basin, northwest Mongolia
Tập 29 Số 2 - Trang 117-126 - 2000