Atlantic water inflow to Labrador Sea and its interaction with ice sheet dynamics during the Holocene
Author:
Funder
Deutsche Forschungsgemeinschaft
Publisher
Elsevier BV
Subject
Geology,Archaeology,Archaeology,Ecology, Evolution, Behavior and Systematics,Global and Planetary Change
Reference136 articles.
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3. Holocene variations in mineral and grain-size composition along the East Greenland glaciated margin (ca 67°-70°N): local versus long-distance sediment transport;Andrews;Quat. Sci. Rev.,2010
4. Abrupt deglaciation events and Holocene palaeoceanography from high-resolution cores, cartwright saddle, labrador shelf, Canada;Andrews;J. Quat. Sci.,1999
5. Late Quaternary changes in sediment composition on the NE Greenland margin (∼73° N) with a focus on the fjords and shelf;Andrews;Boreas,2016
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2. Evaluating middle to late Holocene climate variability from δ18O of aquatic invertebrate remains in southwestern Greenland;Quaternary Science Reviews;2024-06
3. Interaction between ice sheet dynamics and sea surface characteristics in the Labrador Sea during the last 50 ka;Earth and Planetary Science Letters;2024-03
4. Biomarker Records of Environmental Shifts on the Labrador Shelf During the Holocene;Paleoceanography and Paleoclimatology;2023-09
5. Lake Dynamics Modulate the Air Temperature Variability Recorded by Sedimentary Aquatic Biomarkers: A Holocene Case Study From Western Greenland;Journal of Geophysical Research: Biogeosciences;2023-06-27
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