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Maureen Walczak
University of WashingtonMeeting roles in:
Advances in Understanding Global Meridional Overturning Circulation from Past to Future: Insights from Multiple Approaches I Oral
Advances in Understanding Global Meridional Overturning Circulation from Past to Future: Insights from Multiple Approaches II Poster
Is Indian Ocean overturning different? Testing the anomalously old deep Indian Ocean radiocarbon (14C) ages during the last glacial maximum
Comparing Holocene Relative Paleointensity Records from Pacific Northwest Marine and Terrestrial Sediment Cores
GoAPSV50: A New 15-50 ka North Pacific PSV and RPI Reconstruction from the Gulf of Alaska using high-resolution sediments from International Ocean Discovery Program (IODP) Exp. 341
Paleomagnetic Secular Variation and Radiocarbon from the Last Glacial Maximum through the Initiation of Deglaciation: Building a New High-Resolution, Well-Dated Template for the Greenland Region from the Labrador Sea (AR2307-8JC, BADEX)
Using Sedimentology to Inform Paleomagnetic Secular Variation Correlations in Deglacial Records of the western Greenland Ice Sheet
Assessing Diagenetic Alteration of Foraminiferal Geochemistry in Northeast Pacific Continental Margin Sediments
Oceanographic Conditions on the Central West Greenland Margin from Late MIS 3 Through the Holocene: Preliminary Faunal Assemblage Analysis from the Disko Trough Mouth Fan
A Multi-Proxy Investigation of High and Ultra-High Resolution Sediment Records from the Surveyor Fan in the Gulf of Alaska over the Last 50 Ka: Capturing Sediment, Ice, and Oceanographic Dynamics from International Ocean Discovery Program (IODP) Exp. 341
Linkages between modern benthic foraminiferal assemblages and environmental conditions at continental slope depths: from Baffin Bay to the Labrador Sea
Holocene Pacific Northwest Hydroclimate and Columbia River Discharge from Continental Margin Sediments
A >1 km-thick Grounded Ice Shelf in Baffin Bay Buttressed the Greenland, Laurentide, and Innuitian Ice Sheets During the Last Glacial Maximum
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