Image1_Intermediate- and Deep-Water Oxygenation History in the Subarctic North Pacific During the Last Deglacial Period.JPEG

• Main Authors: Ekaterina Ovsepyan, Elena Ivanova, Martin Tetard, Lars Max, Ralf Tiedemann
• Format: Still Image
• Language: unknown
• Published: 2021
• Subjects: Solid Earth Sciences; Climate Science; Atmospheric Sciences not elsewhere classified; Exploration Geochemistry; Inorganic Geochemistry; Isotope Geochemistry; Organic Geochemistry; Geochemistry not elsewhere classified; Igneous and Metamorphic Petrology; Ore Deposit Petrology; Palaeontology (incl. Palynology); Structural Geology; Tectonics; Volcanology; Geology not elsewhere classified; Seismology and Seismic Exploration; Glaciology; Hydrogeology; Natural Hazards; Quaternary Environments; Earth Sciences not elsewhere classified; Evolutionary Impacts of Climate Change; oxygen minimum zone; ocean circulation; sea-surface bioproductivity; teleconnections; transfer function; benthic foraminifers; North Pacific; Southern Ocean; Antarctic; The Antarctic; Bering Sea; Pacific; Shirshov Ridge; Antarc*; NGRIP; North Atlantic; Subarctic
• Online Access: https://doi.org/10.3389/feart.2021.638069.s003; https://figshare.com/articles/figure/Image1_Intermediate-_and_Deep-Water_Oxygenation_History_in_the_Subarctic_North_Pacific_During_the_Last_Deglacial_Period_JPEG/16565499

Deglacial dissolved oxygen concentrations were semiquantitatively estimated for intermediate and deep waters in the western Bering Sea using the benthic foraminiferal-based transfer function developed by Tetard et al. (2017), Tetard et al. (2021a). Benthic foraminiferal assemblages were analyzed fro...