(Table S1) N15 isotope ratios, age determination and accumulation rates of sediment core HLY02-02-17 ...

In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured over the last glacial/interglacial cycle. Compared to the interglacial sections of the core, the sediments of the last ice...

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Bibliographic Details
Main Authors: Brunelle, Brigitte G, Sigman, Daniel M, Cook, Mea S, Keigwin, Lloyd D, Haug, Gerald H, Plessen, Birgit, Schettler, Georg, Jaccard, Samuel L
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.833622
https://doi.pangaea.de/10.1594/PANGAEA.833622
Description
Summary:In a piston core from the central Bering Sea, diatom microfossil-bound N isotopes and the concentrations of opal, biogenic barium, calcium carbonate, and organic N are measured over the last glacial/interglacial cycle. Compared to the interglacial sections of the core, the sediments of the last ice age are characterized by 3 per mil higher diatom-bound d15N, 70 wt % lower opal content and 1200 ppm lower biogenic barium. Taken together and with constraints on sediment accumulation rate, these results suggest a reduced supply of nitrate to the surface due to stronger stratification of the upper water column of the Bering Sea during glacial times, with more complete nitrate consumption resulting from continued iron supply through atmospheric deposition. This finding extends the body of evidence for a pervasive link between cold climates and polar ocean stratification. In addition, we hypothesize that more complete nutrient consumption in the glacial age subarctic Pacific contributed to the previously observed ... : Supplement to: Brunelle, Brigitte G; Sigman, Daniel M; Cook, Mea S; Keigwin, Lloyd D; Haug, Gerald H; Plessen, Birgit; Schettler, Georg; Jaccard, Samuel L (2007): Evidence from diatom-bound nitrogen isotopes for subarctic Pacific stratification during the last ice age and a link to North Pacific denitrification changes. Paleoceanography, 22(1), PA1215 ...