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• W2070419999 abstract "Coincident with the intensification of Northern Hemisphere Glaciation (NHG) around 2.73 million years (Ma) ago, sediment cores from both the open subarctic North Pacific and the Antarctic indicate a rapid decline in diatom opal accumulation flux to the seabed, representing one of the most abrupt and dramatic changes in the marine sediment record associated with the development of Pleistocene glacial cycles. In the North Pacific, bulk sediment nitrogen isotope data and alkenone-derived sea surface temperature (SST) estimates suggest that the productivity decline was driven by reduced exchange between surface and deep water, due to weaker wind-driven upwelling and/or a strengthening of the halocline (i.e. “stratification”). In this study of the 2.73 Ma transition at Ocean Drilling Program (ODP) Site 882 in the western subarctic North Pacific, diatom-bound nitrogen isotopes (δ15Ndb), alkenone mass accumulation rate, and alkenone- and archaeal tetraether-based SST reconstructions support the stratification hypothesis, indicating perennially lower export production, generally higher nitrate consumption, and greater inter-seasonal variation in SST after the 2.73 Ma transition. In addition, the δ15Ndb of large and small size fractions of Coscinodiscus spp. suggest that these diatoms grew mostly during the spring bloom during the late Pliocene, switching to their current fall-to-winter growth period at the 2.73 Ma transition; this view is consistent with their decline in dominance and provides further evidence for increased stratification (reduced vertical exchange) in the North Pacific after 2.73 Ma. The δ15Ndb data indicate that, over the ∼100 kyr period after the 2.73 Ma transition studied here, nitrate consumption did not reach late Pleistocene ice age levels and that nitrate consumption in post-2.73 Ma warm stages was similar to that before the transition, even though productivity was greatly reduced. We tentatively attribute this to relatively weak dust-borne iron inputs in the early post-2.73 Ma period." @default.
• W2070419999 created "2016-06-24" @default.
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• W2070419999 date "2012-10-01" @default.
• W2070419999 modified "2023-10-09" @default.
• W2070419999 title "Enhanced stratification and seasonality in the Subarctic Pacific upon Northern Hemisphere Glaciation–New evidence from diatom-bound nitrogen isotopes, alkenones and archaeal tetraethers" @default.
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• W2070419999 cites W1482073456 @default.
• W2070419999 cites W1482110512 @default.
• W2070419999 cites W1502045764 @default.
• W2070419999 cites W1530582274 @default.
• W2070419999 cites W1547692184 @default.
• W2070419999 cites W1573296852 @default.
• W2070419999 cites W1625579457 @default.
• W2070419999 cites W1632941255 @default.
• W2070419999 cites W1642061853 @default.
• W2070419999 cites W1652059687 @default.
• W2070419999 cites W1657772896 @default.
• W2070419999 cites W1794096300 @default.
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• W2070419999 cites W1832501630 @default.
• W2070419999 cites W1887029327 @default.
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• W2070419999 cites W1988124533 @default.
• W2070419999 cites W1989042161 @default.
• W2070419999 cites W1989872636 @default.
• W2070419999 cites W1991795942 @default.
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• W2070419999 cites W2015947524 @default.
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• W2070419999 cites W2018818716 @default.
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• W2070419999 cites W2030534042 @default.
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• W2070419999 cites W2042476750 @default.
• W2070419999 cites W2048360353 @default.
• W2070419999 cites W2049272276 @default.
• W2070419999 cites W2051302740 @default.
• W2070419999 cites W2053668010 @default.
• W2070419999 cites W2054645529 @default.
• W2070419999 cites W2055898789 @default.
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• W2070419999 cites W2076409230 @default.
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• W2070419999 doi "https://doi.org/10.1016/j.epsl.2012.07.029" @default.
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