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• W3131276491 abstract "Abstract. Iron (Fe) is a key element in the Earth climate system, as it can enhance marine primary productivity in the high-nutrient low-chlorophyll (HNLC) regions where, despite a high concentration of major nutrients, chlorophyll production is low due to iron limitation. Eolian mineral dust represents one of the main Fe sources to the oceans; thus, quantifying its variability over the last glacial cycle is crucial to evaluate its role in strengthening the biological carbon pump. Polar ice cores, which preserve detailed climate records in their stratigraphy, provide a sensitive and continuous archive for reconstructing past eolian Fe fluxes. Here, we show the Northern Hemisphere Fe record retrieved from the NEEM ice core (Greenland), which offers a unique opportunity to reconstruct the past Fe fluxes in a portion of the Arctic over the last 108 kyr. Holocene Fe fluxes (0.042–11.7 ka, 0.5 mg m−2 yr−1) at the NEEM site were 4 times lower than the average recorded over the last glacial period (11.7–108 ka, 2.0 mg m−2 yr−1), whereas they were greater during the Last Glacial Maximum (LGM; 14.5–26.5 ka, 3.6 mg m−2 yr−1) and Marine Isotope Stage 4 (MIS 4; 60–71 ka, 5.8 mg m−2 yr−1). Comparing the NEEM Fe record with paleoceanographic records retrieved from the HNLC North Pacific, we found that the coldest periods, characterized by the highest Fe fluxes, were distinguished by low marine primary productivity in the subarctic Pacific Ocean, likely due to the greater sea ice extent and the absence of major nutrients upwelling. This supports the hypothesis that Fe fertilization during colder and dustier periods (i.e., LGM and MIS 4) was more effective in other regions, such as the midlatitude North Pacific, where a closer relationship between marine productivity and the NEEM Fe fluxes was observed." @default.
• W3131276491 created "2021-03-01" @default.
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• W3131276491 date "2021-02-23" @default.
• W3131276491 modified "2023-10-03" @default.
• W3131276491 title "Atmospheric iron supply and marine productivity in the glacial North Pacific Ocean" @default.
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• W3131276491 cites W1807406143 @default.
• W3131276491 cites W1895855503 @default.
• W3131276491 cites W1903916944 @default.
• W3131276491 cites W1963000257 @default.
• W3131276491 cites W1978704803 @default.
• W3131276491 cites W1986437276 @default.
• W3131276491 cites W1987957061 @default.
• W3131276491 cites W1990693550 @default.
• W3131276491 cites W1992796439 @default.
• W3131276491 cites W1992941940 @default.
• W3131276491 cites W1992983800 @default.
• W3131276491 cites W2000100390 @default.
• W3131276491 cites W2002717773 @default.
• W3131276491 cites W2002812964 @default.
• W3131276491 cites W2010057848 @default.
• W3131276491 cites W2010169680 @default.
• W3131276491 cites W2012655165 @default.
• W3131276491 cites W2014489970 @default.
• W3131276491 cites W2016494665 @default.
• W3131276491 cites W2020642721 @default.
• W3131276491 cites W2021949139 @default.
• W3131276491 cites W2032862522 @default.
• W3131276491 cites W2033744233 @default.
• W3131276491 cites W2037060274 @default.
• W3131276491 cites W2040269627 @default.
• W3131276491 cites W2041794162 @default.
• W3131276491 cites W2042755568 @default.
• W3131276491 cites W2043874066 @default.
• W3131276491 cites W2046541010 @default.
• W3131276491 cites W2054003845 @default.
• W3131276491 cites W2060976955 @default.
• W3131276491 cites W2073228172 @default.
• W3131276491 cites W2086583469 @default.
• W3131276491 cites W2090964269 @default.
• W3131276491 cites W2093519985 @default.
• W3131276491 cites W2100135733 @default.
• W3131276491 cites W2104159045 @default.
• W3131276491 cites W2104202952 @default.
• W3131276491 cites W2118824143 @default.
• W3131276491 cites W2122295209 @default.
• W3131276491 cites W2125753237 @default.
• W3131276491 cites W2126332638 @default.
• W3131276491 cites W2133290278 @default.
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• W3131276491 cites W2150303148 @default.
• W3131276491 cites W2154446767 @default.
• W3131276491 cites W2154889667 @default.
• W3131276491 cites W2155715021 @default.
• W3131276491 cites W2157426825 @default.
• W3131276491 cites W2162228336 @default.
• W3131276491 cites W2170938076 @default.
• W3131276491 cites W2171519564 @default.
• W3131276491 cites W2172525329 @default.
• W3131276491 cites W2192340157 @default.
• W3131276491 cites W2214308497 @default.
• W3131276491 cites W2254804242 @default.
• W3131276491 cites W2327883368 @default.
• W3131276491 cites W2499371091 @default.
• W3131276491 cites W2621869134 @default.
• W3131276491 cites W2658048128 @default.
• W3131276491 cites W2660262358 @default.
• W3131276491 cites W2765180760 @default.
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• W3131276491 doi "https://doi.org/10.5194/cp-17-491-2021" @default.
• W3131276491 hasPublicationYear "2021" @default.
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