TY - JOUR
T1 - Atmospheric iron supply and marine productivity in the glacial North Pacific Ocean
AU - Burgay, François
AU - Spolaor, Andrea
AU - Gabrieli, Jacopo
AU - Cozzi, Giulio
AU - Turetta, Clara
AU - Vallelonga, Paul
AU - Barbante, Carlo
PY - 2021/2/23
Y1 - 2021/2/23
N2 - 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 mgm-2yr-1) at the NEEM site were 4 times lower than the average recorded over the last glacial period (11.7-108 ka, 2.0 mgm-2yr-1), whereas they were greater during the Last Glacial Maximum (LGM; 14.5-26.5 ka, 3.6 mgm-2yr-1) and Marine Isotope Stage 4 (MIS 4; 60- 71 ka, 5.8 mgm-2yr-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.
AB - 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 mgm-2yr-1) at the NEEM site were 4 times lower than the average recorded over the last glacial period (11.7-108 ka, 2.0 mgm-2yr-1), whereas they were greater during the Last Glacial Maximum (LGM; 14.5-26.5 ka, 3.6 mgm-2yr-1) and Marine Isotope Stage 4 (MIS 4; 60- 71 ka, 5.8 mgm-2yr-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.
UR - http://www.scopus.com/inward/record.url?scp=85101417518&partnerID=8YFLogxK
U2 - 10.5194/cp-17-491-2021
DO - 10.5194/cp-17-491-2021
M3 - Article
AN - SCOPUS:85101417518
SN - 1814-9324
VL - 17
SP - 491
EP - 505
JO - Climate of the Past
JF - Climate of the Past
IS - 1
ER -