Iron in the NEEM ice core relative to Asian loess records over the last glacial-interglacial cycle

• Published in: National Science Review
• Main Authors: Xiao, Cunde, Du, Zhiheng, Handley, Mike J., Mayewski, Paul A., Cao, Junji, Schuepbach, Simon, Zhang, Tong, Petit, Jean-Robert, Li, Chuanjin, Han, Yeongcheol, Li, Yuefang, Ren, Jiawen
• Format: Report
• Language: English
• Published: OXFORD UNIV PRESS 2021
• Subjects: Greenland NEEM ice core; iron fertilization; carbon dioxide; Chinese loess; glacial-interglacial cycle; NORTH-ATLANTIC; ATMOSPHERIC IRON; CHINA LOESS; GREENLAND; DUST; CLIMATE; MONSOON; SOLUBILITY; LINK; DISTRIBUTIONS; Science & Technology - Other Topics; Multidisciplinary Sciences; Greenland; ice core; North Atlantic; North Greenland
• Online Access: http://ir.ieecas.cn/handle/361006/17019; http://ir.ieecas.cn/handle/361006/17020; https://doi.org/10.1093/nsr/nwaa144

Mineral dust can indirectly affect the climate by supplying bioavailable iron (Fe) to the ocean. Here, we present the records of dissolved Fe (DFe) and total Fe (TDFe) in North Greenland Eemian Ice Drilling (NEEM) ice core over the past 110 kyr BP. The Fe records are significantly negatively correlated with the carbon-dioxide (CO2) concentrations during cold periods. The results suggest that the changes in Fe fluxes over the past 110 kyr BP in the NEEM ice core are consistent with those in Chinese loess records because the mineral-dust distribution is controlled by the East Asian deserts. Furthermore, the variations in the dust input on a global scale are most likely driven by changes in solar radiation during the last glacial-interglacial cycle in response to Earth's orbital cycles. In the last glacial-interglacial cycle, the DFe/TDFe ratios were higher during the warm periods (following the post-Industrial Revolution and during the Holocene and last interglacial period) than during the main cold period (i.e. the last glacial maximum (LGM)), indicating that the aeolian input of iron and the iron fertilization effect on the oceans have a non-linear relationship during different periods. Although the burning of biomass aerosols has released large amounts of DFe since the Industrial Revolution, no significant responses are observed in the DFe and TDFe variations during this period, indicating that severe anthropogenic contamination has no significant effect on the DFe (TDFe) release in the NEEM ice core.