1. A Marine Barite Perspective of the Late Miocene Biogenic Bloom in the Equatorial Indian Ocean and Equatorial Western Atlantic Ocean.
- Author
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Wu, Xinying, Hu, Yue, Nan, Jingbo, and Yao, Weiqi
- Subjects
CARBON cycle ,GLOBAL cooling ,BIOLOGICAL productivity ,MARINE sediments ,MARINE productivity - Abstract
The marine biological pump is crucial for removing excess carbon dioxide from the atmosphere to the ocean interior and seafloor sediments. The Late Miocene Biogenic Bloom (LMBB), marked by notable increases in biogenic components in marine sediments, provides insights into the response of the biological pump to climate change. However, understanding the timing, distribution, and cause of the LMBB remains limited. We use marine barite, a refractory mineral precipitating from the water column associated with carbon export, and other proxies to reconstruct productivity in the equatorial Indian Ocean and equatorial western Atlantic between 12 and 5 Ma. Multi‐proxy records reveal the onset of the LMBB in the equatorial Indian Ocean at ∼9 Ma, primarily driven by more vigorous upwelling during global cooling. We suggest that the steepened meridional temperature gradient and the Antarctic ice sheet expansion have strengthened ocean overturning, facilitating nutrient supply and biogenic bloom in upwelling regions. Plain Language Summary: The late Miocene (11.6–5.33 Ma), with an atmospheric CO2 concentration similar to the pre‐industrial level, represents an ideal time window for understanding the relationship between anthropogenic climate, ocean circulation, and global carbon cycling. During this time interval, biogenic components in marine sediments have increased significantly, which is known as the Late Miocene Biogenic Bloom (LMBB). However, due to the limitations of traditional productivity proxies (e.g., biogenic calcium carbonate, biogenic silica), the temporal and spatial distributions of this event remain controversial. In this study, we use marine barite accumulation rate as a reliable tracer of the LMBB, as marine barite precipitating from the water column is closely associated with export productivity and has very low solubility. Our new barite records from two low‐latitude sites inside and outside an upwelling regime suggest that the LMBB has commenced at ∼9 Ma in the equatorial Indian Ocean but has not occurred or sustained in the equatorial western Atlantic. By compiling sea‐surface temperature and multi‐proxy data, we attribute the LMBB to intensified ocean overturning under global cooling. The enhanced biological productivity, fueled by nutrient supply from upwelling, provides positive feedback to the late‐Miocene climate cooling. Key Points: Marine barite provides new insight into the Late Miocene Biogenic BloomMulti‐proxy records show inconsistent productivity changes in the equatorial Indian Ocean and equatorial western Atlantic OceanLate‐Miocene cooling strengthens ocean overturning and nutrient supply to the surface, driving biogenic bloom in upwelling regions [ABSTRACT FROM AUTHOR]
- Published
- 2024
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