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Neogene continental denudation and the beryllium conundrum.

Shilei 李石磊 LiSteven L GoldsteinMaureen E Raymo
Published in: Proceedings of the National Academy of Sciences of the United States of America (2021)
Reconstructing Cenozoic history of continental silicate weathering is crucial for understanding Earth's carbon cycle and greenhouse history. The question of whether continental silicate weathering increased during the late Cenozoic, setting the stage for glacial cycles, has remained controversial for decades. Whereas numerous independent proxies of weathering in ocean sediments (e.g., Li, Sr, and Os isotopes) have been interpreted to indicate that the continental silicate weathering rate increased in the late Cenozoic, beryllium isotopes in seawater have stood out as an important exception. Beryllium isotopes have been interpreted to indicate stable continental weathering and/or denudation rates over the last 12 Myr. Here we present a Be cycle model whose results show that variations in the 9 Be weathering flux are counterbalanced by near-coastal scavenging while the cosmogenic 10 Be flux from the upper atmosphere stays constant. As a result, predicted seawater 10 Be/ 9 Be ratios remain nearly constant even when global denudation and Be weathering rates increase by three orders of magnitude. Moreover, 10 Be/ 9 Be records allow for up to an 11-fold increase in Be weathering and denudation rates over the late Cenozoic, consistent with estimates from other proxies. The large increase in continental weathering indicated by multiple proxies further suggests that the increased CO 2 consumption by continental weathering, driven by mountain-building events, was counterbalanced by other geological processes to prevent a runaway icehouse condition during the late Cenozoic. These processes could include enhanced carbonate dissolution via pyrite weathering, accelerated oxidation of fossil organic carbon, and/or reduced basalt weathering as the climate cooled.
Keyphrases
  • climate change
  • mass spectrometry
  • human health
  • polycyclic aromatic hydrocarbons
  • solid phase extraction