日本地球惑星科学連合2022年大会

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セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS18] 古気候・古海洋変動

2022年5月27日(金) 10:45 〜 12:15 304 (幕張メッセ国際会議場)

コンビーナ:長谷川 精(高知大学理工学部)、コンビーナ:岡崎 裕典(九州大学大学院理学研究院地球惑星科学部門)、山本 彬友(国立研究開発法人 海洋研究開発機構)、コンビーナ:山崎 敦子(九州大学大学院理学研究院)、座長:岡崎 裕典(九州大学大学院理学研究院地球惑星科学部門)

11:30 〜 11:45

[MIS18-20] Can Mg and Li isotopes in the authigenic and detrital fractions of sediments be used to trace paleoweathering? Case study: The EOT

*Adam David Sproson1Toshihiro Yoshimura1Takahiro AZE2Shigeyuki Wakaki3Tsuyoshi Ishikawa3Yusuke Yokoyama1,2Naohiko Ohkouchi1 (1.Biogeochemistry Research Center, Japan Agency for Marine-Earth Science and Technology、2.Atmosphere and Ocean Research Institute, The University of Tokyo、3.Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology)

キーワード:Magnesium isotopes, Lithium isotopes, The Eocene-Oligocene Transition, Silicate weathering

Future warming beyond 2oC could lead to the crossing of a threshold beyond which, positive feedbacks within the Earth System could create a “Hothouse Earth” [1]. Understanding the interplay of feedback mechanisms is therefore of utmost importance to predicting future climate change. On million-year timescales, the hydrolysis of silicate minerals and subsequent precipitation of carbonate minerals in the ocean acts as a negative feedback within the carbon-cycle [2]. On shorter, more relevant, timescales, the production of fine-grained material and associated subglacial chemical weathering during expansion and contraction of glaciers may influence global atmospheric CO2 and temperature [3].

The Eocene-Oligocene Transition (EOT; ~34 Ma) marks the appearance of large Antarctic ice sheets associated with a large surge in erosion as recorded by Nd isotopes, Pb isotopes, and clay mineralogy [4, 5]. However, the response of chemical silicate weathering is not well understood. Here, we present Mg isotope (d26Mg), Li isotope (d7Li), rare-earth element (REE), and major element measurements for the authigenic and detrital phases of marine sediments from ODP Site 738 off the coast of East Antarctica (Kerguelen Plateau).

The d26Mg and d7Li records of the authigenic and silicate phases from Site 738 display a large fractionation during the EOT, in a similar manner to previous Pb and Nd isotope records. This fractionation could be due to one of many processes: (1) increase in weathering intensity; (2) lower clay formation; (3) carbonate weathering; and (4) grain size variation. Changing the method used to extract the authigenic and silicate phase may allow us to discriminate between these processes. Overall, our new data sets suggest continental ice sheet expansion over Antarctica led to increased silicate weathering, atmospheric CO2 drawdown and further cooling. Such feedbacks may help reverse future warming as ice sheets begin to retreat.

[1] Steffen et al. (2018) PNAS 115, 8252-8259. [2] Berner (2006) GCA 70, 5653-5664. [3] Bluth & Erel (1995) Nature 373, 415-418. [4] Basak & Martin (2013) Nat. Geosci. 6, 121-124. [5] Scher et al. (2011) Geology 39, 383-386.