使用碳酸结合同位素重建Phanerozoic气候,并对海水的氧同位素组成产生影响

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Nivedita Thiagarajan1, Aivo Lepland2,3,4, Uri Ryb5

  • 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125.

Proceedings of the National Academy of Sciences of the United States of America
|August 26, 2024
PubMed
概括

海洋沉积岩的氧同位素比率自古生物早期以来增加了8%. 新的聚合同位素分析揭示了较低的奥尔多维纪海水值,这表明气候记录需要重新评估二代和温度假设.

关键词:
在奥尔多维纪 (Ordovician) 时期.凝聚的同位素是凝聚在一起的.氧的同位素是氧的同位素.古代气候是一种古气候.

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