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Updated: Jun 18, 2025

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
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在白纪晚期,鱼类耳石结合的有机物质中发生了同位素转移

Zixuan C Rao1,2, Jessica A Lueders-Dumont1,3,4, Gary L Stringer5

  • 1Department of Geosciences, Princeton University, Princeton, NJ 08544.

Proceedings of the National Academy of Sciences of the United States of America
|July 29, 2024
PubMed
概括

化石鱼耳石中的同位素揭示了白纪晚期的环境变化. 温暖的气候与较低的同位素值相关,这表明海洋缺氧区域与全球温度之间存在长期联系.

关键词:
晚期白纪晚期的白纪化石鱼的耳岩石 化石鱼的耳岩石海洋生物地球化学 海洋生物地球化学的同位素是的同位素.

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