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Updated: May 6, 2026

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Thermal Limits Determination for Zooplankton Using a Heat Block
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早期古世时期,西南太平洋的温度演变
Peter K Bijl1, Stefan Schouten, Appy Sluijs
1Palaeoecology, Institute of Environmental Biology, Faculty of Science, Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, The Netherlands. p.k.bijl@uu.nl
Nature
|October 9, 2009
概括
早期的欧热带在赤道和极地之间温度差异很小. 后来的伊欧纪冷却显著增加了这些梯度,导致南极冰盖的形成.
科学领域:
- 古气候学 古气候学
- 海洋地质 海洋地质学
背景情况:
- 纪气候转型,特别是纪-奥利古纪冷却,对于理解地球气候敏感性至关重要.
- 有限的高度温度记录阻碍了对全球冷却事件的充分理解.
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