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晚白垩世末期大型恐龙选择性灭绝机制——基于食物匮乏、氧压波动、地表软化的联合衰竭假说
宇 揣
Zenodo (CERN European Organization for Nuclear Research)20 Feb 2026Open access
PreprintOpen accessFrom the research index
晚白垩世末期大型恐龙选择性灭绝机制——基于食物匮乏、氧压波动、地表软化的联合衰竭假说
宇 揣 · Zenodo (CERN European Organization for Nuclear Research) · 20 Feb 2026
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白垩纪末期生物灭绝事件呈现显著的体型选择性,即巨型陆生恐龙全部灭绝,而小型陆生脊椎动物与鸟类得以存续。本文基于可实测的地质与化石证据,提出联合衰竭假说:晚白垩世末期植物生态系统崩溃(孢粉多样性下降约 45%)引发食物持续性短缺,伴随大气氧压小幅波动及陆地广泛沼泽化导致地表承载力降低,三者共同形成对巨型动物的生理筛选效应。大型恐龙因高能耗、高食物需求及软地表运动劣势,出现营养不良、体重下降、体力衰竭,最终突破生存阈值而灭绝;小型动物因生理负荷低、适应性强而不受致命影响。恐龙足迹形态变化可能反映体重波动,是个体营养状况的潜在指示。本假说可通过物理与生理实验验证真伪,与小行星撞击、火山活动等主流灾变理论兼容,可作为巨型动物选择性灭绝的核心补充机制。
Identifiers
- NobleID
- NI9P754W083R575S814
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- Published
- 20 Feb 2026
- Publisher
- European Organization for Nuclear Research
- Language
- CMN