Regional geological background [19].

<div><p>The Late Ordovician and Early Silurian transition is an important period of geological evolution, attracting increasing attentions. However, the cause for the biotic recovery from the end-Ordovician mass extinction has remained controversial. A set of black shales deposited in th...

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محفوظ في:

التفاصيل البيبلوغرافية
المؤلف الرئيسي:	Zhibo Zhang (22521919) (author)
مؤلفون آخرون:	Jiaming Zhang (346789) (author), Hengye Wei (7116488) (author), Huan Li (120482) (author), Yinghai Guo (22521922) (author), Chunlin Zeng (11993750) (author)
منشور في:	2025
الموضوعات:	Biochemistry Evolutionary Biology Ecology Developmental Biology Environmental Sciences not elsewhere classified Astronomical and Space Sciences not elsewhere classified without obvious change lmx fm .) gradually decreases upward black shales deposited attracting increasing attentions clay mineral composition paleoclimate evolution process global paleoclimate evolution early silurian transition early silurian recorded earliest silurian following smectite mixed layer ordovician mass extinction cold climatic conditions clay minerals evidences biotic recovery started climate evolution period early silurian climate evolution clay minerals biotic recovery silurian epoch geological evolution late ordovician important period following conclusion extinction event biological recovery subordinate minerals montmorillonite minerals xlink "> whole world well yucan tibet area three stages study results stage 3 stage 2 stage 1 smectite illit sichuan basin results show remained controversial mall amount mainly composed longmaxi formation longmaxi age hot rhythms hirnantian glaciation e .,
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Regional geological background [19].

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