Orbital and Millennial‐Scale Cycles Through the Hirnantian (Late Ordovician) in Southern China

The Hirnantian period, making the end of the Ordovician with significant mass extinctions and large ice‐sheets, is a critical interval for studying paleoclimate variations. This research represents the first cyclostratigraphic study of this period, utilizing high‐resolution (1 mm sampling rate) geoc...

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Veröffentlicht in:	Geochemistry, geophysics, geosystems : G3 geophysics, geosystems : G3, 2024-01, Vol.25 (1), p.n/a
Hauptverfasser:	Jin, Siding, Cao, Haiyang, Hou, Mingcai, Wang, Jiawei, Ma, Chao, Liu, Yu
Format:	Artikel
Sprache:	eng
Schlagworte:	cyclostratigraphy Eustatic changes Glaciation glacio‐eustatic processes Mass extinctions millennial band signal Obliquity Ordovician Paleoclimate Periodicities Principal components analysis sedimentary noise modeling the Hirnantian glaciation
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