Article (Scientific journals)
Dynamic Late Ordovician climate responses: The cascading effects of expanding continental ice?
Forsythe, Ian J.; Brett, Carlton E.; Sullivan, Nicholas B. et al.
2026 • In Geology
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Abstract :
[en] The interplay between astronomical forcing, continental ice volume, and biotic immigration is well studied in the Cenozoic, and documentation of such connections in the Paleozoic is rapidly increasing. Herein, we present analyses from late Katian subtropical marine deposits, revealing a transition from obliquity- (∼33.8 ± 0.46 k.y.) and precession- (∼17−22 k.y.) dominated sedimentation to a regime dominated by obliquity and short eccentricity (∼93−125 k.y.). We term this shift the late Katian transition. Transition from precession- to short eccentricity−dominated sedimentary cycles suggests expansion of ice sheets over Gondwana. This shift precedes a major episode of faunal immigration in Laurentia, which may have been facilitated by this climatic transition.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Forsythe, Ian J.;  1H.N. Fisk Laboratory of Sedimentology, Department of Geosciences, University of Cincinnati, Cincinnati, Ohio 45221, USA
Brett, Carlton E.;  1H.N. Fisk Laboratory of Sedimentology, Department of Geosciences, University of Cincinnati, Cincinnati, Ohio 45221, USA
Sullivan, Nicholas B.;  2Earth and Environmental Systems Institute, Pennsylvania State University, University Park, Pennsylvania 16802, USA
Stigall, Alycia L.;  3Department of Earth, Environmental, and Planetary Sciences, University of Tennessee, Knoxville, Tennessee 37996, USA
Da Silva, Anne-Christine  ;  Université de Liège - ULiège > Département de géologie
Language :
English
Title :
Dynamic Late Ordovician climate responses: The cascading effects of expanding continental ice?
Publication date :
20 April 2026
Journal title :
Geology
ISSN :
0091-7613
eISSN :
1943-2682
Publisher :
Geological Society of America
Peer reviewed :
Peer Reviewed verified by ORBi
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since 22 June 2026

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