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Upper cretaceous marl-limestone sequences of Alabama: Possible products of sea-level change, not climate forcing

Journal Article · · Geology; (USA)

Marl-limestone sequences in the Arcola Limestone Member (Campanian) of Alabama have been cited as key examples of climate-forced sedimentation resulting from cycles of production and dilution. However, sedimentologic and stratigraphic data from the Arcola presented herein suggest a more probable link between short-term sea-level changes and marl-limestone sequence genesis. Either relative sea-level change caused by intraplate deformation or short-term eustatic sea-level change is suggested as the causative mechanism for deposition of the marl-limestone sequences.

OSTI ID:
6314748
Journal Information:
Geology; (USA), Journal Name: Geology; (USA) Vol. 18:1; ISSN GLGYB; ISSN 0091-7613
Country of Publication:
United States
Language:
English

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