Demise of Organic Matter–Rich Facies and Changing Paleoenvironmental Conditions Associated with the End of Carbon Isotope Segment C5 of Oceanic Anoxic Event 1a in the North and Northeastern Iberian Peninsula-Reference-Cited by-同舟云学术

Demise of Organic Matter–Rich Facies and Changing Paleoenvironmental Conditions Associated with the End of Carbon Isotope Segment C5 of Oceanic Anoxic Event 1a in the North and Northeastern Iberian Peninsula

Published:2022-03-01 Issue:2 Volume:130 Page:133-170
ISSN:0022-1376
Container-title:The Journal of Geology
language:en
Short-container-title:The Journal of Geology

Author:

Socorro Jander,Maurrasse Florentin J.-M. R.

Publisher

University of Chicago Press

Subject

Geology

Link

https://www.journals.uchicago.edu/doi/pdf/10.1086/718834

Reference270 articles.

1. Aptian bio-events—an integrated biostratigraphic analysis of the Almadich Formation, Inner Prebetic Domain, SE Spain

2. Late Barremian–early Aptian dark facies of the Subbetic (Betic Cordillera, southern Spain): Calcareous nannofossil quantitative analyses, chemostratigraphy and palaeoceanographic reconstructions

3. Integrated biostratigraphy (calcareous nannofossils, planktonic foraminifera, and radiolarians) of an uppermost Barremian–lower Aptian pelagic succession in the Subbetic Basin (southern Spain)

4. Vertical migratory response of benthic foraminifera to controlled oxygen concentrations in an experimental mesocosm

5. Timing and magnitude of early Aptian extreme warming: Unraveling primary δ18O variation in indurated pelagic carbonates at Deep Sea Drilling Project Site 463, central Pacific Ocean

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1. Geochemical factors associated with deposition of lower Aptian organic-rich sediments during OAE1a in the Basque-Cantabrian Basin, northern Spain;Frontiers in Geochemistry;2023-03-08