Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis

Fil: Balseiro, Diego. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales; Argentina.

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Detalles Bibliográficos
Autores principales:	Balseiro, Diego, Powell, Matthew G.
Formato:	publishedVersion article
Lenguaje:	Inglés
Publicado:	2023
Materias:	Geología Edad de hielo del Paleozoico LPIA Paleobiology Database Macrostratigraphy
Acceso en línea:	http://hdl.handle.net/11086/547692 https://pubs.geoscienceworld.org/gsa/geology/article/48/2/118/575927/Carbonate-collapse-and-the-late-Paleozoic-ice-age https://rdu.unc.edu.ar/handle/11086/12914 https://doi.org/10.1130/G46858.1
Aporte de:	Repositorio Digital Universitario (UNC) de Universidad Nacional de Córdoba

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spelling	I10-R141-11086-5476922023-08-30T13:56:09Z Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis Balseiro, Diego Powell, Matthew G. Geología Edad de hielo del Paleozoico LPIA Paleobiology Database Macrostratigraphy info:eu-repo/semantics/publishedVersion Fil: Balseiro, Diego. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales; Argentina. Fil: Balseiro, Diego. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Fil: Powelll, Matthew G. Juniata College. Department of Geology; United States of America. The late Paleozoic ice age (LPIA) was characterized by persistently low diversity of marine invertebrates following a second-order mass extinction. Here, we used a data set of North American (paleotropical) fossil occurrences of brachiopod, bivalve, and coral genera from the Paleobiology Database, combined with lithologic data from Macrostrat, to demonstrate that low diversity was caused by the collapse of carbonate environments during the LPIA. After dividing the data by lithology, low diversity was evident only in carbonate environments, whereas diversity within siliciclastic environments actually increased during the LPIA, after a brief decline in the Serpukhovian (late Mississippian). Diversity patterns closely matched respective changes in the volume of carbonate and siliciclastic rocks. The contrasting patterns observed in the two environments suggest that habitat loss was a direct cause of changes in diversity, because other factors, such as temperature, would have affected genera in both environments. A causal relationship is also supported by the finding that diversity remained high in carbonate refugia (carbonate beds within majority-siliciclastic formations) until the Bashkirian, postdating the onset of icehouse conditions by ∼8 m.y. Our results provide a unifying, mechanistic explanation for the distinctive characteristics of the biotic impact, including its disproportionate effect on the tropical marine invertebrate fauna, prolonged recovery from extinction, low macroevolutionary rates during the recovery interval, and regional differences in its expression. info:eu-repo/semantics/publishedVersion Fil: Balseiro, Diego. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales; Argentina. Fil: Balseiro, Diego. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro de Investigaciones en Ciencias de la Tierra; Argentina. Fil: Powelll, Matthew G. Juniata College. Department of Geology; United States of America. 2023-06-07T18:32:08Z 2023-06-07T18:32:08Z 2020 article Balseiro, D., and Powell, M.G., 2020, Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis: Geology, v. 48, p. 118–122, https://doi.org/10.1130/G46858.1 http://hdl.handle.net/11086/547692 https://pubs.geoscienceworld.org/gsa/geology/article/48/2/118/575927/Carbonate-collapse-and-the-late-Paleozoic-ice-age https://rdu.unc.edu.ar/handle/11086/12914 https://doi.org/10.1130/G46858.1 eng 11086/12914 Attribution-NonCommercial-NoDerivatives 4.0 Internacional http://creativecommons.org/licenses/by-nc-nd/4.0/
institution	Universidad Nacional de Córdoba
institution_str	I-10
repository_str	R-141
collection	Repositorio Digital Universitario (UNC)
language	Inglés
topic	Geología Edad de hielo del Paleozoico LPIA Paleobiology Database Macrostratigraphy
spellingShingle	Geología Edad de hielo del Paleozoico LPIA Paleobiology Database Macrostratigraphy Balseiro, Diego Powell, Matthew G. Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
topic_facet	Geología Edad de hielo del Paleozoico LPIA Paleobiology Database Macrostratigraphy
description	Fil: Balseiro, Diego. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales; Argentina.
format	publishedVersion article
author	Balseiro, Diego Powell, Matthew G.
author_facet	Balseiro, Diego Powell, Matthew G.
author_sort	Balseiro, Diego
title	Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_short	Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_full	Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_fullStr	Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_full_unstemmed	Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_sort	carbonate collapse and the late paleozoic ice age marine biodiversity crisis
publishDate	2023
url	http://hdl.handle.net/11086/547692 https://pubs.geoscienceworld.org/gsa/geology/article/48/2/118/575927/Carbonate-collapse-and-the-late-Paleozoic-ice-age https://rdu.unc.edu.ar/handle/11086/12914 https://doi.org/10.1130/G46858.1
work_keys_str_mv	AT balseirodiego carbonatecollapseandthelatepaleozoiciceagemarinebiodiversitycrisis AT powellmatthewg carbonatecollapseandthelatepaleozoiciceagemarinebiodiversitycrisis
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Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis

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