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.

Bibliographic Details
Main Authors: Balseiro, Diego, Powell, Matthew G.
Format: info:eu-repo/semantics/publishedVersion
Language:eng
Published: 2023
Subjects:
Online Access: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
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author Balseiro, Diego
Powell, Matthew G.
author_facet Balseiro, Diego
Powell, Matthew G.
author_sort Balseiro, Diego
collection Repositorio Digital Universitario
description Fil: Balseiro, Diego. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales; Argentina.
format info:eu-repo/semantics/publishedVersion
id rdu-unc.547692
institution Universidad Nacional de Cordoba
language eng
publishDate 2023
record_format dspace
spelling rdu-unc.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/
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
title 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_short Carbonate collapse and the late Paleozoic ice age marine biodiversity crisis
title_sort carbonate collapse and the late paleozoic ice age marine biodiversity crisis
topic Geología
Edad de hielo del Paleozoico
LPIA
Paleobiology Database
Macrostratigraphy
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
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