A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana

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This work was supported by grants from the National Science Foundation (EAR-8916826) and the Research Foundation of the University of Pennsylvania to H.W.P., grants from the Consejo Nacional de Ciencia y Tecnologia (CONCYTEC) and the Alexander von Humboldt-Stiftung to V.A., and grants from the Conse...

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Detalles Bibliográficos
Autores: Pfefferkorn H.W., Alleman V., Iannuzzi R.
Formato: revisión
Fecha de Publicación:2014
Institución:Consejo Nacional de Ciencia Tecnología e Innovación
Repositorio:CONCYTEC-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.concytec.gob.pe:20.500.12390/876
Enlace del recurso:https://hdl.handle.net/20.500.12390/876
https://doi.org/10.1016/j.gr.2013.08.022
Nivel de acceso:acceso abierto
Materia:Visean
Greenhouse interval
lPaleobotany
Gondwana
Long-distance dispersal
https://purl.org/pe-repo/ocde/ford#1.05.10
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network_acronym_str CONC
network_name_str CONCYTEC-Institucional
repository_id_str 4689
dc.title.none.fl_str_mv A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
title A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
spellingShingle A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
Pfefferkorn H.W.
Visean
Greenhouse interval
lPaleobotany
Gondwana
Long-distance dispersal
https://purl.org/pe-repo/ocde/ford#1.05.10
title_short A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
title_full A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
title_fullStr A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
title_full_unstemmed A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
title_sort A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
author Pfefferkorn H.W.
author_facet Pfefferkorn H.W.
Alleman V.
Iannuzzi R.
author_role author
author2 Alleman V.
Iannuzzi R.
author2_role author
author
dc.contributor.author.fl_str_mv Pfefferkorn H.W.
Alleman V.
Iannuzzi R.
dc.subject.none.fl_str_mv Visean
topic Visean
Greenhouse interval
lPaleobotany
Gondwana
Long-distance dispersal
https://purl.org/pe-repo/ocde/ford#1.05.10
dc.subject.es_PE.fl_str_mv Greenhouse interval
lPaleobotany
Gondwana
Long-distance dispersal
dc.subject.ocde.none.fl_str_mv https://purl.org/pe-repo/ocde/ford#1.05.10
description This work was supported by grants from the National Science Foundation (EAR-8916826) and the Research Foundation of the University of Pennsylvania to H.W.P., grants from the Consejo Nacional de Ciencia y Tecnologia (CONCYTEC) and the Alexander von Humboldt-Stiftung to V.A., and grants from the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq-PQ305687/2010-7) to R.I. We acknowledge the interest and support by former and current Directors of the Paracas Reserva for our paleontological studies; permissions to work in the Reserva Nacional de Paracas by the Instituto Nacional de Recursos Naturales, INRENA; and former students of the Universidad Ricardo Palma for their assistance in the field. Grace Maloney, Dan Ke, and Joanna Karaman prepared the figures.
publishDate 2014
dc.date.accessioned.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.available.none.fl_str_mv 2024-05-30T23:13:38Z
dc.date.issued.fl_str_mv 2014
dc.type.none.fl_str_mv info:eu-repo/semantics/review
format review
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12390/876
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1016/j.gr.2013.08.022
dc.identifier.scopus.none.fl_str_mv 2-s2.0-84896394380
url https://hdl.handle.net/20.500.12390/876
https://doi.org/10.1016/j.gr.2013.08.022
identifier_str_mv 2-s2.0-84896394380
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv Gondwana Research
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:CONCYTEC-Institucional
instname:Consejo Nacional de Ciencia Tecnología e Innovación
instacron:CONCYTEC
instname_str Consejo Nacional de Ciencia Tecnología e Innovación
instacron_str CONCYTEC
institution CONCYTEC
reponame_str CONCYTEC-Institucional
collection CONCYTEC-Institucional
repository.name.fl_str_mv Repositorio Institucional CONCYTEC
repository.mail.fl_str_mv repositorio@concytec.gob.pe
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spelling Publicationrp02043500rp02041500rp02316600Pfefferkorn H.W.Alleman V.Iannuzzi R.2024-05-30T23:13:38Z2024-05-30T23:13:38Z2014https://hdl.handle.net/20.500.12390/876https://doi.org/10.1016/j.gr.2013.08.0222-s2.0-84896394380This work was supported by grants from the National Science Foundation (EAR-8916826) and the Research Foundation of the University of Pennsylvania to H.W.P., grants from the Consejo Nacional de Ciencia y Tecnologia (CONCYTEC) and the Alexander von Humboldt-Stiftung to V.A., and grants from the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq-PQ305687/2010-7) to R.I. We acknowledge the interest and support by former and current Directors of the Paracas Reserva for our paleontological studies; permissions to work in the Reserva Nacional de Paracas by the Instituto Nacional de Recursos Naturales, INRENA; and former students of the Universidad Ricardo Palma for their assistance in the field. Grace Maloney, Dan Ke, and Joanna Karaman prepared the figures.The late Paleozoic ice age (LPIA) is the closest example that can be compared with current climate conditions. Near the beginning of the LPIA fossil plants of Mississippian (late Visean to earliest Serpukhovian) age indicate a widespread frost-free climate in a wide belt on Gondwana indicating an interval of greenhouse conditions between the earlier Visean and later Serpukhovian icehouse times. This warm-temperate floral belt has been named the Paraca floral belt after the locality on the Peruvian coast where it was first recognized.Consejo Nacional de Ciencia, Tecnología e Innovación Tecnológica - ConcytecengElsevierGondwana Researchinfo:eu-repo/semantics/openAccessViseanGreenhouse interval-1lPaleobotany-1Gondwana-1Long-distance dispersal-1https://purl.org/pe-repo/ocde/ford#1.05.10-1A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwanainfo:eu-repo/semantics/reviewreponame:CONCYTEC-Institucionalinstname:Consejo Nacional de Ciencia Tecnología e Innovacióninstacron:CONCYTEC20.500.12390/876oai:repositorio.concytec.gob.pe:20.500.12390/8762024-05-30 15:49:50.565http://purl.org/coar/access_right/c_14cbinfo:eu-repo/semantics/closedAccessmetadata only accesshttps://repositorio.concytec.gob.peRepositorio Institucional CONCYTECrepositorio@concytec.gob.pe#PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE##PLACEHOLDER_PARENT_METADATA_VALUE#<Publication xmlns="https://www.openaire.eu/cerif-profile/1.1/" id="c5e76ff8-bef8-45e7-9a33-aec22e573e52"> <Type xmlns="https://www.openaire.eu/cerif-profile/vocab/COAR_Publication_Types">http://purl.org/coar/resource_type/c_1843</Type> <Language>eng</Language> <Title>A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana</Title> <PublishedIn> <Publication> <Title>Gondwana Research</Title> </Publication> </PublishedIn> <PublicationDate>2014</PublicationDate> <DOI>https://doi.org/10.1016/j.gr.2013.08.022</DOI> <SCP-Number>2-s2.0-84896394380</SCP-Number> <Authors> <Author> <DisplayName>Pfefferkorn H.W.</DisplayName> <Person id="rp02043" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Alleman V.</DisplayName> <Person id="rp02041" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> <Author> <DisplayName>Iannuzzi R.</DisplayName> <Person id="rp02316" /> <Affiliation> <OrgUnit> </OrgUnit> </Affiliation> </Author> </Authors> <Editors> </Editors> <Publishers> <Publisher> <DisplayName>Elsevier</DisplayName> <OrgUnit /> </Publisher> </Publishers> <Keyword>Visean</Keyword> <Keyword>Greenhouse interval</Keyword> <Keyword>lPaleobotany</Keyword> <Keyword>Gondwana</Keyword> <Keyword>Long-distance dispersal</Keyword> <Abstract>The late Paleozoic ice age (LPIA) is the closest example that can be compared with current climate conditions. Near the beginning of the LPIA fossil plants of Mississippian (late Visean to earliest Serpukhovian) age indicate a widespread frost-free climate in a wide belt on Gondwana indicating an interval of greenhouse conditions between the earlier Visean and later Serpukhovian icehouse times. This warm-temperate floral belt has been named the Paraca floral belt after the locality on the Peruvian coast where it was first recognized.</Abstract> <Access xmlns="http://purl.org/coar/access_right" > </Access> </Publication> -1
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A greenhouse interval between icehouse times: Climate change, long-distance plant dispersal, and plate motion in the Mississippian (late Visean-earliest Serpukhovian) of Gondwana
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