Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution
- Autores
- Feild, Taylor S.; Brodribb, Timothy J.; Iglesias, Ari; Chatelet, David S.; Baresch, Andres; Upchurch Jr., Garland R.; Gomez, Bernard; Mohr, Barbara A. R.; Coiffard, Clement; Kvacek, Jiri; Jaramillo, Carlos
- Año de publicación
- 2011
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The flowering plants that dominate modern vegetation possess leaf gas exchange potentials that far exceed those of all other living or extinct plants. The great divide in maximal ability to exchange CO 2 for water between leaves of nonangiosperms and angiosperms forms the mechanistic foundation for speculation about how angiosperms drove sweeping ecological and biogeochemical change during the Cretaceous. However, there is no empirical evidence that angiosperms evolved highly photosynthetically active leaves during the Cretaceous. Using vein density (D V ) measurements of fossil angiosperm leaves, we show that the leaf hydraulic capacities of angiosperms escalated severalfold during the Cretaceous. During the first 30 million years of angiosperm leaf evolution, angiosperm leaves exhibited uniformly low vein D V that overlapped the D V range of dominant Early Cretaceous ferns and gymnosperms. Fossil angiosperm vein densities reveal a subsequent biphasic increase in D V . During the first mid-Cretaceous surge, angiosperm D V first surpassed the upper bound of D V limits for nonangiosperms. However, the upper limits of D V typical of modern megathermal rainforest trees first appear during a second wave of increased D V during the Cretaceous-Tertiary transition. Thus, our findings provide fossil evidence for the hypothesis that significant ecosystem change brought about by angiosperms lagged behind the Early Cretaceous taxonomic diversification of angiosperms.
Facultad de Ciencias Naturales y Museo - Materia
-
Ciencias Naturales
Angiosperm evolution
Plant evolution
Transpiration
Tropical rainforest
Venation - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/84076
Ver los metadatos del registro completo
id |
SEDICI_466384042912e9b46e7b78f9dcc4936d |
---|---|
oai_identifier_str |
oai:sedici.unlp.edu.ar:10915/84076 |
network_acronym_str |
SEDICI |
repository_id_str |
1329 |
network_name_str |
SEDICI (UNLP) |
spelling |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolutionFeild, Taylor S.Brodribb, Timothy J.Iglesias, AriChatelet, David S.Baresch, AndresUpchurch Jr., Garland R.Gomez, BernardMohr, Barbara A. R.Coiffard, ClementKvacek, JiriJaramillo, CarlosCiencias NaturalesAngiosperm evolutionPlant evolutionTranspirationTropical rainforestVenationThe flowering plants that dominate modern vegetation possess leaf gas exchange potentials that far exceed those of all other living or extinct plants. The great divide in maximal ability to exchange CO 2 for water between leaves of nonangiosperms and angiosperms forms the mechanistic foundation for speculation about how angiosperms drove sweeping ecological and biogeochemical change during the Cretaceous. However, there is no empirical evidence that angiosperms evolved highly photosynthetically active leaves during the Cretaceous. Using vein density (D V ) measurements of fossil angiosperm leaves, we show that the leaf hydraulic capacities of angiosperms escalated severalfold during the Cretaceous. During the first 30 million years of angiosperm leaf evolution, angiosperm leaves exhibited uniformly low vein D V that overlapped the D V range of dominant Early Cretaceous ferns and gymnosperms. Fossil angiosperm vein densities reveal a subsequent biphasic increase in D V . During the first mid-Cretaceous surge, angiosperm D V first surpassed the upper bound of D V limits for nonangiosperms. However, the upper limits of D V typical of modern megathermal rainforest trees first appear during a second wave of increased D V during the Cretaceous-Tertiary transition. Thus, our findings provide fossil evidence for the hypothesis that significant ecosystem change brought about by angiosperms lagged behind the Early Cretaceous taxonomic diversification of angiosperms.Facultad de Ciencias Naturales y Museo2011info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf8363-8366http://sedici.unlp.edu.ar/handle/10915/84076enginfo:eu-repo/semantics/altIdentifier/issn/0027-8424info:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.1014456108info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-15T11:08:02Zoai:sedici.unlp.edu.ar:10915/84076Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-15 11:08:02.827SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
title |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
spellingShingle |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution Feild, Taylor S. Ciencias Naturales Angiosperm evolution Plant evolution Transpiration Tropical rainforest Venation |
title_short |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
title_full |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
title_fullStr |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
title_full_unstemmed |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
title_sort |
Fossil evidence for Cretaceous escalation in angiosperm leaf vein evolution |
dc.creator.none.fl_str_mv |
Feild, Taylor S. Brodribb, Timothy J. Iglesias, Ari Chatelet, David S. Baresch, Andres Upchurch Jr., Garland R. Gomez, Bernard Mohr, Barbara A. R. Coiffard, Clement Kvacek, Jiri Jaramillo, Carlos |
author |
Feild, Taylor S. |
author_facet |
Feild, Taylor S. Brodribb, Timothy J. Iglesias, Ari Chatelet, David S. Baresch, Andres Upchurch Jr., Garland R. Gomez, Bernard Mohr, Barbara A. R. Coiffard, Clement Kvacek, Jiri Jaramillo, Carlos |
author_role |
author |
author2 |
Brodribb, Timothy J. Iglesias, Ari Chatelet, David S. Baresch, Andres Upchurch Jr., Garland R. Gomez, Bernard Mohr, Barbara A. R. Coiffard, Clement Kvacek, Jiri Jaramillo, Carlos |
author2_role |
author author author author author author author author author author |
dc.subject.none.fl_str_mv |
Ciencias Naturales Angiosperm evolution Plant evolution Transpiration Tropical rainforest Venation |
topic |
Ciencias Naturales Angiosperm evolution Plant evolution Transpiration Tropical rainforest Venation |
dc.description.none.fl_txt_mv |
The flowering plants that dominate modern vegetation possess leaf gas exchange potentials that far exceed those of all other living or extinct plants. The great divide in maximal ability to exchange CO 2 for water between leaves of nonangiosperms and angiosperms forms the mechanistic foundation for speculation about how angiosperms drove sweeping ecological and biogeochemical change during the Cretaceous. However, there is no empirical evidence that angiosperms evolved highly photosynthetically active leaves during the Cretaceous. Using vein density (D V ) measurements of fossil angiosperm leaves, we show that the leaf hydraulic capacities of angiosperms escalated severalfold during the Cretaceous. During the first 30 million years of angiosperm leaf evolution, angiosperm leaves exhibited uniformly low vein D V that overlapped the D V range of dominant Early Cretaceous ferns and gymnosperms. Fossil angiosperm vein densities reveal a subsequent biphasic increase in D V . During the first mid-Cretaceous surge, angiosperm D V first surpassed the upper bound of D V limits for nonangiosperms. However, the upper limits of D V typical of modern megathermal rainforest trees first appear during a second wave of increased D V during the Cretaceous-Tertiary transition. Thus, our findings provide fossil evidence for the hypothesis that significant ecosystem change brought about by angiosperms lagged behind the Early Cretaceous taxonomic diversification of angiosperms. Facultad de Ciencias Naturales y Museo |
description |
The flowering plants that dominate modern vegetation possess leaf gas exchange potentials that far exceed those of all other living or extinct plants. The great divide in maximal ability to exchange CO 2 for water between leaves of nonangiosperms and angiosperms forms the mechanistic foundation for speculation about how angiosperms drove sweeping ecological and biogeochemical change during the Cretaceous. However, there is no empirical evidence that angiosperms evolved highly photosynthetically active leaves during the Cretaceous. Using vein density (D V ) measurements of fossil angiosperm leaves, we show that the leaf hydraulic capacities of angiosperms escalated severalfold during the Cretaceous. During the first 30 million years of angiosperm leaf evolution, angiosperm leaves exhibited uniformly low vein D V that overlapped the D V range of dominant Early Cretaceous ferns and gymnosperms. Fossil angiosperm vein densities reveal a subsequent biphasic increase in D V . During the first mid-Cretaceous surge, angiosperm D V first surpassed the upper bound of D V limits for nonangiosperms. However, the upper limits of D V typical of modern megathermal rainforest trees first appear during a second wave of increased D V during the Cretaceous-Tertiary transition. Thus, our findings provide fossil evidence for the hypothesis that significant ecosystem change brought about by angiosperms lagged behind the Early Cretaceous taxonomic diversification of angiosperms. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://sedici.unlp.edu.ar/handle/10915/84076 |
url |
http://sedici.unlp.edu.ar/handle/10915/84076 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/issn/0027-8424 info:eu-repo/semantics/altIdentifier/doi/10.1073/pnas.1014456108 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
dc.format.none.fl_str_mv |
application/pdf 8363-8366 |
dc.source.none.fl_str_mv |
reponame:SEDICI (UNLP) instname:Universidad Nacional de La Plata instacron:UNLP |
reponame_str |
SEDICI (UNLP) |
collection |
SEDICI (UNLP) |
instname_str |
Universidad Nacional de La Plata |
instacron_str |
UNLP |
institution |
UNLP |
repository.name.fl_str_mv |
SEDICI (UNLP) - Universidad Nacional de La Plata |
repository.mail.fl_str_mv |
alira@sedici.unlp.edu.ar |
_version_ |
1846064136937537536 |
score |
13.22299 |