Article: High-precision 40Ar/ 39Ar age constraints on the basal Lanqi Formation and its implications for the origin of angiosperm plants

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TitleHigh-precision 40Ar/ 39Ar age constraints on the basal Lanqi Formation and its implications for the origin of angiosperm plants
AuthorsChang, Sc1
Zhang, H3
Renne, PR1 2
Fang, Y3
Keywords40Ar/ 39Ar
angiosperm
floral evolution
Jurassic
Lanqi Formation
Liaoning
Issue Date2009
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/epsl
CitationEarth And Planetary Science Letters, 2009, v. 279 n. 3-4, p. 212-221 [How to Cite?]
DOI: http://dx.doi.org/10.1016/j.epsl.2008.12.045
AbstractAbundant Mesozoic terrestrial fossils were discovered in the Haifanggou Formation and the overlying Lanqi Formation in northeastern China. The recent discovery of Schmeissneria sinensis from the Haifanggou Formation provides evidence that the origin of angiosperms could be much earlier than previously believed. 92 taxa of plant fossils from the Lanqi Formation provide unique opportunities to understand the floral evolution and its diversification in the Mesozoic. Here we present robust high-precision 40Ar/ 39Ar data of 160.7 ± 0.4 Ma and 158.7 ± 0.6 Ma for two tuffs from the lowest part of the Lanqi Formation near the main outcrop of floral fossils in Beipiao City, Liaoning, China. Our age results indicate the whole Lanqi Formation was deposited in the Late Jurassic; consequently, the underlying Haifanggou Formation and Schmeissneria sinensis are at least Middle Jurassic in age. Besides its importance for floral evolution, our high-precision age results for the basal Lanqi Formation indicate the paleoenvironment in the north margin of the North China Craton was dry and hot in the Late Jurassic. Moreover, the new age data for the basal Lanqi Formation suggest that the unearthed fossils from the Haifanggou Formation and Lanqi Formation should be equivalent to the Daohugou Biota in Inner Mongolia, China. © 2009 Elsevier B.V. All rights reserved.
ISSN0012-821X
2011 Impact Factor: 4.18
2011 SCImago Journal Rankings: 0.329
DOIhttp://dx.doi.org/10.1016/j.epsl.2008.12.045
ISI Accession Number IDWOS:000264743200007
Funding AgencyGrant Number
National Science Foundation of China40872015
Ann and Gordon Getty Foundation
Leroy Hill Opportunity Fund
Funding Information:

This research was supported by the National Science Foundation of China (40872015), the Ann and Gordon Getty Foundation, and the Leroy Hill Opportunity Fund. We thank Pei-ji Chen for suggesting the sampling location, Tim Becker for mass spectrometry assistance and three anonymous reviewers for their useful comments. Su-chin Chang thanks her dissertation committee member Kevin Padian for discussion.

ReferencesReferences in Scopus
DC Field
Value
dc.contributor.authorChang, Sc
dc.contributor.authorZhang, H
dc.contributor.authorRenne, PR
dc.contributor.authorFang, Y
dc.date.accessioned2011-04-04T06:35:24Z
dc.date.available2011-04-04T06:35:24Z
dc.date.issued2009
dc.description.abstractAbundant Mesozoic terrestrial fossils were discovered in the Haifanggou Formation and the overlying Lanqi Formation in northeastern China. The recent discovery of Schmeissneria sinensis from the Haifanggou Formation provides evidence that the origin of angiosperms could be much earlier than previously believed. 92 taxa of plant fossils from the Lanqi Formation provide unique opportunities to understand the floral evolution and its diversification in the Mesozoic. Here we present robust high-precision 40Ar/ 39Ar data of 160.7 ± 0.4 Ma and 158.7 ± 0.6 Ma for two tuffs from the lowest part of the Lanqi Formation near the main outcrop of floral fossils in Beipiao City, Liaoning, China. Our age results indicate the whole Lanqi Formation was deposited in the Late Jurassic; consequently, the underlying Haifanggou Formation and Schmeissneria sinensis are at least Middle Jurassic in age. Besides its importance for floral evolution, our high-precision age results for the basal Lanqi Formation indicate the paleoenvironment in the north margin of the North China Craton was dry and hot in the Late Jurassic. Moreover, the new age data for the basal Lanqi Formation suggest that the unearthed fossils from the Haifanggou Formation and Lanqi Formation should be equivalent to the Daohugou Biota in Inner Mongolia, China. © 2009 Elsevier B.V. All rights reserved.
dc.description.natureLink_to_subscribed_fulltext
dc.identifier.citationEarth And Planetary Science Letters, 2009, v. 279 n. 3-4, p. 212-221 [How to Cite?]
DOI: http://dx.doi.org/10.1016/j.epsl.2008.12.045
dc.identifier.doihttp://dx.doi.org/10.1016/j.epsl.2008.12.045
dc.identifier.epage221
dc.identifier.isiWOS:000264743200007
Funding AgencyGrant Number
National Science Foundation of China40872015
Ann and Gordon Getty Foundation
Leroy Hill Opportunity Fund
Funding Information:

This research was supported by the National Science Foundation of China (40872015), the Ann and Gordon Getty Foundation, and the Leroy Hill Opportunity Fund. We thank Pei-ji Chen for suggesting the sampling location, Tim Becker for mass spectrometry assistance and three anonymous reviewers for their useful comments. Su-chin Chang thanks her dissertation committee member Kevin Padian for discussion.

dc.identifier.issn0012-821X
2011 Impact Factor: 4.18
2011 SCImago Journal Rankings: 0.329
dc.identifier.issue3-4
dc.identifier.openurl
dc.identifier.scopuseid_2-s2.0-60949113742
dc.identifier.spage212
dc.identifier.urihttp://hdl.handle.net/10722/132845
dc.identifier.volume279
dc.languageeng
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/epsl
dc.publisher.placeNetherlands
dc.relation.ispartofEarth and Planetary Science Letters
dc.relation.referencesReferences in Scopus
dc.subject40Ar/ 39Ar
dc.subjectangiosperm
dc.subjectfloral evolution
dc.subjectJurassic
dc.subjectLanqi Formation
dc.subjectLiaoning
dc.titleHigh-precision 40Ar/ 39Ar age constraints on the basal Lanqi Formation and its implications for the origin of angiosperm plants
dc.typeArticle
Author Affiliations
  1. UC Berkeley
  2. Berkeley Geochronology Center
  3. Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences