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Reinvestigation of the occurrence of cutan in plants: implications for the leaf fossil record
Cutan, a resistant non-hydrolyzable aliphatic biopolymer, was first reported in the cuticle of Agave americana and has generally been considered ubiquitous in leaf cuticles along with the structural biopolyester cutin. Because leaves and cuticles in the fossil record almost always have an aliphatic...
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Published in: | Paleobiology 2006-09, Vol.32 (3), p.432-449 |
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description | Cutan, a resistant non-hydrolyzable aliphatic biopolymer, was first reported in the cuticle of Agave americana and has generally been considered ubiquitous in leaf cuticles along with the structural biopolyester cutin. Because leaves and cuticles in the fossil record almost always have an aliphatic composition, it was argued that selective preservation of cutan played an important role in leaf preservation. However, the analysis of leaves using chemical degradation techniques involving hydrolysis to test for the presence of cutan reveals that it is absent in 16 of 19 taxa (angiosperm and gymnosperm), including many previously reported to contain cutan on the basis of pyrolysis data. Cutan is clearly much less widespread in leaves than previously thought, and its presence or absence does not exert any major bias on the preservation of leaves in the fossil record. In the absence of cutan, other constituents—cutin, plant waxes, and internal plant lipids—are incorporated into the geomacromolecule and contribute to the formation of a resistant aliphatic polymer by in situ polymerization during diagenesis. |
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Cutan is clearly much less widespread in leaves than previously thought, and its presence or absence does not exert any major bias on the preservation of leaves in the fossil record. In the absence of cutan, other constituents—cutin, plant waxes, and internal plant lipids—are incorporated into the geomacromolecule and contribute to the formation of a resistant aliphatic polymer by in situ polymerization during diagenesis.</description><identifier>ISSN: 0094-8373</identifier><identifier>EISSN: 1938-5331</identifier><identifier>DOI: 10.1666/05038.1</identifier><identifier>CODEN: PALBBM</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Angiospermae ; Animal cuticle ; cutan ; experimental studies ; fossil record ; Fossils ; gas chromatograms ; Geochemistry ; Gymnospermae ; Hydrolysis ; laboratory studies ; Leaves ; Lignin ; Lipids ; living taxa ; mass spectra ; modern analogs ; organic compounds ; Paleobotany ; paleoecology ; physiology ; Plant cuticle ; Plantae ; Plants ; preservation ; Pyrolysis ; s ; spectra ; Spermatophyta</subject><ispartof>Paleobiology, 2006-09, Vol.32 (3), p.432-449</ispartof><rights>The Paleontological Society</rights><rights>Copyright © The Paleontological Society</rights><rights>GeoRef, Copyright 2020, American Geosciences Institute. 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Abstract, Copyright, The Paleontological Society</rights><rights>Copyright 2006 The Paleontological Society</rights><rights>Copyright Paleontological Society Summer 2006</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a462t-168f6bbca1bd0ffbed9d3fb26aa3516ceccba6c327208037b9d34e735e3ad16e3</citedby><cites>FETCH-LOGICAL-a462t-168f6bbca1bd0ffbed9d3fb26aa3516ceccba6c327208037b9d34e735e3ad16e3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/4096960$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4096960$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,58238,58471</link.rule.ids></links><search><creatorcontrib>Gupta, Neal S</creatorcontrib><creatorcontrib>Collinson, Margaret E</creatorcontrib><creatorcontrib>Briggs, Derek E. G</creatorcontrib><creatorcontrib>Evershed, Richard P</creatorcontrib><creatorcontrib>Pancost, Richard D</creatorcontrib><title>Reinvestigation of the occurrence of cutan in plants: implications for the leaf fossil record</title><title>Paleobiology</title><addtitle>Paleobiology</addtitle><description>Cutan, a resistant non-hydrolyzable aliphatic biopolymer, was first reported in the cuticle of Agave americana and has generally been considered ubiquitous in leaf cuticles along with the structural biopolyester cutin. Because leaves and cuticles in the fossil record almost always have an aliphatic composition, it was argued that selective preservation of cutan played an important role in leaf preservation. However, the analysis of leaves using chemical degradation techniques involving hydrolysis to test for the presence of cutan reveals that it is absent in 16 of 19 taxa (angiosperm and gymnosperm), including many previously reported to contain cutan on the basis of pyrolysis data. Cutan is clearly much less widespread in leaves than previously thought, and its presence or absence does not exert any major bias on the preservation of leaves in the fossil record. In the absence of cutan, other constituents—cutin, plant waxes, and internal plant lipids—are incorporated into the geomacromolecule and contribute to the formation of a resistant aliphatic polymer by in situ polymerization during diagenesis.</description><subject>Angiospermae</subject><subject>Animal cuticle</subject><subject>cutan</subject><subject>experimental studies</subject><subject>fossil record</subject><subject>Fossils</subject><subject>gas chromatograms</subject><subject>Geochemistry</subject><subject>Gymnospermae</subject><subject>Hydrolysis</subject><subject>laboratory studies</subject><subject>Leaves</subject><subject>Lignin</subject><subject>Lipids</subject><subject>living taxa</subject><subject>mass spectra</subject><subject>modern analogs</subject><subject>organic compounds</subject><subject>Paleobotany</subject><subject>paleoecology</subject><subject>physiology</subject><subject>Plant cuticle</subject><subject>Plantae</subject><subject>Plants</subject><subject>preservation</subject><subject>Pyrolysis</subject><subject>s</subject><subject>spectra</subject><subject>Spermatophyta</subject><issn>0094-8373</issn><issn>1938-5331</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNp1kF9LwzAUxYMoOKf4BXwIgohIZ9K0aeubDP_BQBB9lJKkNzOja2bSKn5703WoID6Fm_O799x7EDqkZEI55xckJSyf0C00ogXLo5Qxuo1GhBRJlLOM7aI97xck1CnPRujlEUzzDr41c9Ea22CrcfsK2CrVOQeNgv5Hda1osGnwqhZN6y-xWa5qo9YdHmvr1j01CB0K702NHSjrqn20o0Xt4WDzjtHzzfXT9C6aPdzeT69mkUh43EaU55pLqQSVFdFaQlVUTMuYC8FSyhUoJQVXLM5ikhOWySAnkLEUmKgoBzZGx8PclbNvXbimXNjONcGyjOOCEZ7ESYBOB0i5sKMDXa6cWQr3WVJS9tGV6-hKGsijgVz41rpvLCEFLzgJ8vkgz8F6ZfqQPqyrq1-mhIRpGUt4b3u2sRVL6Uw1hx_ur_HJwEpjbQP_LvgF_jaS-A</recordid><startdate>200609</startdate><enddate>200609</enddate><creator>Gupta, Neal S</creator><creator>Collinson, Margaret E</creator><creator>Briggs, Derek E. 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G</au><au>Evershed, Richard P</au><au>Pancost, Richard D</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Reinvestigation of the occurrence of cutan in plants: implications for the leaf fossil record</atitle><jtitle>Paleobiology</jtitle><addtitle>Paleobiology</addtitle><date>2006-09</date><risdate>2006</risdate><volume>32</volume><issue>3</issue><spage>432</spage><epage>449</epage><pages>432-449</pages><issn>0094-8373</issn><eissn>1938-5331</eissn><coden>PALBBM</coden><abstract>Cutan, a resistant non-hydrolyzable aliphatic biopolymer, was first reported in the cuticle of Agave americana and has generally been considered ubiquitous in leaf cuticles along with the structural biopolyester cutin. Because leaves and cuticles in the fossil record almost always have an aliphatic composition, it was argued that selective preservation of cutan played an important role in leaf preservation. However, the analysis of leaves using chemical degradation techniques involving hydrolysis to test for the presence of cutan reveals that it is absent in 16 of 19 taxa (angiosperm and gymnosperm), including many previously reported to contain cutan on the basis of pyrolysis data. Cutan is clearly much less widespread in leaves than previously thought, and its presence or absence does not exert any major bias on the preservation of leaves in the fossil record. In the absence of cutan, other constituents—cutin, plant waxes, and internal plant lipids—are incorporated into the geomacromolecule and contribute to the formation of a resistant aliphatic polymer by in situ polymerization during diagenesis.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1666/05038.1</doi><tpages>18</tpages></addata></record> |
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subjects | Angiospermae Animal cuticle cutan experimental studies fossil record Fossils gas chromatograms Geochemistry Gymnospermae Hydrolysis laboratory studies Leaves Lignin Lipids living taxa mass spectra modern analogs organic compounds Paleobotany paleoecology physiology Plant cuticle Plantae Plants preservation Pyrolysis s spectra Spermatophyta |
title | Reinvestigation of the occurrence of cutan in plants: implications for the leaf fossil record |
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