Glacial trees from the La Brea tar pits show physiological constraints of low CO₂

© 2011 The Authors. New Phytologist © 2011 New Phytologist Trust.

Bibliographische Detailangaben
Veröffentlicht in:The New phytologist. - 1979. - 194(2012), 1 vom: 26. Apr., Seite 63-69
1. Verfasser: Gerhart, Laci M (VerfasserIn)
Weitere Verfasser: Harris, John M, Nippert, Jesse B, Sandquist, Darren R, Ward, Joy K
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2012
Zugriff auf das übergeordnete Werk:The New phytologist
Schlagworte:Journal Article Research Support, Non-U.S. Gov't Research Support, U.S. Gov't, Non-P.H.S. Carbon Isotopes Tars Carbon Dioxide 142M471B3J
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245 1 0 |a Glacial trees from the La Brea tar pits show physiological constraints of low CO₂ 
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500 |a published: Print-Electronic 
500 |a CommentIn: New Phytol. 2012 Apr;194(1):4-6. - PMID 22364117 
500 |a Citation Status MEDLINE 
520 |a © 2011 The Authors. New Phytologist © 2011 New Phytologist Trust. 
520 |a • While studies of modern plants indicate negative responses to low [CO₂] that occurred during the last glacial period, studies with glacial plant material that incorporate evolutionary responses are rare. In this study, physiological responses to changing [CO₂] were compared between glacial (La Brea tar pits) and modern Juniperus trees from southern California. • Carbon isotopes were measured on annual rings of glacial and modern Juniperus. The intercellular:atmospheric [CO₂] ratio (c(i) /c(a) ) and intercellular [CO₂] (c(i) ) were then calculated on an annual basis and compared through geologic time. • Juniperus showed constant mean c(i) /c(a) between the last glacial period and modern times, spanning 50,000 yr. Interannual variation in physiology was greatly dampened during the last glacial period relative to the present, indicating constraints of low [CO₂] that reduced responses to other climatic factors. Furthermore, glacial Juniperus exhibited low c(i) that rarely occurs in modern trees, further suggesting limiting [CO₂] in glacial plants. • This study provides some of the first direct evidence that glacial plants remained near their lower carbon limit until the beginning of the glacial-interglacial transition. Our results also suggest that environmental factors that dominate carbon-uptake physiology vary across geologic time, resulting in major alterations in physiological response patterns through time 
650 4 |a Journal Article 
650 4 |a Research Support, Non-U.S. Gov't 
650 4 |a Research Support, U.S. Gov't, Non-P.H.S. 
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650 7 |a Tars  |2 NLM 
650 7 |a Carbon Dioxide  |2 NLM 
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700 1 |a Harris, John M  |e verfasserin  |4 aut 
700 1 |a Nippert, Jesse B  |e verfasserin  |4 aut 
700 1 |a Sandquist, Darren R  |e verfasserin  |4 aut 
700 1 |a Ward, Joy K  |e verfasserin  |4 aut 
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