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Drought and changes in leaf orientation for two California chaparral shrubs: Ceanothus megacarpus and Ceanothus crassifolius
Predawn xylem pressure potentials were measured on two California chaparral shrubs, Ceanothus megacarpus and Ceanothus crassifolius, throughout the winter and spring growing season and into the summer drought. On the days xylem pressure potentials were measured, leaf orientation measurements were ma...
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Published in: | Oecologia 1985-03, Vol.65 (4), p.531-535 |
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description | Predawn xylem pressure potentials were measured on two California chaparral shrubs, Ceanothus megacarpus and Ceanothus crassifolius, throughout the winter and spring growing season and into the summer drought. On the days xylem pressure potentials were measured, leaf orientation measurements were made on a population of marked leaves from the same shrubs. Predawn xylem pressure potentials decreased from -0.1 MPa in both species to -7.8 and -6.6 MPa in C. megacarpus and C. crassifolius, respectively, between May and August, 1981. Leaf inclinations became more vertical during this period with the greatest change observed in C. crassifolius. This change in leaf inclination was reversible, and, in the late winter and early spring, one year old leaves became more horizontal. Leaf azimuths were random and did not change seasonally. Simulations of solar radiation interception indicated that the increase in leaf inclination associated with summer drought reduced the absorption of solar radiation in August by 6% for C. megacarpus and 20% for C. crassifolius. Standard leaf energy budget calculations suggest that steep leaf inclinations would result in slightly lower leaf temperatures and transpiration rates under summer conditions. |
doi_str_mv | 10.1007/BF00379668 |
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On the days xylem pressure potentials were measured, leaf orientation measurements were made on a population of marked leaves from the same shrubs. Predawn xylem pressure potentials decreased from -0.1 MPa in both species to -7.8 and -6.6 MPa in C. megacarpus and C. crassifolius, respectively, between May and August, 1981. Leaf inclinations became more vertical during this period with the greatest change observed in C. crassifolius. This change in leaf inclination was reversible, and, in the late winter and early spring, one year old leaves became more horizontal. Leaf azimuths were random and did not change seasonally. Simulations of solar radiation interception indicated that the increase in leaf inclination associated with summer drought reduced the absorption of solar radiation in August by 6% for C. megacarpus and 20% for C. crassifolius. Standard leaf energy budget calculations suggest that steep leaf inclinations would result in slightly lower leaf temperatures and transpiration rates under summer conditions.</description><identifier>ISSN: 0029-8549</identifier><identifier>EISSN: 1432-1939</identifier><identifier>DOI: 10.1007/BF00379668</identifier><identifier>PMID: 28311861</identifier><identifier>CODEN: OECOBX</identifier><language>eng</language><publisher>Berlin: Springer-Verlag</publisher><subject>Animal and plant ecology ; Animal, plant and microbial ecology ; Autoecology ; Azimuth ; Biological and medical sciences ; Ceanothus ; ceanothus crassifolius ; ceanothus megacarpus ; Chaparral ; Drought ; environmental factors ; Fundamental and applied biological sciences. Psychology ; Growing seasons ; leaf orientation ; Leaves ; photosynthesis ; Plants ; Plants and fungi ; seasons ; Shrubs ; Solar radiation ; transpiration ; Vegetation canopies ; Xylem</subject><ispartof>Oecologia, 1985-03, Vol.65 (4), p.531-535</ispartof><rights>Copyright 1985 Springer-Verlag</rights><rights>1986 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c359t-34342999ed19c4fba01d543f500c18b4c27d015234113ba9c057ff6979135c833</citedby><cites>FETCH-LOGICAL-c359t-34342999ed19c4fba01d543f500c18b4c27d015234113ba9c057ff6979135c833</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/4217567$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4217567$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,58238,58471</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=8414998$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/28311861$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Comstock, J.P</creatorcontrib><creatorcontrib>Mahall, B.E</creatorcontrib><title>Drought and changes in leaf orientation for two California chaparral shrubs: Ceanothus megacarpus and Ceanothus crassifolius</title><title>Oecologia</title><addtitle>Oecologia</addtitle><description>Predawn xylem pressure potentials were measured on two California chaparral shrubs, Ceanothus megacarpus and Ceanothus crassifolius, throughout the winter and spring growing season and into the summer drought. On the days xylem pressure potentials were measured, leaf orientation measurements were made on a population of marked leaves from the same shrubs. Predawn xylem pressure potentials decreased from -0.1 MPa in both species to -7.8 and -6.6 MPa in C. megacarpus and C. crassifolius, respectively, between May and August, 1981. Leaf inclinations became more vertical during this period with the greatest change observed in C. crassifolius. This change in leaf inclination was reversible, and, in the late winter and early spring, one year old leaves became more horizontal. Leaf azimuths were random and did not change seasonally. Simulations of solar radiation interception indicated that the increase in leaf inclination associated with summer drought reduced the absorption of solar radiation in August by 6% for C. megacarpus and 20% for C. crassifolius. Standard leaf energy budget calculations suggest that steep leaf inclinations would result in slightly lower leaf temperatures and transpiration rates under summer conditions.</description><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Autoecology</subject><subject>Azimuth</subject><subject>Biological and medical sciences</subject><subject>Ceanothus</subject><subject>ceanothus crassifolius</subject><subject>ceanothus megacarpus</subject><subject>Chaparral</subject><subject>Drought</subject><subject>environmental factors</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Growing seasons</subject><subject>leaf orientation</subject><subject>Leaves</subject><subject>photosynthesis</subject><subject>Plants</subject><subject>Plants and fungi</subject><subject>seasons</subject><subject>Shrubs</subject><subject>Solar radiation</subject><subject>transpiration</subject><subject>Vegetation canopies</subject><subject>Xylem</subject><issn>0029-8549</issn><issn>1432-1939</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1985</creationdate><recordtype>article</recordtype><recordid>eNpFkEtvEzEURi0EomlgwxqBFywQ0oCvHzM2Owj0IVViAV2P7njsZKqJndozQkj98XWUkK7ulb6jsziEvAH2GRhrvny_YEw0pq71M7IAKXgFRpjnZMEYN5VW0pyR85zvGAMJSr0kZ1wLAF3Dgjz8SHFebyaKoad2g2HtMh0CHR16GtPgwoTTEAP1MdHpb6QrHIfyhwH3-A5TwpHmTZq7_JWuHIY4beZMt26NFtOuvHvz02AT5lwM4zDnV-SFxzG718e7JLcXP_-srqqbX5fXq283lRXKTJWQQnJjjOvBWOk7ZNArKbxizILupOVNz0BxIQFEh8Yy1Xhfm8aAUFYLsSQfD95divezy1O7HbJ144jBxTm3oButudAl45J8OqA2xZyT8-0uDVtM_1pg7b52-1S7wO-O3rnbuv6E_s9bgA9HALPF0ScMdsgnTkuQxuw9bw_YXZ5iOs2SQ6PqpszvD7PH2OI6FcPtb85AMF6XBiDEI2kemXE</recordid><startdate>19850301</startdate><enddate>19850301</enddate><creator>Comstock, J.P</creator><creator>Mahall, B.E</creator><general>Springer-Verlag</general><general>Springer</general><scope>FBQ</scope><scope>IQODW</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>19850301</creationdate><title>Drought and changes in leaf orientation for two California chaparral shrubs: Ceanothus megacarpus and Ceanothus crassifolius</title><author>Comstock, J.P ; Mahall, B.E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c359t-34342999ed19c4fba01d543f500c18b4c27d015234113ba9c057ff6979135c833</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1985</creationdate><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Autoecology</topic><topic>Azimuth</topic><topic>Biological and medical sciences</topic><topic>Ceanothus</topic><topic>ceanothus crassifolius</topic><topic>ceanothus megacarpus</topic><topic>Chaparral</topic><topic>Drought</topic><topic>environmental factors</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Growing seasons</topic><topic>leaf orientation</topic><topic>Leaves</topic><topic>photosynthesis</topic><topic>Plants</topic><topic>Plants and fungi</topic><topic>seasons</topic><topic>Shrubs</topic><topic>Solar radiation</topic><topic>transpiration</topic><topic>Vegetation canopies</topic><topic>Xylem</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Comstock, J.P</creatorcontrib><creatorcontrib>Mahall, B.E</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>Oecologia</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Comstock, J.P</au><au>Mahall, B.E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Drought and changes in leaf orientation for two California chaparral shrubs: Ceanothus megacarpus and Ceanothus crassifolius</atitle><jtitle>Oecologia</jtitle><addtitle>Oecologia</addtitle><date>1985-03-01</date><risdate>1985</risdate><volume>65</volume><issue>4</issue><spage>531</spage><epage>535</epage><pages>531-535</pages><issn>0029-8549</issn><eissn>1432-1939</eissn><coden>OECOBX</coden><abstract>Predawn xylem pressure potentials were measured on two California chaparral shrubs, Ceanothus megacarpus and Ceanothus crassifolius, throughout the winter and spring growing season and into the summer drought. On the days xylem pressure potentials were measured, leaf orientation measurements were made on a population of marked leaves from the same shrubs. Predawn xylem pressure potentials decreased from -0.1 MPa in both species to -7.8 and -6.6 MPa in C. megacarpus and C. crassifolius, respectively, between May and August, 1981. Leaf inclinations became more vertical during this period with the greatest change observed in C. crassifolius. This change in leaf inclination was reversible, and, in the late winter and early spring, one year old leaves became more horizontal. Leaf azimuths were random and did not change seasonally. Simulations of solar radiation interception indicated that the increase in leaf inclination associated with summer drought reduced the absorption of solar radiation in August by 6% for C. megacarpus and 20% for C. crassifolius. Standard leaf energy budget calculations suggest that steep leaf inclinations would result in slightly lower leaf temperatures and transpiration rates under summer conditions.</abstract><cop>Berlin</cop><pub>Springer-Verlag</pub><pmid>28311861</pmid><doi>10.1007/BF00379668</doi><tpages>5</tpages></addata></record> |
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subjects | Animal and plant ecology Animal, plant and microbial ecology Autoecology Azimuth Biological and medical sciences Ceanothus ceanothus crassifolius ceanothus megacarpus Chaparral Drought environmental factors Fundamental and applied biological sciences. Psychology Growing seasons leaf orientation Leaves photosynthesis Plants Plants and fungi seasons Shrubs Solar radiation transpiration Vegetation canopies Xylem |
title | Drought and changes in leaf orientation for two California chaparral shrubs: Ceanothus megacarpus and Ceanothus crassifolius |
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