Will loss of snow cover during climatic warming expose New Zealand alpine plants to increased frost damage?
If snow cover in alpine environments were reduced through climatic warming, plants that are normally protected by snow-lie in winter would become exposed to greater extremes of temperature and solar radiation. We examined the annual course of frost resistance of species of native alpine plants from...
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description | If snow cover in alpine environments were reduced through climatic warming, plants that are normally protected by snow-lie in winter would become exposed to greater extremes of temperature and solar radiation. We examined the annual course of frost resistance of species of native alpine plants from southern New Zealand that are normally buried in snowbanks over winter (Celmisia haastii and Celmisia prorepens) or in sheltered areas that may accumulate snow (Hebe odora) and other species, typical of more exposed areas, that are relatively snow-free (Celmisia viscosa, Poa colensoi, Dracophyllum muscoides). The frost resistance of these principal species was in accord with habitat: those from snowbanks or sheltered areas showed the least frost resistance, whereas species from exposed areas had greater frost resistance throughout the year. P. colensoi had the greatest frost resistance (-32.5°C). All the principal species showed a rapid increase in frost resistance from summer to early winter (February-June) and maximum frost resistance in winter (July-August). The loss of resistance in late winter to early summer (August-December) was most rapid in P. colensoi and D. muscoides. Seasonal frost resistance of the principal species was more strongly related to daylength than to temperature, although all species except C. viscosa were significantly related to temperature when the influence of daylength was accounted for. Measurements of chlorophyll fluorescence indicated that photosynthetic efficiency of the principal species declined with increasing daylength. Levels of frost resistance of the six principal alpine plant species, and others measured during the growing season, were similar to those measured in tropical alpine areas and somewhat more resistant than those recorded in alpine areas of Europe. The potential for frost damage was greatest in spring. The current relationship of frost resistance with daylength is sufficient to prevent damage at any time of year. While warmer temperatures might lower frost resistance, they would also reduce the incidence of frosts, and the incidence of frost damage is unlikely to be altered. The relationship of frost resistance with daylength and temperature potentially provides a means of predicting the responses of alpine plants in response to global warming. |
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We examined the annual course of frost resistance of species of native alpine plants from southern New Zealand that are normally buried in snowbanks over winter (Celmisia haastii and Celmisia prorepens) or in sheltered areas that may accumulate snow (Hebe odora) and other species, typical of more exposed areas, that are relatively snow-free (Celmisia viscosa, Poa colensoi, Dracophyllum muscoides). The frost resistance of these principal species was in accord with habitat: those from snowbanks or sheltered areas showed the least frost resistance, whereas species from exposed areas had greater frost resistance throughout the year. P. colensoi had the greatest frost resistance (-32.5°C). All the principal species showed a rapid increase in frost resistance from summer to early winter (February-June) and maximum frost resistance in winter (July-August). The loss of resistance in late winter to early summer (August-December) was most rapid in P. colensoi and D. muscoides. Seasonal frost resistance of the principal species was more strongly related to daylength than to temperature, although all species except C. viscosa were significantly related to temperature when the influence of daylength was accounted for. Measurements of chlorophyll fluorescence indicated that photosynthetic efficiency of the principal species declined with increasing daylength. Levels of frost resistance of the six principal alpine plant species, and others measured during the growing season, were similar to those measured in tropical alpine areas and somewhat more resistant than those recorded in alpine areas of Europe. The potential for frost damage was greatest in spring. The current relationship of frost resistance with daylength is sufficient to prevent damage at any time of year. While warmer temperatures might lower frost resistance, they would also reduce the incidence of frosts, and the incidence of frost damage is unlikely to be altered. The relationship of frost resistance with daylength and temperature potentially provides a means of predicting the responses of alpine plants in response to global warming.</description><identifier>ISSN: 0029-8549</identifier><identifier>EISSN: 1432-1939</identifier><identifier>DOI: 10.1007/s00442-005-0087-3</identifier><identifier>PMID: 15891822</identifier><identifier>CODEN: OECOBX</identifier><language>eng</language><publisher>Berlin: Springer</publisher><subject>Adaptation, Physiological - physiology ; Alpine environments ; Alpine plants ; Altitude ; Animal and plant ecology ; Animal, plant and microbial ecology ; Applied ecology ; Biological and medical sciences ; Celmisia haastii ; Celmisia prorepens ; Celmisia viscosa ; Climate change ; Dracophyllum muscoides ; Ecophysiology ; Ecotoxicology, biological effects of pollution ; Flowers & plants ; Freezing ; Frost ; Frost damage ; frost injury ; Frost resistance ; Fundamental and applied biological sciences. Psychology ; General aspects ; Geography ; Global warming ; Greenhouse Effect ; Growing season ; Hebe odora ; Indigenous species ; Leaves ; New Zealand ; Photoperiod ; Plant Physiological Phenomena ; Plant species ; Plants ; Poa colensoi ; Seasons ; Snow ; Snow accumulation ; Snow cover ; Solar radiation ; Species Specificity ; Summer ; Sunlight ; Temperature ; Temperature resistance ; Winter</subject><ispartof>Oecologia, 2005-06, Vol.144 (2), p.245-256</ispartof><rights>Copyright 2005 Springer-Verlag Berlin Heidelberg</rights><rights>2005 INIST-CNRS</rights><rights>Springer-Verlag 2005</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c433t-bb9dadea5244c5e1d31335440cb0dcf7ed717371f877176b8cae3c061bae37663</citedby><cites>FETCH-LOGICAL-c433t-bb9dadea5244c5e1d31335440cb0dcf7ed717371f877176b8cae3c061bae37663</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/20062325$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/20062325$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16863168$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/15891822$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Bannister, P</creatorcontrib><creatorcontrib>Maegli, T</creatorcontrib><creatorcontrib>Dickinson, K.J.M</creatorcontrib><creatorcontrib>Halloy, S.R.P</creatorcontrib><creatorcontrib>Knight, A</creatorcontrib><creatorcontrib>Lord, J.M</creatorcontrib><creatorcontrib>Mark., A.F</creatorcontrib><creatorcontrib>Spencer, K.L</creatorcontrib><title>Will loss of snow cover during climatic warming expose New Zealand alpine plants to increased frost damage?</title><title>Oecologia</title><addtitle>Oecologia</addtitle><description>If snow cover in alpine environments were reduced through climatic warming, plants that are normally protected by snow-lie in winter would become exposed to greater extremes of temperature and solar radiation. We examined the annual course of frost resistance of species of native alpine plants from southern New Zealand that are normally buried in snowbanks over winter (Celmisia haastii and Celmisia prorepens) or in sheltered areas that may accumulate snow (Hebe odora) and other species, typical of more exposed areas, that are relatively snow-free (Celmisia viscosa, Poa colensoi, Dracophyllum muscoides). The frost resistance of these principal species was in accord with habitat: those from snowbanks or sheltered areas showed the least frost resistance, whereas species from exposed areas had greater frost resistance throughout the year. P. colensoi had the greatest frost resistance (-32.5°C). All the principal species showed a rapid increase in frost resistance from summer to early winter (February-June) and maximum frost resistance in winter (July-August). The loss of resistance in late winter to early summer (August-December) was most rapid in P. colensoi and D. muscoides. Seasonal frost resistance of the principal species was more strongly related to daylength than to temperature, although all species except C. viscosa were significantly related to temperature when the influence of daylength was accounted for. Measurements of chlorophyll fluorescence indicated that photosynthetic efficiency of the principal species declined with increasing daylength. Levels of frost resistance of the six principal alpine plant species, and others measured during the growing season, were similar to those measured in tropical alpine areas and somewhat more resistant than those recorded in alpine areas of Europe. The potential for frost damage was greatest in spring. The current relationship of frost resistance with daylength is sufficient to prevent damage at any time of year. While warmer temperatures might lower frost resistance, they would also reduce the incidence of frosts, and the incidence of frost damage is unlikely to be altered. The relationship of frost resistance with daylength and temperature potentially provides a means of predicting the responses of alpine plants in response to global warming.</description><subject>Adaptation, Physiological - physiology</subject><subject>Alpine environments</subject><subject>Alpine plants</subject><subject>Altitude</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Applied ecology</subject><subject>Biological and medical sciences</subject><subject>Celmisia haastii</subject><subject>Celmisia prorepens</subject><subject>Celmisia viscosa</subject><subject>Climate change</subject><subject>Dracophyllum muscoides</subject><subject>Ecophysiology</subject><subject>Ecotoxicology, biological effects of pollution</subject><subject>Flowers & plants</subject><subject>Freezing</subject><subject>Frost</subject><subject>Frost damage</subject><subject>frost injury</subject><subject>Frost resistance</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General aspects</subject><subject>Geography</subject><subject>Global warming</subject><subject>Greenhouse Effect</subject><subject>Growing season</subject><subject>Hebe odora</subject><subject>Indigenous species</subject><subject>Leaves</subject><subject>New Zealand</subject><subject>Photoperiod</subject><subject>Plant Physiological Phenomena</subject><subject>Plant species</subject><subject>Plants</subject><subject>Poa colensoi</subject><subject>Seasons</subject><subject>Snow</subject><subject>Snow accumulation</subject><subject>Snow cover</subject><subject>Solar radiation</subject><subject>Species Specificity</subject><subject>Summer</subject><subject>Sunlight</subject><subject>Temperature</subject><subject>Temperature resistance</subject><subject>Winter</subject><issn>0029-8549</issn><issn>1432-1939</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><sourceid>EIF</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNqFkU2P1DAMhiMEYmcXfgAHIFoJbgU7H016QmjFl7SCA6yQuERpko46dJqStAz8ezLqiJW4cEicxI_t2C8hjxBeIIB6mQGEYBWALEurit8hGxScVdjw5i7ZALCm0lI0Z-Q85x0ACpTyPjlDqRvUjG3I96_9MNAh5kxjR_MYD9TFnyFRv6R-3FI39Hs7944ebNofH8KvKeZAP4YD_RbsYEdP7TD1Y6BTucyZzpH2o0vB5uBpl2Keqbd7uw2vHpB7nR1yeHiyF-Tm7ZsvV--r60_vPly9vq6c4Hyu2rbx1gcrmRBOBvQcOZdCgGvBu04Fr1BxhZ1W5VC32tnAHdTYFqvqml-Q52veKcUfS8iz2ffZhaH8L8Qlm1oLocoo_guiwlJJsgJe_gPu4pLG0oTRDLiSkh3L4gq50nROoTNTKsNLvw2COeplVr1M0csc9TK8xDw5JV7affC3ESeBCvDsBNjs7NAlO7o-33K1rnnZCvd45XZ5jumvnwHUjDNZ_E9Xf2ejsdtUctx8ZoAcEFDzWvA_UIWv6g</recordid><startdate>20050601</startdate><enddate>20050601</enddate><creator>Bannister, P</creator><creator>Maegli, T</creator><creator>Dickinson, K.J.M</creator><creator>Halloy, S.R.P</creator><creator>Knight, A</creator><creator>Lord, J.M</creator><creator>Mark., A.F</creator><creator>Spencer, K.L</creator><general>Springer</general><general>Springer Nature B.V</general><scope>FBQ</scope><scope>IQODW</scope><scope>CGR</scope><scope>CUY</scope><scope>CVF</scope><scope>ECM</scope><scope>EIF</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7QG</scope><scope>7QL</scope><scope>7SN</scope><scope>7SS</scope><scope>7T7</scope><scope>7TN</scope><scope>7U9</scope><scope>7X7</scope><scope>7XB</scope><scope>88A</scope><scope>88E</scope><scope>8AO</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FI</scope><scope>8FJ</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>FYUFA</scope><scope>GHDGH</scope><scope>GNUQQ</scope><scope>H94</scope><scope>H95</scope><scope>HCIFZ</scope><scope>K9.</scope><scope>L.G</scope><scope>LK8</scope><scope>M0S</scope><scope>M1P</scope><scope>M7N</scope><scope>M7P</scope><scope>P64</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>7X8</scope></search><sort><creationdate>20050601</creationdate><title>Will loss of snow cover during climatic warming expose New Zealand alpine plants to increased frost damage?</title><author>Bannister, P ; Maegli, T ; Dickinson, K.J.M ; Halloy, S.R.P ; Knight, A ; Lord, J.M ; Mark., A.F ; Spencer, K.L</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c433t-bb9dadea5244c5e1d31335440cb0dcf7ed717371f877176b8cae3c061bae37663</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Adaptation, Physiological - physiology</topic><topic>Alpine environments</topic><topic>Alpine plants</topic><topic>Altitude</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Applied ecology</topic><topic>Biological and medical sciences</topic><topic>Celmisia haastii</topic><topic>Celmisia prorepens</topic><topic>Celmisia viscosa</topic><topic>Climate change</topic><topic>Dracophyllum muscoides</topic><topic>Ecophysiology</topic><topic>Ecotoxicology, biological effects of pollution</topic><topic>Flowers & plants</topic><topic>Freezing</topic><topic>Frost</topic><topic>Frost damage</topic><topic>frost injury</topic><topic>Frost resistance</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General aspects</topic><topic>Geography</topic><topic>Global warming</topic><topic>Greenhouse Effect</topic><topic>Growing season</topic><topic>Hebe odora</topic><topic>Indigenous species</topic><topic>Leaves</topic><topic>New Zealand</topic><topic>Photoperiod</topic><topic>Plant Physiological Phenomena</topic><topic>Plant species</topic><topic>Plants</topic><topic>Poa colensoi</topic><topic>Seasons</topic><topic>Snow</topic><topic>Snow accumulation</topic><topic>Snow cover</topic><topic>Solar radiation</topic><topic>Species Specificity</topic><topic>Summer</topic><topic>Sunlight</topic><topic>Temperature</topic><topic>Temperature resistance</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Bannister, P</creatorcontrib><creatorcontrib>Maegli, T</creatorcontrib><creatorcontrib>Dickinson, K.J.M</creatorcontrib><creatorcontrib>Halloy, S.R.P</creatorcontrib><creatorcontrib>Knight, A</creatorcontrib><creatorcontrib>Lord, J.M</creatorcontrib><creatorcontrib>Mark., A.F</creatorcontrib><creatorcontrib>Spencer, K.L</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>Medline</collection><collection>MEDLINE</collection><collection>MEDLINE (Ovid)</collection><collection>MEDLINE</collection><collection>MEDLINE</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Animal Behavior Abstracts</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Oceanic Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Health & Medical Collection</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Medical Database (Alumni Edition)</collection><collection>ProQuest Pharma Collection</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Hospital Premium Collection</collection><collection>Hospital Premium Collection (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Health Research Premium Collection</collection><collection>Health Research Premium Collection (Alumni)</collection><collection>ProQuest Central Student</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Health & Medical Complete (Alumni)</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Health & Medical Collection (Alumni Edition)</collection><collection>Medical Database</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>MEDLINE - Academic</collection><jtitle>Oecologia</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Bannister, P</au><au>Maegli, T</au><au>Dickinson, K.J.M</au><au>Halloy, S.R.P</au><au>Knight, A</au><au>Lord, J.M</au><au>Mark., A.F</au><au>Spencer, K.L</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Will loss of snow cover during climatic warming expose New Zealand alpine plants to increased frost damage?</atitle><jtitle>Oecologia</jtitle><addtitle>Oecologia</addtitle><date>2005-06-01</date><risdate>2005</risdate><volume>144</volume><issue>2</issue><spage>245</spage><epage>256</epage><pages>245-256</pages><issn>0029-8549</issn><eissn>1432-1939</eissn><coden>OECOBX</coden><abstract>If snow cover in alpine environments were reduced through climatic warming, plants that are normally protected by snow-lie in winter would become exposed to greater extremes of temperature and solar radiation. We examined the annual course of frost resistance of species of native alpine plants from southern New Zealand that are normally buried in snowbanks over winter (Celmisia haastii and Celmisia prorepens) or in sheltered areas that may accumulate snow (Hebe odora) and other species, typical of more exposed areas, that are relatively snow-free (Celmisia viscosa, Poa colensoi, Dracophyllum muscoides). The frost resistance of these principal species was in accord with habitat: those from snowbanks or sheltered areas showed the least frost resistance, whereas species from exposed areas had greater frost resistance throughout the year. P. colensoi had the greatest frost resistance (-32.5°C). All the principal species showed a rapid increase in frost resistance from summer to early winter (February-June) and maximum frost resistance in winter (July-August). The loss of resistance in late winter to early summer (August-December) was most rapid in P. colensoi and D. muscoides. Seasonal frost resistance of the principal species was more strongly related to daylength than to temperature, although all species except C. viscosa were significantly related to temperature when the influence of daylength was accounted for. Measurements of chlorophyll fluorescence indicated that photosynthetic efficiency of the principal species declined with increasing daylength. Levels of frost resistance of the six principal alpine plant species, and others measured during the growing season, were similar to those measured in tropical alpine areas and somewhat more resistant than those recorded in alpine areas of Europe. The potential for frost damage was greatest in spring. The current relationship of frost resistance with daylength is sufficient to prevent damage at any time of year. While warmer temperatures might lower frost resistance, they would also reduce the incidence of frosts, and the incidence of frost damage is unlikely to be altered. The relationship of frost resistance with daylength and temperature potentially provides a means of predicting the responses of alpine plants in response to global warming.</abstract><cop>Berlin</cop><pub>Springer</pub><pmid>15891822</pmid><doi>10.1007/s00442-005-0087-3</doi><tpages>12</tpages></addata></record> |
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subjects | Adaptation, Physiological - physiology Alpine environments Alpine plants Altitude Animal and plant ecology Animal, plant and microbial ecology Applied ecology Biological and medical sciences Celmisia haastii Celmisia prorepens Celmisia viscosa Climate change Dracophyllum muscoides Ecophysiology Ecotoxicology, biological effects of pollution Flowers & plants Freezing Frost Frost damage frost injury Frost resistance Fundamental and applied biological sciences. Psychology General aspects Geography Global warming Greenhouse Effect Growing season Hebe odora Indigenous species Leaves New Zealand Photoperiod Plant Physiological Phenomena Plant species Plants Poa colensoi Seasons Snow Snow accumulation Snow cover Solar radiation Species Specificity Summer Sunlight Temperature Temperature resistance Winter |
title | Will loss of snow cover during climatic warming expose New Zealand alpine plants to increased frost damage? |
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