Stomatal density responds to the glacial cycle of environmental change
1993; Royal Society; Volume: 251; Issue: 1331 Linguagem: Inglês
10.1098/rspb.1993.0019
ISSN1471-2954
AutoresDavid J. Beerling, William Gilbert Chaloner, Brian Huntley, John Richard Anthony Pearson, M. J. Tooley,
Tópico(s)Plant responses to elevated CO2
ResumoRestricted accessMoreSectionsView PDF ToolsAdd to favoritesDownload CitationsTrack Citations ShareShare onFacebookTwitterLinked InRedditEmail Cite this article Beerling D. J. , Chaloner William Gilbert , Huntley Brian , Pearson John Richard Anthony and Tooley M. J. 1993Stomatal density responds to the glacial cycle of environmental changeProc. R. Soc. Lond. B.251133–138http://doi.org/10.1098/rspb.1993.0019SectionRestricted accessArticleStomatal density responds to the glacial cycle of environmental change D. J. Beerling Google Scholar Find this author on PubMed Search for more papers by this author , William Gilbert Chaloner Google Scholar Find this author on PubMed Search for more papers by this author , Brian Huntley Google Scholar Find this author on PubMed Search for more papers by this author , John Richard Anthony Pearson Google Scholar Find this author on PubMed Search for more papers by this author and M. J. Tooley Google Scholar Find this author on PubMed Search for more papers by this author D. J. Beerling Google Scholar Find this author on PubMed , William Gilbert Chaloner Google Scholar Find this author on PubMed , Brian Huntley Google Scholar Find this author on PubMed , John Richard Anthony Pearson Google Scholar Find this author on PubMed and M. J. Tooley Google Scholar Find this author on PubMed Published:22 February 1993https://doi.org/10.1098/rspb.1993.0019AbstractExamining the response of stomatal density to past changes in atmospheric CO2 concentration helps us to understand how plants adapted to palaeoenvironmental change, and so helps in predicting their response to future global environmental change. Stomatal density is an important physiological parameter that underpins the productivity of terrestrial vegetation by affecting both rate of carbon uptake and water use efficiency. Previous work on temperate tree species showed a decrease in stomatal density in response to a 60 p. p. m. v. increase in atmospheric CO2 concentration over the past 200 years. However, such a short timespan largely excludes the genetic component of plant adaptation to change in CO2 concentration. We present the first record of stomatal density from fossil leaves extending over 140 ka. Our record for the arctic-alpine dwarf shrub Salix herbacea L. extends back to the penultimate glacial stage, spanning two intervals when atmospheric CO2 concentration was considerably lower (by ca. 170 p. p. m. v.) than at present. Our results demonstrate a decrease in stomatal density in response to long-term increases in atmospheric CO2 concentration, and are in accordance with previous short-term observations and experiments. This implies that relaxation of the stress imposed by low atmospheric CO2 concentration has enabled terrestrial plants to exhibit an adaptive response to the other limiting factor of water availability by reducing stomatal density and hence improving water use efficiency.FootnotesThis text was harvested from a scanned image of the original document using optical character recognition (OCR) software. As such, it may contain errors. Please contact the Royal Society if you find an error you would like to see corrected. Mathematical notations produced through Infty OCR. Previous ArticleNext Article VIEW FULL TEXT DOWNLOAD PDF FiguresRelatedReferencesDetailsCited by Riding J, Scott A and Collinson M (2019) A biography and obituary of William G. Chaloner FRS (1928–2016), Palynology, 10.1080/01916122.2018.1535458, 44:1, (127-166), Online publication date: 2-Jan-2020. 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