Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1007/s00442-009-1515-6
Volltext Shareable Link
Titel (primär) Phylogenetically balanced evidence for structural and carbon isotope responses in plants along elevational gradients
Autor Zhu, Y.; Siegwolf, R.T.W.; Durka, W. ORCID logo ; Körner, C.
Quelle Oecologia
Erscheinungsjahr 2010
Department BZF; RESPONSES
Band/Volume 162
Heft 4
Seite von 853
Seite bis 863
Sprache englisch
Supplements https://static-content.springer.com/esm/art%3A10.1007%2Fs00442-009-1515-6/MediaObjects/442_2009_1515_MOESM1_ESM.doc
Keywords Elevation; Atmospheric pressure; Morphology; Reproduction; Temperature
Abstract We tested three hypotheses related to the functioning of mountain plants, namely their reproductive effort, leaf surface structure and effectiveness of CO2 assimilation, using archive material from contrasting elevations. Analysis of elevational trends is at risk of suffering from two major biases: a phylogenetic bias (i.e. an elevational change in the abundance of taxonomic groups), and covariation of different environmental drivers (e.g. water, temperature, atmospheric pressure), which do not permit a mechanistic interpretation. We solved both problems in a subcontinental survey of elevational trends in key plant traits in the European Alps and the high Arctic (northern Sweden, Svalbard), using herbarium samples of 147 species belonging to the genera Carex, Saxifraga and Potentilla. We used both species and phylogenetically independent contrasts as data points. The analysis revealed enhanced reproductive efforts at higher elevation in insect-pollinated taxa (not in wind-pollinated taxa), no increase in leaf pubescence at high elevation (as is often assumed), and a strong correlation between 13C discrimination and elevation. Alpine taxa operate at a smaller mesophyll resistance to CO2 uptake relative to diffusive resistance (stomata). By comparison with congeneric low altitude polar taxa (low temperature, but high atmospheric pressure), the response could be attributed to the elevational decline in atmospheric pressure rather than temperature (a mean increase in d13C by 1.4? km-1). The signal is consistent within and across genera and within species, suggesting rapid adjustment of leaf physiology to reduced partial pressure of CO2. These results offer answers to long-debated issues of plant responses to high elevation life conditions.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=10695
Zhu, Y., Siegwolf, R.T.W., Durka, W., Körner, C. (2010):
Phylogenetically balanced evidence for structural and carbon isotope responses in plants along elevational gradients
Oecologia 162 (4), 853 - 863 10.1007/s00442-009-1515-6