Leaf form–climate relationships on the global stage: an ensemble of characters
Tóm tắt
Early in their evolution, angiosperms evolved a diversity of leaf form far greater than that of any other group of land plants. Some of this diversity evolved in response to varying climate. Our aim is to test the global relationship between leaf form in woody dicot angiosperms and the climate in which they live.
We have compiled a data set describing leaf form (using 31 standardized categorical characters) from 378 natural or naturalized vegetation sites from around the world. Our data include sites from all continents except
We chose the
Woody dicot leaf characters form a physiognomic spectrum that reflects local climate conditions. On a global scale, correlations between leaf form and climate are consistent, irrespective of climate regime, vegetation type or biogeographic history. Relationships with temperature variables are maintained even when leaf margin characters, regarded as being particularly well correlated with mean annual temperature, are removed.
In natural woody dicot vegetation an integrated spectrum of leaf form has developed across multiple leaf character states and species. This spectrum appears more strongly influenced by prevailing climate than biogeographic history. The covariation of leaf traits across species suggests strong integration of leaf form. New methods of exploring structure in multidimensional physiognomic space enable better application of leaf form to palaeoclimate reconstruction.
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Tài liệu tham khảo
Cariglino B., 2005, Paleoclimate estimation from digital leaf physiognomy of fossil leaf floras: preliminary results, GSA Abstracts, 37, 137
Falconer D.S., 1996, Introduction to quantitative genetics
Givnish T.J., 1984, Biological diversity in México: origins and distribution, 109
Janesko D.A., 2004, Digital leaf physiognomy: an automated routine for analyzing size and shape of plant leaves for paleoclimate and paleoecological analysis, GSA Abstracts, 36, 63
Kennedy E.M., 2001, Abstracts and programme, Geological Society of New Zealand Annual Conference 2001 ‘Advances in geosciences’, University of Waikato, Hamilton
Kovach W.L., 1995, Canonical correspondence analysis of leaf physiognomy: a contribution to the development of a new palaeoclimatological tool, Palaeoclimates, 1, 125
Olsen D.M., 2001, Terrestrial ecoregions of the world: a new map of life on Earth: a new global map of terrestrial ecoregions provides an innovative tool for conserving biodiversity, Bioscience, 51, 933, 10.1641/0006-3568(2001)051[0933:TEOTWA]2.0.CO;2
Peppe D.J., 2009, Digital leaf physiognomy: using leaf size and shape to reconstruct ancient climates, GSA Abstracts, 41, 568
R Core Team(2012)R: a language and environment for statistical computing.R Foundation for Statistical Computing Vienna Austria.
Royer D.L., 2004, Digital leaf physiognomy: calibration of a new method for reconstructing climate from fossil plants, GSA Abstracts, 36, 95
Royer D.L., 2008, Digital leaf physiognomy: a multivariate technique for reconstructing climate from fossil leaves, GSA Abstracts, 40, 100
Uhl D., 2007, Fossil leaves as palaeoclimate proxies in the Palaeogene of Spitsbergen (Svalbard), Acta Palaeobotanica, 47, 89
Upchurch G.R., 1987, The origin of angiosperms and their biological consequences, 75
Wolfe J.A., 1978, A paleobotanical interpretation of Tertiary climates in the Northern Hemisphere, American Science, 66, 694
Wolfe J.A., 1979, Temperature parameters of humid to mesic forests of Eastern Asia and relation to forests of other regions of the Northern Hemisphere and Australasia, Geological Survey Professional Paper, 1106, 1