Contemporary richness of holarctic trees and the historical pattern of glacial retreat

Ecography - Tập 30 Số 2 - Trang 173-182 - 2007
Daniel Montoya, Miguel Á. Rodrı́guez, Miguel Á. Zavala, Bradford A. Hawkins

Tóm tắt

The length of time land has been available for colonization by plants and other organisms could provide a partial explanation of the contemporary richness gradients of trees. According to this hypothesis, increasing times of land availability entail higher chances of recolonization, which eventually have positive effects on tree richness. To test this, we generated a dataset of the Holarctic trees and evaluated the influence of cell age, a measure of the time since an area became free of ice, on the observed tree richness gradients. We found that cell age is associated with richness in both Europe and North America, after controlling for contemporary climate patterns, suggesting that the historical pattern of glacial retreat in response to post‐Pleistocene global warming has left a signal still detectable after at least 14 000 yr. The results were consistent using a range of modelling approaches or whether Europe and North America were analyzed separately or in concert. We conclude that, although secondary to contemporary climate, the post‐glacial recolonization hypothesis is broadly supported at temperate latitudes.

Từ khóa


Tài liệu tham khảo

10.1038/339699a0

10.1111/j.2005.0906-7590.04253.x

Begon M., 1996, Ecology

10.2307/2845248

10.1111/j.1365-2699.2004.01203.x

Burnham K. P., 2002, Model selection and multimodel inference: a practical information‐theoretic approach

10.1002/9781119115151

10.1086/285144

10.1038/329326a0

10.1046/j.1466-822X.2003.00322.x

Dykes A. S., 1987, Late Wisconsinan and Holocene history of the Laurentide ice sheet, Geogr. Phys. Quat., 41, 237

10.1046/j.1365-2699.2000.00430.x

10.1111/j.1365-2699.2006.01533.x

10.1890/04-1910

10.1086/368223

10.1017/CBO9780511754944

10.1126/science.1087570

10.1046/j.1466-822X.2003.00060.x

10.1890/03-8006

10.1111/j.1365-2699.2006.01452.x

Hawkins B. A., Global models for predicting woody plant richness from climate: comment, 10.1890/0012-9658(2007)88[255:GMFPWP]2.0.CO;2

10.1111/j.1095-8312.1999.tb01160.x

10.1038/35016000

10.1016/j.tree.2003.10.013

10.1046/j.1365-2699.2002.00743.x

Legendre P., 1998, Numerical ecology

MacArthur R. H., 1967, The theory of island biogeography

10.2307/2997586

10.1890/04-1036

10.1038/35002501

10.2307/2845670

10.1046/j.1365-2699.1998.252166.x

Peltier W., 1993, Time dependent topography through glacial cycle

10.1046/j.1365-2699.2000.00425.x

10.1086/303230

Rangel T. F. L. V. B., 2005, SAM v.1.0 beta – Spatial analysis in macroecology

10.2307/3546454

10.1111/j.1466-822X.2006.00206.x

10.1111/j.1365-2699.2004.01223.x

10.1046/j.1461-0248.2003.00477.x

10.1111/j.1461-0248.2004.00614.x

10.1111/j.1365-2699.2005.01219.x

Svenning J.‐C., Ice Age legacies in the geographical distribution of tree species richness in Europe, 10.1111/j.1466-8238.2006.00280.x

10.1046/j.1365-2699.2000.00429.x

Thornwaite C. W., 1948, An approach toward a rational classification of climate, Geogr. Rev., 38, 55, 10.2307/210739

10.1016/j.baae.2004.08.004

10.1038/335539a0

10.1034/j.1600-0706.2000.890222.x

10.1046/j.1365-2699.2000.00428.x

10.1016/0160-9327(96)10019-3

10.1016/j.quascirev.2004.06.002