Evolutionary consequences of changes in species' geographical distributions driven by Milankovitch climate oscillations.
By M. Dynesius, Roland Jansson. Proceedings of the National Academy of Sciences of the United States of America, 2000
897 citations recorded by the source corpus.
Subfields: Ecology, Evolution, Behavior and Systematics, Genetics
View Paper: https://www.semanticscholar.org/paper/d5137967dc4eed8c5ba8985a5024af35992545f1
How researchers see this paper
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In Ecology, Evolution, Behavior and Systematics
- B. Hawkins
- H. Kreft
- Miguel B. Araújo
- Jens‐Christian Svenning
- Carsten F. Dormann
- J. Diniz-Filho
- Kevin J. Gaston
- Walter Jetz
In Genetics
- R. Petit
- A. Hoffmann
- Steven L. Chown
- Miguel B. Araújo
- A. Hampe
- Jens‐Christian Svenning
- Carsten F. Dormann
- G. Vendramin
Citations in the corpus
- Molecular evidence for glacial refugia of mountain plants in the European Alps (2005, background): “Phylogeographic patterns allowed to infer the glacial history of many animals and plants (Comes & Kadereit 1998; Dynesius & Jansson 2000; Hewitt 2000; Davis & Shaw 2001; Kropf et al . 2002, 2003; Stehlik 2003; Tribsch & Schonswetter 2003; Bennett 2004) ranging from organisms of tropical rainforest”
- Genetic differentiation and secondary contact zone in the seagrass Cymodocea nodosa across the Mediterranean–Atlantic transition region (2008, background): “During the LGM (18–10 kyr bp), the Western Mediterranean had colder water temperature and higher thermal amplitude when compared with the more stable Levantine Sea (Thunell, 1979; Hayes et al., 2005) and the Atlantic in the Canaries–Mauritania region (Dynesius & Jansson, 2000).”
- From Europe to Africa and vice versa: evidence for multiple intercontinental dispersal in ribbed salamanders (Genus Pleurodeles) (2004, background): “Recently, the impact of such climatic deterioration following substantial glaciation on amphibian speciation in the Northern hemisphere has been appreciated (Veith et al., 2003a,b; see also Dynesius & Jansson, 2000 for a general model of speciation following glaciation).”
- Post‐Eocene climate change, niche conservatism, and the latitudinal diversity gradient of New World birds (2006, background): “The gradient of both basal and derived groups is further complicated by extinction episodes during the Pleistocene (Dynesius & Jansson, 2000), which could result in lower diversity levels in the north even if speciation rates were as high as in the tropics.”
- The concept of the taxon cycle in biogeography (2002, background): “The Milankovic cycles that drove the ice ages have periods of 23 000, 41 000 and 100 000 years ( Dynesius & Jannson, 2000 ).”
- The influence of paleoclimate on present-day patterns in biodiversity and ecosystems (2015, background): “Because this lag is expected to depend on dispersal ability, communities exposed to high ORD are likely to contain many particularly vagile species (Dynesius & Jansson 2000, Jansson & Dynesius 2002).”
- The Iberian contribution to cryptic diversity in European bats (2006, background): “These periodic pulses have had strong consequences on the evolution of organisms’ life histories (Dynesius and Jansson, 2000).”
- Evolution and the latitudinal diversity gradient: speciation, extinction and biogeography. (2007, background): “Extinction rates are expected to be higher at high latitudes due to climatic variation, but selection for larger species ranges may decrease the probability of extinction (Dynesius & Jansson 2000).”
- Geography determines genetic relationships between species of mountain pine (Pinus mugo complex) in western Europe (2010, background): “These populations are strongly differentiated, and, as southern ‘rear edge’ populations, they may harbour important adaptations relevant to the conservation of the species (Dynesius & Jansson, 2000; Hampe & Petit, 2005).”
- Impacts of climate change on species, populations and communities: palaeobiogeographical insights and frontiers (2008, background): “It has been predicted, however, that orbitally forced climate change on Milankovitch timescales would have had resulted in a reduction in diversity resulting from changes in geographical distributions and local extinctions (Bennett, 1997; Dynesius and Jansson, 2000).”