Deterministic Plio‐Pleistocene extinctions in the European cool‐temperate tree flora
By Jens‐Christian Svenning. 2003
310 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/af49b5d9b1a123ebd1cd5f37b312ef0d01b16725
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- A. Hampe
- D. Nogués-Bravo
- Miguel B. Araújo
- R. Ricklefs
- R. Petit
- S. Normand
- F. Médail
- Jonathan Lenoir
In Ecology, Evolution, Behavior and Systematics
- A. Hampe
- R. Ricklefs
- Jens‐Christian Svenning
- C. Rahbek
- Miguel B. Araújo
- D. Nogués-Bravo
- James M Sobel
- F. Rodríguez‐Sánchez
In Nature and Landscape Conservation
- Jens‐Christian Svenning
- C. Rahbek
- A. Hampe
- D. Nogués-Bravo
- Miguel B. Araújo
- C. Hof
- S. Normand
- Camilla Fløjgaard
Citations in the corpus
- Applications of species distribution modeling to paleobiology (2011, background): “For details on the SDM, see Svenning et al. (2008a). LGM ice sheet extent (light blue area) follows Ehlers and Gibbard (2004).”
- Macroecological patterns of species and genetic diversity in vascular plants of the Mediterranean basin (2010, background): “Climate explains well the maintenance or disappearance of species during the Pleistocene glacial cycles (Huntley, 1993; Svenning, 2003), with plant species richness increasing with topographical heterogeneity in southern Europe (Svenning et al.”
- From Mediterranean shores to central Saharan mountains: key phylogeographical insights from the genus Myrtus (2012, background): “During the Neogene, the progressive climatic transition from the warm conditions that characterized the early Miocene to the cooler Pleistocene period (Fauquette et al., 1999; van Dam, 2006) led to a decrease in habitat suitable for plants with ‘tropical affinities’ (Herrera, 1992; Svenning, 2003).”
- A comprehensive framework for global patterns in biodiversity (2004, background): “…Asia, eastern North America, and Europe clearly reflect the isolation of North America from Tertiary centres of tree diversification in Eurasia and rapid late Tertiary climate cooling in the disappearance of species from the flora of Europe (Sauer 1988; Latham & Ricklefs 1993a; Svenning 2003).”
- Reconstructing the demise of Tethyan plants: climate‐driven range dynamics of Laurus since the Pliocene (2008, background): “Madrean taxa in Europe (Svenning, 2003).”
- Past tree range dynamics in the Iberian Peninsula inferred through phylogeography and palaeodistribution modelling: A review (2010, unknown): “( Svenning, 2003; Martínez-Meyer and Peterson, 2006).”
- Conserving biodiversity under climate change: the rear edge matters. (2005, background): “Svenning (2003) showed recently, in a thorough analysis of the Northwest European Tertiary tree flora, that only the most climate-tolerant genera were able to cope with Quaternary climate oscillations, whereas cold-sensitive but relatively drought-tolerant genera are now restricted to the southern…”
- Evolution and the latitudinal diversity gradient: speciation, extinction and biogeography. (2007, background): “Negative impacts of cooling climates on diversity at high latitudes have been documented during the late Tertiary for terrestrial plants (Sauer 1988; Latham & Ricklefs 1993; Svenning 2003 ).”
- Latitudinal and Elevational Range Shifts under Contemporary Climate Change (2013, background): “environment (niche shift) (Davis and Shaw, 2001); (3) go extinct (Svenning, 2003); or some combination of these responses.”
- Rethinking species' ability to cope with rapid climate change (2011, background): “5 million years to the present) did not cause a noticeable level of broad-scale, continent-wide extinctions of species; instead, it appeared to primarily affect a few specific groups, mainly large mammals (Koch & Barnosky, 2006) and European trees (Svenning, 2003).”