Reconstructing historical ranges with fossil data at continental scales
By Jason S. McLachlan, James S. Clark. 2004
99 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/3efa02a6c9471984cfacae74c56de586cae8479f
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In Atmospheric Science
In Ecology, Evolution, Behavior and Systematics
- J. P. Grime
- Pamela S. Soltis
- D. Soltis
- Paul S. Manos
- J. Fridley
- G. Vendramin
- Mark Bush
- Frank E. Zachos
In Nature and Landscape Conservation
- J. P. Grime
- Paul S. Manos
- J. Fridley
- Mark Bush
- Jason S. McLachlan
- S. Aitken
- A. Askew
- Sierra Curtis-McLane
Citations in the corpus
- On metapopulations and microrefugia: palaeoecological insights (2011, background): “Subsequent genetic and fossil studies have revealed that in adopting such cut-offs, very important signals 420 Journal of Biogeography 38, 419–429 ª 2011 Blackwell Publishing Ltd may have been discarded among the noise (McLachlan & Clark, 2004, 2005; Hu et al., 2009).”
- Comparative phylogeography of unglaciated eastern North America (2006, background): “However, reconstructions of historical range dynamics (e.g. Davis 1981; Delcourt & Delcourt 1981) are hampered by the fact that pollen is a poor sensor of small populations (McLachlan & Clark 2004).”
- Genetic homogeneity in Juglans nigra (Juglandaceae) at nuclear microsatellites (2006, background): “However, interpretation of the paleoecological evidence is far from unequivocal (e.g., see McLachlan and Clark, 2004).”
- MOLECULAR INDICATORS OF TREE MIGRATION CAPACITY UNDER RAPID CLIMATE CHANGE (2005, background): “Pollen data can fail to identify small or diffuse populations, but they reliably record the distribution of populations once they reach higher densities (Davis et al. 1991, McLachlan and Clark 2004).”
- Comparative phylogeography and population structure of European Betula species, with particular focus on B. pendula and B. pubescens (2007, background): “…there is mounting evidence for the presence of intermediate-latitude refugia, i.e. populations located north of what has been assumed to be the species main refugia and that could also have contributed to recolonization (McLachlan & Clark, 2004; Magri et al., 2006).”
- Soil heterogeneity buffers community response to climate change in species‐rich grassland (2011, background): “…of plant and animal taxa in 'thermal hotspots' in periglacial environments during the Pleistocene is supported by both fossil and genetic data (McLachlan & Clark, 2004; McLachlan et al., 2005; Soltis et al., 2006), and the heterogeneous response of Arctic ecosystems to contemporary climate…”
- Late Neogene history of the laurel tree (Laurus L., Lauraceae) based on phylogeographical analyses of Mediterranean and Macaronesian populations (2009, unknown): “Moreover, the information on past distributions provided by the fossil record might be poorly correlated with the actual palaeodistribution of lowdensity species (McLachlan & Clark, 2004).”
- Fossil evidence and phylogeography of temperate species: ‘glacial refugia’ and post‐glacial recolonization (2009, background): “At the very least, therefore, it should be made absolutely clear in each context which phase of the Quaternary is being referred to when the term glacial refugium is used (see also McLachlan & Clark, 2004; Holderegger & Thiel-Egenter, 2009).”
- Adaptation, migration or extirpation: climate change outcomes for tree populations (2008, background): “…using pollen records showed post-glacial migration rates of up to 200 m per year, but cpDNA evidence of low-density refugial populations of angiosperm trees much farther north than previously thought has caused these estimates to be revised (McLachlan and Clark 2004; McLachlan et al. 2007).”