Where and why have all the flowers gone? Depletion and turnover in the New Zealand Cenozoic angiosperm flora in relation to palaeogeography and climate
By Daphne E. Lee, William G. Lee, N. Mortimer. 2001
217 citations recorded by the source corpus.
Subfields: Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation
View Paper: https://www.semanticscholar.org/paper/c3eefc864b4e1a70c6a4671dfe10576cb9f228e3
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In Ecology, Evolution, Behavior and Systematics
- Andrew Lowe
- Sarah J. Richardson
- Hugh P. Possingham
- M. Crisp
- Gregory J. Jordan
- P. Heenan
- Gunnar Keppel
- L. Cook
In Nature and Landscape Conservation
- M. Crisp
- Andrew Lowe
- Sarah J. Richardson
- Hugh P. Possingham
- Gregory J. Jordan
- P. Heenan
- Gunnar Keppel
- L. Cook
Citations in the corpus
- Comparative biogeography of New Zealand trees: species richness, height, leaf traits and range sizes (2010, background): “The first major impact of the glacials appears to have been a wave of tree extinctions (Mildenhall 1980; Markgraf & McGlone 2005), although a considerable reduction of tree genera occurred earlier during the late Tertiary (Lee et al. 2001).”
- Changing perspectives on the biogeography of the tropical South Pacific: influences of dispersal, vicariance and extinction (2009, background): “Similarly, there is debate about what fraction of the biota survived the high Oligocene sea levels in New Zealand and New Caledonia (Pole, 1994; Cooper & Cooper, 1995; Hickson et al., 2000; Lee et al., 2001, 2007; McGlone et al., 2001; Landis et al., 2008).”
- Evolution of New Zealand alpine and open-habitat plant species during the late Cenozoic (2013, background): “The extinction of cold-intolerant species is well documented during the Pliocene, with at least 15 families and 36 genera from the warm-temperate and humid climates of the Miocene being documented in the fossil record for the last time (e.g. Mildenhall & Pocknall 1989; Lee et al. 2001).”
- Directional asymmetry of long‐distance dispersal and colonization could mislead reconstructions of biogeography (2005, background): “Although the two land masses first separated 85 Ma (Kroenke, 1996; Lee et al., 2001), when New Zealand rifted from Antarctica, they are currently separated by only 2000 km of ocean – a distance that has been relatively stable for 55–60 Ma (Pole, 1994; Kroenke, 1996).”