Regional climate shifts caused by gradual global cooling in the Pliocene epoch
By A. Ravelo, Dyke H. Andreasen, M. Lyle, A. O. Lyle, M. Wara. Nature, 2004
657 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology, Paleontology
View Paper: https://www.semanticscholar.org/paper/f70c4687a081c1ef815a586be00382a0ddf8a592
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In Atmospheric Science
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In Ecology
In Paleontology
Citations in the corpus
- High Earth-system climate sensitivity determined from Pliocene carbon dioxide concentrations (2010, background): “However, an assessment of the timing of oceanographic and climate change”
- Early Pliocene increase in thermohaline overturning: A precondition for the development of the modern equatorial Pacific cold tongue (2010, background): “, 2009], the modern Northern Hemisphere ice cap was absent, and sea level was ∼25 m higher than today [e.g., Raymo et al., 1996; Dowsett et al., 1999; Ravelo et al., 2004; Mudelsee and Raymo, 2005].”
- Slow dynamics of the Northern Hemisphere glaciation (2005, background): “This heterogeneity and the above finding of spatial variations in start, end, and d 18 O amplitude indicate differences on short-term to midterm timescales (� 41– 100 kyr) among regional temperature histories across the NHG (Table 3). This supports the idea that during a global climate change, regio”
- Climate change effects on physiology and population processes of hosts and vectors that influence the spread of hemipteran‐borne plant viruses (2009, background): “Although the Earth’s climate fluctuates for astronomical and geological reasons (Bush et al., 2004; Ravelo et al., 2004; Hansen et al., 2006; Kuper & Kröpelin, 2006; Thompson et al., 2006), the present warming is unprecedented in its speed (Jones et al., 2001), and its very likely cause: the…”
- Complex network approach for recurrence analysis of time series (2009, background): “ 2.3 and 2.0 Ma BP [48]. The Early Pliocene Warm Period ended between 3.3 and 2.8 Ma BP with the Pliocene optimum (3.24–3.05 Ma BP) and the onset of the northern hemisphere glaciation (2.8–2.7 Ma BP) [47, 49], which was intensified during the mid-Pleistocene climate shift at 1.0–0.7 Ma BP [50]. It ha”
- Primate Biogeography and Ecology on the Sunda Shelf Islands: A Paleontological and Zooarchaeological Perspective (2006, neutral): “75 Ma (King, 1996; Ravelo et al., 2004).”