Evolution of Ocean Temperature and Ice Volume Through the Mid-Pleistocene Climate Transition
By H. Elderfield, P. Ferretti, M. Greaves, S. Crowhurst, I. McCave, D. Hodell, A. Piotrowski. Science, 2012
817 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/1f37b3791eaa4d169f6a3b5b06e1ad4db0779e6b
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
- Robert M. DeConto
- Frank Pattyn
- F. Parrenin
- Catherine Ritz
- Stefan Rahmstorf
- M. Raymo
- G. Milne
- R. Mulvaney
In Ecology
- W. Ludt
- Robert M. DeConto
- Luiz A. Rocha
- Stefan Rahmstorf
- Jonathan Aitchison
- J. Severinghaus
- J. Ali
- Brian W. Bowen
In Oceanography
- Robert M. DeConto
- Luiz A. Rocha
- Stefan Rahmstorf
- M. Raymo
- G. Milne
- P. Clark
- R. Mulvaney
- P. Whitehouse
Citations in the corpus
- Shifting seas: the impacts of Pleistocene sea‐level fluctuations on the evolution of tropical marine taxa (2015, background): “The timing of sea-level fluctuations also shifted throughout the Pleistocene, occurring approximately every 41 kyr prior to the mid-Pleistocene transition 900 ka, and Journal of Biogeography 42, 25–38 ª 2014 John Wiley & Sons Ltd 26 every 100 kyr since (Elderfield et al., 2012).”
- Exploring the combined role of eustasy and oceanic island thermal subsidence in shaping biodiversity on the Galápagos (2014, background): “Since at least 700 ka, sea level has for 5–10 kyr intervals every c. 100 kyr fallen to between about 90 and 130 m below the present datum (Bintanja et al., 2005; Rohling et al., 2009; Elderfield et al., 2012).”
- Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core (2013, background): “The sequence of the last 8 glacial cycles documented in natural paleoclimate archives (Lisiecki and Raymo, 2005; Wang et al., 2008; Wolff et al., 2006; EPICA community members, 2006; Pahnke and Zahn, 2005; Elderfield et al., 2012) is characterized by irregular 100 000 yr cycles, whose association to”
- Sea-level rise due to polar ice-sheet mass loss during past warm periods (2015, background): “By comparison, paired d(18)O-Mg/Ca measurements of benthic foraminifera suggest GMSL duringMIS 11 in excess of 50 ± ~20 m above present (31, 54), although, as with the MPWP reconstructions, the uncertainties on these estimates may be much larger.”