Cenozoic deep-Sea temperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite

By C. Lear, H. Elderfield, P. Wilson. Science, 2000

1,111 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography, Paleontology

View Paper: https://www.semanticscholar.org/paper/5e4e71c6c99ab1f383029a99272a173854603fa3

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Citations in the corpus

Decline of a biome: evolution, contraction, fragmentation, extinction and invasion of the Australian mesic zone biota (2011, neutral): “reviewed extensively elsewhere (Quilty, 1994; Lear et al., 2000; Zachos et al., 2001; Hall, 2002), particularly in relation to the complex spatio-temporal details of the aridification of Australia (Bowler, 1982; Kershaw et al.”
Species-energy relationship in the deep sea: a test using the Quaternary fossil record (2005, background): “Consequently, temperature in the deep-sea is a relatively simple system that is much less affected by seasonal, latitudinal and geographical sources of variation that are so prominent in terrestrial and shallow marine ecosystems ( Lear et al. 2000 ).”
The evolution of arid ecosystems in eastern Africa (2006, background): “There was a significant decline in marine temperatures during the Late Eocene, and an abrupt dip during the Eocene–Oligocene boundary, associated with the initial build up of Antarctic ice (Lear et al., 2000; Zachos et al., 2001; Coxall et al., 2005).”
Eocene bipolar glaciation associated with global carbon cycle changes (2005, background): “(4) The decrease in benthic and bulk carbonate d(18)O (grey interval) indicates deglaciation.”
The solid Earth’s influence on sea level (2013, background): “Seawater cooling by ~12 °C (Lear et al., 2000) also likely caused an additional ~12 m of sea-level drop (Miller et al., 2009).”
Hysteresis in Cenozoic Antarctic ice-sheet variations (2005, positive): “: +1 413 545 3426; fax: +1 413 865 1200. sea core records of d18O and Mg/Ca in benthic foraminifera (Zachos et al., 2001; Lear et al., 2000).”
Global climate change and North American mammalian evolution (2000, background): “Similarly, the highly averaged isotopic records used in our analysis do show major features that have been interpreted in the past as evidence for global climatic change, such as the Paleocene/Eocene boundary event, the Eocene thermal maximum, warming/ice volume decrease in the early Miocene, and sh”
Cenozoic sea-level and cryospheric evolution from deep-sea geochemical and continental margin records (2020, background): “GMSL higher than 12 m above modern requires loss of ice sheets in Greenland, West Antarctica, and sensitive areas of East Antarctica, the Wilkes, and Aurora Basins (70).”
Evolution and diversity of the benthic fauna of the Southern Ocean continental shelf (2004, background): “2b: Lear et al. 2000).”
Sea ice feedback and Cenozoic evolution of Antarctic climate and ice sheets (2007, background): “[8] This paper addresses the role of sea ice in the climatic and glacial evolution of the Antarctic region through the Cenozoic, including the sometimes sudden variations in the Cenozoic ice volume inferred from benthic marine oxygen isotope and Mg/Ca records [Billups and Schrag, 2003; Coxall et al.”
The origin and evolution of tertiary relict floras (2002, background): “Datisca 10–40a Isozymes and Subhumid Liston et al. cpDNAa (1989a) Liston et al.”