Timing of the Last Glacial Maximum from observed sea-level minima

By Yusuke Yokoyama, K. Lambeck, P. Deckker, P. Johnston, L. Fifield. Nature, 2000

951 citations recorded by the source corpus.

Subfields: Anthropology, Atmospheric Science, Earth-Surface Processes

View Paper: https://www.semanticscholar.org/paper/1bde894683a177a80b6de724781a377d868d2f0d

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Citations in the corpus

Global glacial isostatic adjustment: palaeogeodetic and space‐geodetic tests of the ICE‐4G (VM2) model (2002, background): “2b and c, are additional intercomparisons with two recently published relative sea-level records from the western equatorial Pacific Ocean, respectively from the Sunda Shelf (Hanebuth et al., 2000) and from Bonaparte Gulf (Yokoyama et al., 2000).”
High genetic diversities and complex genetic structure in an Indo-Pacific tropical reef fish (Chlorurus sordidus): evidence of an unstable evolutionary past? (2004, background): “…sea levels driven by cycles of glaciation profoundly affected coral reef habitats and the patterns of connectivity amongst their resident biota, especially in the western Pacific region of the Indo-Australia archipelago (Palumbi 1994; Benzie 1999; Lambeck and Chappell 2001; Yokoyama et al. 2000).”
Sea-level probability for the last deglaciation: A statistical analysis of far-field records (2011, background): “…and Polach, 1991; Cutler et al., 2003; Fairbanks et al., 2005, Peltier and Fairbanks, 2006), and on plant fragments and calcareous marine organisms contained within marine sediment cores (Hanebuth et al., 2000, 2009; Yokoyama et al., 2000, 2001; Toscano and Macintyre, 2003 and references therein).”
Glacial isostatic adjustment on 3‐D Earth models: a finite‐volume formulation (2005, background): “The excess volume of ice at the LGM was sufficient to lower global sea levels by ∼130 m (Yokoyama et al. 2000) and the subsequent deglaciation event, which ended ∼5000 BP, initiated a period of dramatic disequilibrium and adjustment in the Earth system that persists to the present day.”
Links between climate and sea levels for the past three million years (2002, background): “; this period constitutes the LGM when land-based ice volumes were ∼55 × 10 6 km 3 greater than presen”