Rapid flooding of the sunda shelf: A late-glacial sea-level record

By T. Hanebuth, K. Stattegger, P. Grootes. Science, 2000

913 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Geology

View Paper: https://www.semanticscholar.org/paper/aad5e14d0d0bb9d6036685dde829d6d39140534c

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In Atmospheric Science

In Earth-Surface Processes

W. Richard Peltier

In Geology

Citations in the corpus

A geophysically constrained large ensemble analysis of the deglacial history of the North American ice-sheet complex (2004, background): “A key issue that has yet to be resolved is the eustatic sea-level contribution from NA that contributed to the approximately 120–130 m LGM drop inferred on the basis of the Barbados and Sunda Shelf records (Fairbanks, 1989; Bard et al., 1990; Hanebuth et al., 2000) as discussed in Peltier (2002b).”
Shifting seas: the impacts of Pleistocene sea‐level fluctuations on the evolution of tropical marine taxa (2015, background): “Low sea levels culminated in coastlines 115–130 m below current level, reaching a minimum during the Last Glacial Maximum (LGM) c. 17–19 ka (Fairbanks, 1989; Hanebuth et al., 2000; Voris, 2000; Bintanja et al., 2005; Bintanja & van de Wal, 2008; Clark et al., 2009).”
The late Quaternary extinction and future resurrection of birds on Pacific islands (2003, background): “Changes in sea level were drastic (ca. 118–135 m) during the glacial– interglacial transition from ca. 20 to 8 Cal BP (Clark and Mix 2000; Hanebuth et al., 2000).”
Neogene marine transgressions, palaeogeography and biogeographic transitions on the Thai–Malay Peninsula (2003, background): “Details of the local course of post-glacial flooding are provided by Hanebuth et al. (2000) who report a mean sea level of )96 m at 14.6 ka, )80 m at 14.3 ka, )64 m at 13.1 ka and )50 m at c. 11 ka.”
Mollusc Shell Encrustation and Bioerosion Rates in a Modern Epeiric Sea: Taphonomy Experiments in the Java Sea, Indonesia (2002, background): “Pulau Panjang is a nearshore coral cay, with about 80% carbonate content, subject to anthropogenic eutrophication from sewage, agricultural runoff, and aquacultural effluent (Edinger et al., 1998; Heikoop et al., 2000).”
Global glacial isostatic adjustment: palaeogeodetic and space‐geodetic tests of the ICE‐4G (VM2) model (2002, background): “Firstly, we require significant additional continental ice in the model in order to fit the new constraints on the LGM depression of eustatic sea level provided by the Sunda Shelf and Bonaparte Gulf observations (it is also critical that we can achieve this and remain compatible with the data set fr”
Primate Biogeography and Ecology on the Sunda Shelf Islands: A Paleontological and Zooarchaeological Perspective (2006, background): “A sea level curve based on sediment analysis from the Sunda Shelf documents an increase in sea level between 19–13 ka (from −114 to −64 m) (Hanebuth et al., 2000).”
Comparative Phylogeography of the Coral Triangle and Implications for Marine Management (2011, background): “The Sunda and Arafura shelves represent the largest tropical continental shelf area on earth [49].”
Wallace's Line and plant distributions: two or three phytogeographical areas and where to group Java? (2011, background): “In the Malay Archipelago (or Malesia; Raes & Van Welzen, 2009) a famous zoological boundary based on the biogeographical work of Wallace is found (i.e. Wallace’s Line), with the name being coined by Huxley (1868). The line (Fig.”