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From Wikipedia, the free encyclopedia

The Older Peron was the name for a period identified in 1961[1] as an episode of a global sea-level (i.e. eustatic) high-stand during the Holocene Epoch.[2][3] Modern understanding of the various factors involved in quantifying eustatic sea level, particularly processes relating to ocean siphoning and glacio-hydro-isostatic adjustment, claim that such previous instances of purported high-stands were not globally coherent, and do not constitute episodes of eustatic sea level higher than present.[4][5]

References

  1. ^ Fairbridge, Rhodes W. (1961). "Eustatic Changes in Sea Level". Physics and Chemistry of the Earth. 4: 99–185. Bibcode:1961PCE.....4...99F. doi:10.1016/0079-1946(61)90004-0.
  2. ^ Lewis, S. E.; Sloss, C. R.; Murray-Wallace, C. V.; Woodroffe, C. D.; Smithers, S. G. (2013). "Post-glacial sea-level changes around the Australian margin: a review". Quaternary Science Reviews. 74: 115–138. Bibcode:2013QSRv...74..115L. doi:10.1016/j.quascirev.2012.09.006.
  3. ^ Wyrwoll, Karl-Heinz; Zhu, Zhongrong; Kendrick, George; Collins, Lindsay; Eisenhauer, Anton (1995). "Holocene Sea-Level Events in Western Australia: Revisiting Old Questions". Journal of Coastal Research (Special Issue 17): 321–326. JSTOR 25735659.
  4. ^ Mitrovica, J. X.; Peltier, W. R. (1991). "On postglacial geoid subsidence over the equatorial oceans". Journal of Geophysical Research. 96 (B12): 20, 053. Bibcode:1991JGR....9620053M. doi:10.1029/91jb01284.
  5. ^ Fleming, Kevin; Johnston, Paul; Zwartz, Dan; Yokoyama, Yusuke; Lambeck, Kurt; Chappell, John (1998). "Refining the eustatic sea-level curve since the Last Glacial Maximum using far- and intermediate-field sites". Earth and Planetary Science Letters. 163 (1–4): 327–342. Bibcode:1998E&PSL.163..327F. doi:10.1016/s0012-821x(98)00198-8.
This page was last edited on 5 October 2021, at 09:30
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