Sea-level changes during the late Pleistocene and Holocene in the Strait of Malacca

Geyh, Mebus A.; Streif, Hansjörg; Kudrass, H. R.

doi:10.1038/278441a0

Cited by 231 publications

(154 citation statements)

References 8 publications

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“…Abrasion platforms and sea-level notches are used to assess the indicative meaning of possible raised shorelines in the region. Tija ( 1996) draws a sea-level envelope based on 130 radiocarbon dated shoreline indicators that would appear to suggest a sea-level highstand of up to 5m, in agreement with Geyh et al (1979). The reconstruction also shows two sea-level highstands as demonstrated by Bezerra et al (2003) and Baxter and Meadows (1999).…”

Section: Geomorphological Approachmentioning

confidence: 60%

Mangrove pollen of Indonesia and its suitability as a sea-level indicator

et al. 2007

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The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source• a link is made to the metadata record in Durham E-Theses• the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Mangrove Pollen of Indonesia and its Suitability as a Sea-Level IndicatorThe copyright of this thesis rests with the author or the university to which it was submitted. No quotation from it, or information derived from it may be published without the prior written consent of the author or university, and any information derived from it should be acknowledged. Simon Edward EngelhartThesis The copyright of this thesis rests with the author. No quotations from it should be published without his prior written consent and information derived from it should be acknowledged.11 AcknowledgemeBlts I would like to thank all those people who have helped in the production of this thesis.

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Section: Geomorphological Approachmentioning

confidence: 60%

Mangrove pollen of Indonesia and its suitability as a sea-level indicator

et al. 2007

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“…Investigations of Holocene RSL in the far-field region of Asia are concentrated in southeast Asia [150][151][152][153], although studies have expanded in recent years to include South Korea [154], the Philippines [155], China [145 -148], the MalayThai peninsula [160 -164 ], and Japan [165 ]. These records are characterized by a mid-Holocene highstand attributed to hydro-isostatic processes [166,167 ], which varies in magnitude and timing of initiation.…”

Section: Asiamentioning

confidence: 99%

“…Holocene studies from the Malay-Thai peninsula suggest a RSL highstand of up to 5 m between 6 and 4 ka, which may have exhibited an oscillatory subsequent fall [153,160,164,[169][170][171][172][173]. The highstand varies in magnitude by 3 to 4 m due to spatial variability from hydro-isostasy [167 ].…”

Section: Asiamentioning

confidence: 99%

Holocene Relative Sea-Level Changes from Near-, Intermediate-, and Far-Field Locations

Khan

Ashe

Shaw

et al. 2015

Curr Clim Change Rep

117

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Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic (glacio-and hydro-) factors. We fit RSL histories from near-, intermediate-, and far-field locations with noisy-input Gaussian process models to assess rates of RSL change. Records from near-field regions (e.g., Antarctica, Greenland, Canada, Sweden, and Scotland) reveal a complex pattern of RSL fall from a maximum marine limit due to the net effect of eustatic sea-level rise and glacio-isostatic uplift with rates of RSL fall as great as −69±9 m/ka. Intermediatefield regions (e.g., mid-Atlantic and Pacific coasts of the USA, Netherlands, Southern France, St. Croix) display variable rates of RSL rise from the cumulative effect of eustatic and isostatic factors. Fast rates of RSL rise (up to 10±1 m/ka) are found in the early Holocene in regions near the center of forebulge collapse. Far-field RSL records exhibit a midHolocene highstand, the timing (between 8 and 4 ka) and magnitude (between <1 and 6 m) of which varies among South America, Africa, Asia, and Oceania regions.

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“…As in A. indicus (Tables 5,10 & 11), A. serrulatus appears to have also undergone late-Pleistocene expansion, due to the fluctuating sea levels (Wong 2013). The estimates of the time since the most recent population expansion event for A. serrulatus took place approximately 61000-28000 years ago, coinciding with rising sea levels during the late Pleistocene (Geyh et al 1979;Hanebuth et al 2000;Voris 2000).…”

Section: Intraspecific Variation Of Acetes Speciesmentioning

confidence: 99%