Sea-level changes in the tectonically stable Malay-Thai Peninsula

Tjia, H. D.

doi:10.1016/1040-6182(95)00025-e

Cited by 152 publications

(126 citation statements)

References 2 publications

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“…The divergence was further complicated by the fact that Borneo remained as part of Asian mainland (linked to the Asian mainland through Peninsular Malaysia and Sumatra) before the Miocene or Pliocene (Wilson and Moss, 1999;Hall, 2001). The paleographical data obtained also showed that the migration of life forms on the Asian mainland and Sundaland was enabled through land bridges during the Pleistocene period (Sartono, 1973;Heaney, 1986;Tjia, 1996). Therefore, the cladogenic activity in Borneo made it possible for the primates to migrate to Sumatra and Java, Indonesia and Peninsular Malaysia through the land bridges connecting them.…”

Section: Discussionmentioning

confidence: 85%

Phylogenetic relationships of leaf monkeys (Presbytis; Colobinae) based on cytochrome b and 12S rRNA genes

Vf¹,

Mc²,

Lakim³

et al. 2011

Genet. Mol. Res.

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ABSTRACT.Little is known about the classification and phylogenetic relationships of the leaf monkeys (Presbytis). We analyzed mitochondrial DNA sequences of cytochrome b (Cyt b) and 12S rRNA to determine the phylogenetic relationships of the genus Presbytis. Gene fragments of 388 and 371 bp of Cyt b and 12S rRNA, respectively, were sequenced from samples of Presbytis melalophos (subspecies femoralis, siamensis, robinsoni, and chrysomelas), P. rubicunda and P. hosei. The genus Trachypithecus (Cercopithecidae) was used as an outgroup. The Cyt b NJ and MP phylogeny trees showed P. m. chrysomelas to be the most primitive, followed by P. hosei, whereas 12S rRNA tree topology only indicated that these two species have close relationships with the other members of the genus. In our analysis, chrysomelas, previously classified as a subspecies of P. melalophos, was not included in either the P. m. femoralis clade or the P. m. siamensis clade. Whether or not there should be a separation at the species level remains to be clarified. The tree topologies also showed that P. m. siamensis is paraphyletic with P. m. robinsoni, and P. m. femoralis with P. rubicunda, in two different Phylogenetic relationships of Presbytis clades. Cyt b and 12S rRNA are good gene candidates for the study of phylogenetic relationships at the species level. However, the systematic relationships of some subspecies in this genus remain unclear.

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Section: Discussionmentioning

confidence: 85%

Phylogenetic relationships of leaf monkeys (Presbytis; Colobinae) based on cytochrome b and 12S rRNA genes

Vf¹,

Mc²,

Lakim³

et al. 2011

Genet. Mol. Res.

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“…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

125

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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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“…RSL reconstructions from far-field sites exhibit differing responses to eustatic change due to the principles of equatorial ocean siphoning and continental levering advanced by Mitrovica and Milne (2002). These principles may be responsible for how far-field sites respond to eustatic change with certain sites exhibiting a midHolocene highstand (Nunn 2000), a double mid-Holocene highstand (Tija 1996) or no highstand (Kayanne et al 1993). The unfiltered eustatic signal that far-field sites can provide has resulted in a large number of research projects concentrating on these areas to understand the deglacia1 chronology of the polar ice sheets.…”

Section: Far-field Sitesmentioning

confidence: 99%

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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Sea-level changes in the tectonically stable Malay-Thai Peninsula

Cited by 152 publications

References 2 publications

Phylogenetic relationships of leaf monkeys (Presbytis; Colobinae) based on cytochrome b and 12S rRNA genes

Phylogenetic relationships of leaf monkeys (Presbytis; Colobinae) based on cytochrome b and 12S rRNA genes

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

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

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