Cited by 1,968Geology and Paleoclimatology ResearchGeological formations and processesMarine and environmental studies

Maps of Pleistocene sea levels in Southeast Asia: shorelines, river systems and time durations

Voris, Harold K.·2000·Journal of Biogeography

Abstract

Aim Glaciation and deglaciation and the accompanying lowering and rising of sea levels during the late Pleistocene are known to have greatly affected land mass configurations in Southeast Asia. The objective of this report is to provide a series of maps that estimate the areas of exposed land in the Indo‐Australian region during periods of the Pleistocene when sea levels were below present day levels. Location The maps presented here cover tropical Southeast Asia and Austral‐Asia. The east–west coverage extends 8000 km from Australia to Sri Lanka. The north–south coverage extends 5000 km from Taiwan to Australia. Methods Present‐day bathymetric depth contours were used to estimate past shore lines and the locations of the major drowned river systems of the Sunda and Sahul shelves. The timing of sea level changes associated with glaciation over the past 250,000 years was taken from multiple sources that, in some cases, account for tectonic uplift and subsidence during the period in question. Results This report provides a series of maps that estimate the areas of exposed land in the Indo‐Australian region during periods of 17,000, 150,000 and 250,000 years before present. The ancient shorelines are based on present day depth contours of 10, 20, 30, 40, 50, 75, 100 and 120 m. On the maps depicting shorelines at 75, 100 and 120 m below present levels the major Pleistocene river systems of the Sunda and Sahul shelves are depicted. Estimates of the number of major sea level fluctu…

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Crossref · 10.1046/j.1365-2699.2000.00489.x

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  • On the Sunda Shelf, freshwater connections probably occurred between various regions, including Southeast Asia, eastern Peninsula Malaysia, and parts of Borneo and Sumatra, although a central ridge in the Java Sea separated some areas.

    “On the Sunda Shelf, freshwater connections probably occurred between various regions, including Southeast Asia, eastern Peninsula Malaysia, and parts of Borneo and Sumatra, although a central ridge in the Java Sea separated some areas [58,59].”
  • At the height of the last glacial maximum, the Indo-Pacific Sea level dropped about 120 m, exposing the Sunda and Sahul shelves and isolating marine and coastal faunas of the Indian and Pacific Ocean.

    “At the height of the last glacial maximum, the Indo-Pacific Sea level dropped about 120 m, exposing the Sunda and Sahul shelves and isolating marine and coastal faunas of the Indian and Pacific Ocean [58,60].”

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Authors
Voris, H. K.
Affiliations
Field Museum of Natural History (US)
Corresponding author
Voris, Harold K.
Venue
Journal of Biogeography
Publisher
Wiley
Published
2000-09
Volume
27
Issue
5
Pages
1153-1167
ISSN
  • 0305-0270 (ISSN-L)
  • 1365-2699
OpenAlex
W2128408957
Cited by
1,968
References
0
Citations by year
2026: 69 · 2025: 81 · 2024: 72 · 2023: 87 · 2022: 99 · 2021: 129 · 2020: 98 · 2019: 102 · 2018: 140 · 2017: 108 · 2016: 112 · 2015: 79 · 2014: 103 · 2013: 101 · 2012: 78
FWCI
12.34
Type
journal article
Language
en
Open access
closed
Locations
Journal of Biogeography (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Earth-Surface Processes › Geological formations and processes
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and environmental studies
Keywords
Pleistocene sea level, sea-level change, paleoshorelines, Sunda Shelf, Sahul Shelf, Indo-Australian region, sea-level fluctuations, tectonic uplift and subsidence, tropical Southeast Asia

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