Sunda Shelf

Biogeographically, Sundaland is a term for the region of Southeastern Asia which encompasses these areas of the Asian continental shelf that were exposed during the last ice age. Sundaland included the Malay Peninsula on the Asian mainland, as well as the large islands of Borneo, Java, and Sumatra, and their surrounding islands. The same steep undersea gradients that mark the eastern boundary of Sundaland are identified biogeographically by the Wallace Line, identified by Alfred Russel Wallace, which marks the eastern boundary of Asia's land mammal fauna, and is the boundary between the Indomalayan and Australasian realms. The shelf has resulted from millennia of volcanic activity and erosion of the Asian continental mass, and the build up and consolidation of debris along the margins as sea levels rose and fell. It lies on its own tectonic plate, the Sunda plate. during the Last Glacial Maximum The seas between the islands cover relatively stable ancient peneplains that are characterised by low seismicity, low isostatic gravity anomalies and no active volcanoes with the exception of Sumatra, Java, and Bali, which while connected to the Sunda Shelf, belong geologically to the young Sunda Arc orogenic system (i.e., the Sunda Mountain System). Present sea levels submerge a number of Pleistocene paleo river systems that drained much of Sundaland during the last glacial maximum 18,000 to 20,000 years ago. To the east of the Sunda Shelf is the Sahul Shelf. Separating these two regions of shallow seas is Wallacea, which encompasses Sulawesi and the thousands of smaller islands making up Nusa Tenggara and Maluku. Within Wallacea lie some of the deepest seas in the world, with depths of up to 7,000 metres. Passing between Bali and Lombok, and Borneo and Sulawesi, Wallacea is marked by a transition zone of flora and fauna first described by Alfred Russel Wallace. W. Earle in 1845 was the first to describe the general features of the Sunda and Sahul Shelves, which he termed the "Great Asiatic Bank" and the "Great Australian Bank" respectively. ==Submerged river systems==

The paleo river systems of the Sunda Shelf are vast submerged river systems that extend present-day river systems and may be interpreted to follow topographic lows in a down-slope direction. During the driest period of the Pleistocene era (about 17,000 years BP) some four distinct catchment areas form the Malacca, Siam and Sunda river systems. The Siam river system consists of a northern and a western arm. The northern arm extends the Chao Phraya River to drain the Gulf of Thailand. The western arm forming out of some rivers in central Sumatra flows through the Singapore Straits before joining up with the northern arm to empty into an estuary and the South China Sea to the north of North Natuna Island. The Malacca Straits river system is formed by a joining of waters from northeastern Sumatra and the western Malay Peninsula, draining into the Andaman Sea. The Northern Sunda river system, also known as the Great Sunda river system, or Molengraaff river system, was named after a Dutch biologist and geologist who traveled the region extensively in the late 19th century and first proposed the existence of this river system based on his observations in Borneo. The river, arising between Belitung Island and Borneo, flowed in a northeasterly direction, where it collected waters from some rivers in Central Sumatra and the rivers in Western and Northern Borneo, before flowing into the South China Sea between the North and South Natuna Islands. Finally the Eastern Sunda river system emptied northern Java and southern Borneo, flowing in an easterly direction between Borneo and Java into the Java Sea. ==See also==