Cenozoic geological and plate tectonic evolution of SE Asia and the SW Pacific: computer-based reconstructions, model and animations

By R. Hall. 2002

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View Paper: https://www.semanticscholar.org/paper/3cb3839fdac69027430c939b3856966bb3b33e1b

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Citations in the corpus

Evolving force balance during incipient subduction (2004, methodology): “Hall (2001), Tectonic setting of”
The roles of geological history and colonization abilities in genetic differentiation between mammalian populations in the Philippine archipelago (2005, background): “The Philippine archipelago is an especially interesting arena for investigating biological diversification (Heaney, 1986, 1991a,b; Mitchell et al., 1986; Packham, 1996; Hall, 1998, 2002; Steppan et al., 2003).”
Subduction-triggered magmatic pulses: A new class of plumes? (2010, background): “the distribution of the velocity anomaly of Hall and Spakman (2002). VT: Vitiaz Trench,”
Comparative Phylogeography of the Coral Triangle and Implications for Marine Management (2011, background): “At about this time, roughly coincident with the closure of the Tethys Sea, the Australian plate began to collide with island arcs in the Pacific, and the southeast margin of the Eurasian plate, dramatically altering surface circulation and effectively defining the modern basins of the Indian and Pac”
The butterflies of Sulawesi : annotated checklist for a critical island fauna (2003, background): “…of geological evolution The region is of very great interest to geologists, and access to much of the older geological literature, together with valuable accounts of current ideas on the geological history of the area, can be found in Hall & Blundell (1996), Hall & Holloway (1998) and Hall (2002).”
Panbiogeography of New Caledonia, south‐west Pacific: basal angiosperms on basement terranes, ultramafic endemics inherited from volcanic island arcs and old taxa endemic to young islands (2008, background): “Hall (2002) suggested there was no good geological evidence to distinguish between the two alternatives.”
Integrating phylogenetic and taxonomic evidence illuminates complex biogeographic patterns along Huxley’s modification of Wallace’s Line (2010, background): “If one were willing to assume a molecular clock, even with a fast rate of divergence (0.054 Myr)1: Drovetski et al., 2004), these lineages would have been isolated for c. 4–8 Myr.”
Biogeography of the Indo-Australian Archipelago (2011, background): “It began to move rapidly northward from approximately 45 Mya (Hall 2002).”
Evolutionary and biogeographical history of an ancient and global group of arachnids (Arachnida: Opiliones: Cyphophthalmi) with a new taxonomic arrangement (2012, background): “Several lineages may have returned to the Thai-Malay Peninsula or moved between islands around the Cretaceous/ Tertiary boundary during a period in which southeast Asia was subjected to drastic changes and the Indo-Malay Archipelago variously connected (Hall, 2002; Ali & Aitchison, 2008).”
Neogene marine transgressions, palaeogeography and biogeographic transitions on the Thai–Malay Peninsula (2003, background): “Fortunately, this situation has improved recently (Hall & Holloway, 1998; Hall, 2001, 2002) and the evidence now permits a first-order analysis that will hopefully stimulate further research.”
The center of the center of marine shore fish biodiversity: the Philippine Islands (2005, background): “However, these plates were separated during the early Cenozoic (Hall 2002, Figure 4) and the shore faunas on these plates were widely separated and presumably evolved separately.”
Molecular phylogeny of the endemic Philippine rodent Apomys (Muridae) and the dynamics of diversification in an oceanic archipelago (2003, background): “With the exception of one small set (the Palawan group), all of the islands are oceanic in origin, having emerged because of a complex but now well-documented set of tectonic events (Hall, 1996, 1998, 2002).”
Assembly and division of the South and South-East Asian flora in relation to tectonics and climate change (2018, background): “Therefore, to understand the processes involved in the assembly of high diversity in South-East Asia requires knowledge of the tectonic and climatic histories of the region (de Bruyn et al. 2014, Hall 2002, 2009; Morley 2000), and patterns of diversification within individual clades.”
Biogeographical modules and island roles: a comparison of Wallacea and the West Indies (2012, background): “For most of the fragments and volcanic islands, emergence above sea level is relatively recent, that is, < 5 Ma (Audley-Charles, 1993; Monk et al., 1997; Hall, 2002).”
Biogeography and conservation in Southeast Asia: how 2.7 million years of repeated environmental fluctuations affect today’s patterns and the future of the remaining refugial-phase biodiversity (2010, background): “The earlier geological history of the region, including the assembly of the [20 Gondwanan terranes by continental drift, are described elsewhere (Hutchison 1989; Hall 2001, 2002; Metcalfe et al. 2001; Metcalfe 2009).”
Extent and timing of floristic exchange between Australian and Asian rain forests (2011, background): “Because the island of New Guinea is connected to Australia when sea levels are low and is partly a Gondwanan fragment (Hall, 2002), taxa shared between Australia and New Guinea were not counted as disjunct clades unless the taxon extended beyond those land masses.”
West to east dispersal and subsequent rapid diversification of the mega‐diverse genus Begonia (Begoniaceae) in the Malesian archipelago (2012, background): “…the 20th and 21st centuries has supported many of Wallace’s ideas, and the multitude of islands in Malesia indeed differ greatly in their origin, age and their past land connections, as well as in the composition of their floras (Hall, 2002, 2009; van Welzen et al., 2005; van Welzen & Slik, 2009).”
Systematics of a widespread Southeast Asian frog, Rana chalconota (Amphibia: Anura: Ranidae) (2009, background): “Borneo and the Malay Peninsula had broad land connections through most of the Cenozoic (Hall, 1998) and remained approximately at their present latitude throughout that interval (Hall, 2002).”