The breakup history of Gondwana and its impact on pre-Cenozoic floristic provincialism

By S. McLoughlin. 2001

782 citations recorded by the source corpus.

Subfields: Ecology, Evolution, Behavior and Systematics, Nature and Landscape Conservation, Paleontology

View Paper: https://www.semanticscholar.org/paper/ff2f2cc4b0244e8923818c8c06906eb6200b89b8

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Citations in the corpus

Marine dispersal as a pre‐requisite for Gondwanan vicariance among elements of the galaxiid fish fauna (2012, background): “This could apply to the ancestor of Aplochiton and Lovettia, which may have maintained a period of marine connectivity between Australia and South America following continental fragmentation 52 Ma, given the overlapping range of lineage divergence time estimates (Fig.”
Geographical affinities of the Cape flora, South Africa (2006, background): “The Kerguelen Plateau may have provided a mid-ocean stepping stone (Sampson et al., 1998; Cooper et al., 2001; McLoughlin, 2001).”
Phylogenetic systematics of the Gondwanan nephilid spider lineage Clitaetrinae (Araneae, Nephilidae) (2006, background): “29) suggests the area cladogram ((Africa + Madagascar with adjacent islands) + Indian subcontinent), which does not agree with the currently understood continental drift theory (Brown & Lomolino 1998; McLoughlin 2001), because Indian and Madagascar species do not group.”
Extent and timing of floristic exchange between Australian and Asian rain forests (2011, background): “Arrows show times of divergence (solid arrows) and convergence (dashed arrows) between land masses (McLoughlin, 2001; Hall, 2002).”
Review of plant biogeographic studies in Brazil (2009, background): “After the initial development of the South Atlantic Ocean ca. 135 mya (McLoughlin, 2001), northern South America and Africa remained connected until 110–95 mya (Sanmartı́n & Ronquist, 2004), and some island chains may have permitted dispersal routes for floristic exchanges between the two…”
Parasitic angiosperms: How often and how many? (2020, positive): “The age for Hydnora roughly corresponds to a Gondwana breakup model that shows South America and northwest Africa remaining in contact till ca. 110 mya (McLoughlin, 2001; Seton & al., 2012).”
Clades, Clocks, and Continents: Historical and Biogeographical Analysis of Myrtaceae, Vochysiaceae, and Relatives in the Southern Hemisphere (2004, background): “…Passage between Antarctica and South America nor the passage between Australia and S98 INTERNATIONAL JOURNAL OF PLANT SCIENCES Antarctica was open at 40 Ma, but both passageways were open to middle and deep water circulation by the early Oligocene (32 Ma) (Lawver and Gahagan 1998; McLoughlin 2001).”
Vicariance or long‐distance dispersal: historical biogeography of the pantropical subfamily Chrysophylloideae (Sapotaceae) (2011, background): “These studies demonstrate that the timing of the diversification of those families is incongruent with the breakup sequence of Gondwana (McLoughlin, 2001).”
Out of the Palaeotropics? Historical biogeography and diversification of the cosmopolitan ectomycorrhizal mushroom family Inocybaceae (2009, background): “Because none of these taxa exhibits ages older than 80 Myr, vicariance between Australia and New Zealand is rejected (McLoughlin, 2001).”
Hello New Zealand (2006, background): “, 1988), ‘New Zealand Plateau’ (NIWA) and Tasmantia (Storey, 1996; McLoughlin, 2001), but none of these terms have found as much favour as Zealandia.”
Biogeography and phylogeny of the New Zealand cicada genera (Hemiptera: Cicadidae) based on nuclear and mitochondrial DNA data (2004, background): “Dettman & Jarzen (1990) suggested that organisms may have been able to island hop between New Caledonia and New Zealand via the Kermadec and Colville ridges until c. 40 Ma. A different route is suggested by the geological data of Herzer et al. (1997) who found evidence for a series of long low islan”
A dated molecular perspective of eucalypt taxonomy, evolution and diversification (2019, background): “…with this new older date, is how newcalypt(s) persisted on land in the Pacific during the time that New Caledonia was subducted between 60 and 37 million years ago (McLoughlin 2001; Ladiges andCantrill 2007; Grandcolas et al. 2008; Thornhill et al. 2015), before arriving to 10where they are extant.”