1996
DOI: 10.1016/0034-4257(95)00226-x
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Mesoscale circulation features of the great barrier reef region inferred from NOAA satellite imagery

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Cited by 45 publications
(36 citation statements)
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“…The first is environmental changes in water temperature associated with post-Pleistocene climate variation. The geographical range disjunction between the two Cryptasterina species in Australia is about 375 km and approximately coincides with the location where colder eastern Pacific waters mix with warmer tropical waters transported by the East Australian Current (EAC) [58]. Our estimate of 6000 ypb for the speciation event is much more recent than the last glacial maximum (LGM), but it coincides with other significant Holocene oceanographic events.…”
Section: Discussionsupporting
confidence: 53%
See 1 more Smart Citation
“…The first is environmental changes in water temperature associated with post-Pleistocene climate variation. The geographical range disjunction between the two Cryptasterina species in Australia is about 375 km and approximately coincides with the location where colder eastern Pacific waters mix with warmer tropical waters transported by the East Australian Current (EAC) [58]. Our estimate of 6000 ypb for the speciation event is much more recent than the last glacial maximum (LGM), but it coincides with other significant Holocene oceanographic events.…”
Section: Discussionsupporting
confidence: 53%
“…We hypothesize that a small number of C. pentagona individuals or larvae were able to colonize the presentday range of C. hystera, and that this habitat [58] provided a divergent selective regime that led to the loss of planktonic development and other associated life-history changes, with reproductive isolation and speciation as a consequence. The speed of this speciation event suggests that it occurred via selection upon preexisting genetic variation on an ecological time scale, because it is unlikely that a complex suite of derived life-history characters including hermaphroditism, selfing and live-bearing could so quickly evolve via drift-and mutation-driven processes [9,63,64].…”
Section: Discussionmentioning
confidence: 99%
“…Even in dense reef areas of the GBR (i.e., areas with a large ratio of reef area to the area between the reefs), such as the Swains reefs, an inflow from the adjacent Coral Sea can be traced. In this paper we have only presented two examples of extensive intrusion in the GBR but such intrusions had already been reported in the literature [Burrage et al, 1996;Brinkman et al, 2002]. More work is needed using satellite imagery to analyze the frequency of these intrusions, however the data presented here support the proposition that, on occasions, very large water exchange events occur.…”
Section: Description Of the Drifter Trajectories In The Gbrsupporting
confidence: 50%
“…In the southern GBR, evidence of oceanic waters intruding inside the lagoon can be seen on the Chl-a images but associated with colder waters. These have been attributed to upwelling events taking place along the Capricorn Bunker shelf and in the mouth of the Capricorn Channel [Kleypas and Burrage, 1994;Burrage et al, 1996]. Even in dense reef areas of the GBR (i.e., areas with a large ratio of reef area to the area between the reefs), such as the Swains reefs, an inflow from the adjacent Coral Sea can be traced.…”
Section: Description Of the Drifter Trajectories In The Gbrmentioning
confidence: 99%
“…The formation of a stable cyclonic eddy in the lee of the shelf bathymetry was later postulated as contributing toward north-westward flow in the Capricorn Channel region (Griffin et al 1987). Subsequent oceanographic deployments and satellite sea surface temperature studies have shown these cyclonic features to trigger upwelling along the continental shelf (Kleypas and Burrage 1994;Middleton et al 1994;Burrage et al 1996).…”
Section: The Capricorn Eddymentioning
confidence: 99%