The Geomorphology of the Great Barrier Reef: Development, Diversity and ChangeCambridge University Press, 17. 5. 2007. This 2007 book reviews the history of geomorphological studies of the Great Barrier Reef and assesses the influences of sea-level change and oceanographic processes on the development of reefs over the last 10,000 years. It presents analyses of recently attained data from the Great Barrier Reef and reconstructions of the sequence of events which have led to its more recent geomorphology. The authors emphasise the importance of the geomorphological time span and its applications for present management applications. This is a valuable reference for academic researchers in geomorphology and oceanography, and will also appeal to graduate students in related fields. |
Из књиге
Резултати 1-5 од 76
Страница 6
... depth at which reef- building organisms seemed to flourish (about 100m). He ... sea level change postulated (for discussion see Hopley, 1982; Woodroffe, 2002a). Only ... water reef limestone was recovered, overlying basaltic (volcanic) ...
... depth at which reef- building organisms seemed to flourish (about 100m). He ... sea level change postulated (for discussion see Hopley, 1982; Woodroffe, 2002a). Only ... water reef limestone was recovered, overlying basaltic (volcanic) ...
Страница 27
... depth between these two locations. The overall influence of basement rocks within the continental shelf on the GBR and its evolution can only be surmised but is likely to have been significant. 2.3 Evolution of the Coral Sea The ...
... depth between these two locations. The overall influence of basement rocks within the continental shelf on the GBR and its evolution can only be surmised but is likely to have been significant. 2.3 Evolution of the Coral Sea The ...
Страница 30
... water sediments from short periods of high sea level. Sediment supply ... depth for reef building (McKenzie and Davies, 1993; Watts et al., 1993) ... sea level stand. Symonds et al. (1983) suggest that carbonate sediments from the reefs ...
... water sediments from short periods of high sea level. Sediment supply ... depth for reef building (McKenzie and Davies, 1993; Watts et al., 1993) ... sea level stand. Symonds et al. (1983) suggest that carbonate sediments from the reefs ...
Страница 37
... water temperature dropped below 208C, the result of reorganization of oceanic circulation in the Coral Sea (Isern et ... depth of water (between 30 and 80m) on the outer shelf produced by a specific eustatic sea level high (see Section ...
... water temperature dropped below 208C, the result of reorganization of oceanic circulation in the Coral Sea (Isern et ... depth of water (between 30 and 80m) on the outer shelf produced by a specific eustatic sea level high (see Section ...
Страница 42
... Sea. level: a. primary. control. of. long-term. reef. growth. and. geomorphological ... depths exceeding 100m under exceptional circumstances; for example, corals ... water temperature, salinity, substrate stability, and aragonite saturation ...
... Sea. level: a. primary. control. of. long-term. reef. growth. and. geomorphological ... depths exceeding 100m under exceptional circumstances; for example, corals ... water temperature, salinity, substrate stability, and aragonite saturation ...
Друга издања - Прикажи све
Чести термини и фразе
accretion accumulation appear associated Barrier Reef beach cays central GBR channels Chapter coast complex continental coral coral reefs cores currents cyclone dates Davies deposits depth described detail discussed dominated drilling edge effects energy established evidence example extend Figure Flood foundations fringing reefs front further geomorphological Halimeda higher holes Holocene Hopley identified important increase indicated inner lagoon less limited mainland major mangrove margin maximum morphology northern noted occur outer patches period planar platform Pleistocene possible present processes produced range rates reached recent record reef flat reef growth reef islands region relatively ribbon rise River sand sea level sediment shallow shelf shingle significant similar slope Stoddart structure studies submerged suggested surface Swain Reefs Table tidal tide vegetated wave wide windward zone