Last interglacial reef growth beneath modern reefs in the southern Great Barrier Reef
Studies of modem coral reefs have shown that Holocene reef growth is relatively thin, and that in many instances it has developed on an older limestone surface 1–4 . This surface is commonly associated with leaching and pedogenic processes, indicative of subaerial exposure, and has been termed the s...
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Veröffentlicht in: | Nature (London) 1984-01, Vol.307 (5946), p.44-46 |
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Format: | Artikel |
Sprache: | eng |
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