By E. Alison Kay
Книга является первым детальным справочником по морским и пресноводным раковинам Гавайских островов.
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Extra resources for Shells of Hawai'i
Sample text
J. ), pp. 36 5-378. Ocean Drilling Program, College Station, TX. H. C. (1988) Qua ternary isotope stratigraphy of hole 59 3, Challenger Plateau, South Tasman Sea: preliminary observations 38 P. J. Davies & F. M. Peerdeman based on foraminifers and calcareous nannofossils . P. ), pp. 1413-1424. US Government Printing Office, Washington, D C. PALMIERI, v. (1971) Tertiary subsurf ace biostra tigraphy of the Capricorn Basin. Report No. 52, Geological Survey of Queensland. PALMIERI, V. (1974) Correlationand environmental trends of the subsurf ace Tertiary Capricorn Basin.
R. (1993) Isotopic and trace-element indicators of palaeoclimate and sea-level, Site 820. J. ) , pp. 163173. Ocean Drilling Program, College Station, TX. PRELL, WL. (1982) Oxygen and carbon isotope stratigra phy of the Quaternary of Hole 502B: evidence for two modes of isotope variability. L. ), pp. 4 5 5-464. US Government Printing Of fice, Washington, DC. C. & HILL, D . (1942) Great Barrier Reef Cores, 1 926and 1 937-Descriptions, Analysesand Inter pretations. Report No. 25, Great Barrier Reef Commit tee.
Central part of the guyot. Grey, skeletal packstones, grainstones and wackestones contain fragments of bivalves (including rudists, which may represent up to 77% of the skeletal components), echinoderms, sparse corallinacean algae and ostracods (Fig. 6A). The larger benthic foraminifers, Sulcoperculina and Asterorbis, are rare, whereas Dicyclina, miliolids, textulariids and rotaliids are common. , 1 995). An abundance of pyrite results from sulphate reduction soon after deposition. At the top of DS-2, subaerial exposure is indicated both by sedimentological criteria such as rhizoliths and alveolar texture (Fig.