A Field Guide to the Atlantic Seashore: From the Bay of by Kenneth L. Gosner PDF

By Kenneth L. Gosner

ISBN-10: 061800209X

ISBN-13: 9780618002092

Greater than 1,000 illustrations, prepared in response to visible similarities, express plant and animal species of the Atlantic Coast from the Bay of Fundy to Cape Hatteras. This advisor contains details on the right way to find every one species through geographic diversity, tidal variety, tidal point, season, topography, and weather.

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Extra resources for A Field Guide to the Atlantic Seashore: From the Bay of Fundy to Cape Hatteras (Peterson Field Guide)

Sample text

Three of these holes (819, 820 and 821) occur on the upper slope immediately in front of the outer barrier: drilling the slope sequences provided evi­ dence that was compelling, but some found it difficult to believe. , 1989) were likely to be wrong and that the Great Barrier Reef appeared to be much younger. The · 26 P. J. Davies & F. M. Peerdeman conflict focused on just how young, and there were two schools of thought. On the basis of poorly defined seismic mounding, Feary et al. (1993) pro­ posed that reefs were present low in the section and with an age greater than 1 Ma.

Konishi, personal communication), so that from a combined sedi­ mentological and isotopic viewpoint, Site 820 is considered to be by far the most complete section and therefore forms the basis for the analysis defined below. Three sedimentological units are recognized (Fig. 5): Unit A between 0 and 65 m, Unit B between 65 and 145 m, and Unit C between 145 and 220 m. Unit A corresponds to the top 65 m of the section and is composed of wackestones separated by 8 m thick sandy bioclastic packstones composed of planktonic and benthic forams, molluscs, ptero­ pods, minor echinoids, corals, corallines, bryozo­ ans, rhodoliths (at 7 and 32 m) and Halimeda.

Ass. Sediment. No. 3. Blackwell Scientific Publications, Oxford. , KUYPERS, A. R. (1986) A mid Brunhes climatic event: long term climatic changes in global atmosphere and oceanic circulation. Science, 232, 619-622. KEANY, J. P. (1972) Pliocene-early Pleis­ tocene palaeoclimatic history recorded in Antarctic­ Sub Antarctic deep-sea cores. , Part A, 19, 529-548. KINSEY, D. & HOPLEY, D. (1991) The significance of coral reefs as global carbon sinks-response to Greenhouse. Palaeogeogr. Palaeoclimatol.

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A Field Guide to the Atlantic Seashore: From the Bay of Fundy to Cape Hatteras (Peterson Field Guide) by Kenneth L. Gosner


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