Titlebook: Cold-Water Corals and Ecosystems; André Freiwald,J. Murray Roberts Book 2005 Springer-Verlag Berlin Heidelberg 2005 Cold-water coral reef.

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書目名稱Cold-Water Corals and Ecosystems被引頻次學(xué)科排名




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書目名稱Cold-Water Corals and Ecosystems讀者反饋學(xué)科排名

olfction

adumbrate

Corals from deep-water methane-seep deposits in Paleogene strata of Western Oregon and Washington, Une and Oligocene rocks of the Lincoln Creek Formation include the corals . Durham, and an undescribed . (.) species. A new species of . appears to be restricted to a single methane-seep site. The corals . Durham, and . Durham have been reported from what may be methane-seeps sites in the Lincoln Cre

Orthodontics

Growth, deposition, and facies of Pleistocene bathyal coral communities from Rhodes, Greecers from the mound-forming . occurrences as known, e.g., from the NE-Atlantic or the Florida Strait. Instead, it appears similar to the modern ‘white coral community’ of the western Mediterranean Sea that is usually associated with submarine cliffs. Much like the latter, the St. Paul’s Bay Limestone

正式演說(shuō)

BOLT

Sedimentary patterns in the vicinity of a carbonate mound in the Hovland Mound Province, northern Polightly older than 31 kyr BP, coherent with Heinrich event 3 deposition. During Late Marine Isotope Stage 3 (MIS 3) and MIS 2 shelf erosion prevailed with abundant gravity flows and turbidity currents. A change from glaciomarine to hemipelagic contourite sedimentation during the onset of the Holocen

BOLT

Deep-water corals of the northeastern Atlantic margin: carbonate mound evolution and upper intermedion on the summit of carbonate mounds, with sediment accumulation rates in the order of ～0.3 mm yr.. However, coral growth is discontinuous and irregular, and complete coral sequences are frequently altered (dissolved) likely due to organic matter consumption by oxidizing pore fluids. Mound top sedim

Keratin

引起

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