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Hollister et al., 1975

Animal Traces on the Deep-Sea Floor

Hollister, C. D., Heezen, B. C., Nafe, K. E.
DOI
DOI10.1007/978-3-642-65923-2_21
Year1975
BookThe Study of Trace Fossils
Editor(s)Frey, R. W.
PublisherSpringer
Publisher placeBerlin, Heidelberg
Belongs toFrey, 1975 (eds)
Pages493-510
Typechapter in book
LanguageEnglish
Id23725

Abstract

The deep-sea floor is a cold, dark, forbidding place, yet it harbors a significant number of trace-making organisms. These animals include enter opneusts, polychaetes, arthropods, holothurians, echinoids, and stelleroids, especially, and scattered representatives of other groups. Most tracemakers are mobile deposit feeders specifically adapted for gathering food in the abyss, and they leave behind a characteristic array of tracks, trails, shalloio burrows, and fecal castings.

Most deep-sea animal traces are made on the substrate surface or shallowly within it; but because very slow depositional rates generally permit extensive sediment reworking-even by very sparsely populated animals-the entire length of cores may exhibit bioturbate textures. Structures observed in cores and in photographs of the modern abyssal seafloor are valuable in the interpretation of suspected deep-water trace fossils contained in the geologic record.

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