Trace Fossils 2007
DOI: 10.1016/b978-044452949-7/50138-8
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The Trace-Fossil Record of Vertebrates

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Cited by 74 publications
(43 citation statements)
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“…Aestivation is a state of torpor often associated with arid conditions at high environmental temperature and without food or water intake for an extended period. It is characterized mainly by physical inactivity and low metabolic rate (Pinder et al, 1992;Hasiotis et al, 2007;Withers and Cooper, 2010). In nature, aestivation can occur inside a subterranean mud cocoon.…”
Section: Introductionmentioning
confidence: 99%
“…Aestivation is a state of torpor often associated with arid conditions at high environmental temperature and without food or water intake for an extended period. It is characterized mainly by physical inactivity and low metabolic rate (Pinder et al, 1992;Hasiotis et al, 2007;Withers and Cooper, 2010). In nature, aestivation can occur inside a subterranean mud cocoon.…”
Section: Introductionmentioning
confidence: 99%
“…Terrestrial environments and ecosystems of the past can be better understood with the use of neoichological studies, which allow the connection of burrow morphologies to tracemakers (Hasiotis, 2007;Hasiotis et al, 2007). Documenting the burrow morphologies, burrowing techniques, and behaviors of extant species enables an accurate assessment of possible tracemakers and thus the presence of an organism without requiring body fossils.…”
Section: Discussionmentioning
confidence: 99%
“…Interpretations of the identity and behavior of the trace-making organism can be made aided by the analysis of trace fossil morphology (Bromley, 1996). In doing so, biodiversity can be estimated from trace fossil assemblages, improving interpretations made from body fossils alone since trace fossils record the presence of organisms inhabiting environments with low preservation potential such as soils (Bromley, 1996;Hasiotis, 2007;Hasiotis et al, 2007). Trace fossil morphology is also controlled by the environmental conditions under which the trace was produced allowing for the interpretation of conditions that cannot be determined from the physical sedimentary record (Bromley, 1996;Hasiotis, 2007;MacEachern et al, 2007b).…”
Section: Introductionmentioning
confidence: 99%
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“…In Cenozoic sand-dominated sequences, the tracks of ungulates and proboscideans have been largely studied in cross-section, though bedding-plane expressions (impressions or casts) also exist (Loope 1986;Lea 1996;Milàn et al 2007b). Whereas laboratory experiments on track morphology and preservations are being increasingly undertaken, there is a need for neoichnological studies of modern vertebrate tracks in their natural environmental context (Laporte, Behrensmeyer 1980;Martin 2003;Milàn, Bromley 2006;Hasiotis et al 2007;Genise et al 2009;Platt et al 2012;Platt, Hasiotis 2014). Holocene coastal environments (beaches, dunes, inlet channel margins) and their sedimentary sequences provide ready access to a variety of mammalian and avian traces and serve as modern analogues of numerous coastal formations in the rock record.…”
Section: Introductionmentioning
confidence: 99%