1989
DOI: 10.2307/3514586
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Effects of Taphonomy and Habitat on the Record of Benthic Foraminifera in Modern Sediments

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Cited by 60 publications
(18 citation statements)
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“…However, in areas with a reasonable sediment accumulation (> 1-2 mmlyear) even integrated variations over time can be detected if the environmental changes have significantly altered the indigenous assemblage composition. Taphonomic processes are also least active in areas of rapid sedimentation, where the bioturbated zone is thin, and under oxygen-deficient conditions (Denne and Sen Gupta, 1989). When, for instance, pulp fibers are added to a system, the physical characteristics of the sediments are altered and physically smaller and surface dwelling animals start to predominate (Pearson and Rosenberg, 1976).…”
Section: Historical Perspectivesmentioning
confidence: 98%
“…However, in areas with a reasonable sediment accumulation (> 1-2 mmlyear) even integrated variations over time can be detected if the environmental changes have significantly altered the indigenous assemblage composition. Taphonomic processes are also least active in areas of rapid sedimentation, where the bioturbated zone is thin, and under oxygen-deficient conditions (Denne and Sen Gupta, 1989). When, for instance, pulp fibers are added to a system, the physical characteristics of the sediments are altered and physically smaller and surface dwelling animals start to predominate (Pearson and Rosenberg, 1976).…”
Section: Historical Perspectivesmentioning
confidence: 98%
“…However, studies of detailed changes at different depths in a core can be complicated by taphonomic and diagenetic changes (e.g. DENNE & SEN GUPTA 1989;LOUBERE & GARY 1990). Responses to pollution and environmentally related morphological variations observed in benthic Foraminifera (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…The living fauna represents a snapshot in a particular environmental context that may vary considerably over short timescales. Conversely, total assemblages give an averaged picture for a much longer period of time (years to centuries), and their composition has been transformed by taphonomical losses (e.g., Murray and Alve, 1999;Denne and Sen Gupta, 1989;Jorissen and Wittling, 1999). This concerns especially agglutinated taxa, many of which are rapidly decomposed after the death of the organisms (Bizon and Bizon, 1985;Schröder, 1988).…”
Section: Data On Living Faunas Versus Total/dead Faunasmentioning
confidence: 99%