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  • 1
    Online Resource
    Online Resource
    Annual Reviews ; 2002
    In:  Annual Review of Ecology and Systematics Vol. 33, No. 1 ( 2002-11), p. 561-588
    In: Annual Review of Ecology and Systematics, Annual Reviews, Vol. 33, No. 1 ( 2002-11), p. 561-588
    Abstract: ▪ Abstract  Advances in taphonomy and stratigraphy over the past two decades have dramatically improved our understanding of the causes, effects, and remedies of incompleteness in the fossil record for the study of evolution. Taphonomic research has focused on quantifying probabilities of preservation across taxonomic groups, the temporal and spatial resolution of fossil deposits, and secular changes in preservation over the course of the Phanerozoic. Stratigraphic research has elucidated systematic trends in the formation of sedimentary gaps and permanent stratigraphic records, the quantitative consequences of environmental change and variable rock accumulation rates over short and long timescales, and has benefited from greatly improved methods of correlation and absolute age determination. We provide examples of how these advances are transforming paleontologic investigations of the tempo and mode of morphologic change, phylogenetic analysis, and the environmental and temporal analysis of macroevolutionary patterns.
    Type of Medium: Online Resource
    ISSN: 0066-4162
    URL: Issue
    RVK:
    Language: English
    Publisher: Annual Reviews
    Publication Date: 2002
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  • 2
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2000
    In:  Paleobiology Vol. 26, No. 1 ( 2000), p. 103-115
    In: Paleobiology, Cambridge University Press (CUP), Vol. 26, No. 1 ( 2000), p. 103-115
    Abstract: Bivalve death assemblages from subtidal environments within the tropical Bocas del Toro embayment of Caribbean Panama permit a test of the extent to which levels of damage are determined by the intrinsic nature of shell supply (proportion of epifaunal species, thick shells, calcitic shells, low-organic microstructures), as opposed to the extrinsic postmortem environment that shells experience. Only damage to interior surfaces of shells was used, to ensure that damage was unambiguously postmortem in origin. We find that facies-level differences in patterns of damage (the rank order importance of postmortem encrustation, boring, edge-rounding, fine-scale surface degradation) are overwhelmingly controlled by environmental conditions: in each environment, all subsets of the death assemblage present the same damage profile. The composition of shell supply affects only the intensity of the taphonomic signature (i.e., percentage of shells affected) only in environments containing hard substrata (patch reefs, Halimeda gravelly sand, mud among patch reefs). In these environments, epifauna, whether aragonitic or calcitic and whether thin or thick, exhibit significantly higher damage than co-occurring infauna, probably due to the initial period of seafloor exposure they typically experience after death. Thick shells ( 〉 0.5 mm), regardless of life habit or mineralogy, are damaged more frequently than thin shells, probably because of selective colonization by fouling organisms. Calcitic shells show no consistently greater frequency of damage than aragonitic shells high-organic microstructures yield mixed patterns. Taphofacies surveys in such depositional systems could thus be confidently based on any subset of the fauna, including diagenetically residual assemblages of calcitic shells and thick-shelled molds. Further tests are needed to determine whether the higher levels of damage observed on some subsets of shells are a consequence of greater time-averaging (thus lower temporal resolution), greater exposure time, preferential attack (potential bias in relative abundance), or some combination of these. Paleobiologically, however, the implication is that ecological subsets of bivalve assemblages are not isotaphonomic, either in tangible damage or in probable bias, within hard-substrate environments, although they may be within soft-sediment environments. In actualistic studies, targeting broad classes of taxa for comparison across environments maximizes our ability to extrapolate taphonomic guidelines into the fossil record, where life habits, skeletal types shallow subtidal habitats have dramatically different patterns of abundance and deployment.
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2000
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  • 3
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2000
    In:  Paleobiology Vol. 26, No. 1 ( 2000), p. 80-102
    In: Paleobiology, Cambridge University Press (CUP), Vol. 26, No. 1 ( 2000), p. 80-102
    Abstract: Contrary to the geological stereotype of pure-carbonate reef platforms, approximately 50% of shallow shelf area in the Tropics is accumulating siliciclastic and mixed siliciclastic-carbonate sediments. Taphonomic characterization of these settings is thus essential for assessing variation among major facies types within the Tropics, as well as for eventual comparison with higher-latitude settings. Our grab samples and dredge samples of bivalve death assemblages from nine stations in five subtidal habitats in a large marine embayment of Caribbean Panama (Bocas del Toro) provide the first actualistic information on the taphonomic condition of shells in Recent tropical siliciclastic sediments. Focusing on unambiguous damage to bivalve shell interiors, we found that the quality of shell preservation in fine-grained siliciclastics is superb: commonly «10% of specimens are affected by encrustation, boring, edge-rounding fine-scale surface alteration via dissolution, microbioerosion maceration. Pure-carbonate and mixed siliciclastic-carbonate environments containing hard substrata (patch reefs, Halimeda gravelly sand, mud among patch reefs) contain higher numbers of more severely damaged shells (generally 〉 25%) and also higher diversities of fossilizable encrusters and borers. Disarticulation and fragmentation are pervasive across all environments and are probably related to predation rather than to postmortem processes. As in other shallow subtidal study areas, the taxonomic compositions of death assemblages have not been homogenized by postmortem transport but show high spatial fidelity to the distribution of living species. Assemblages from the five sedimentary environments have distinct taphonomic signatures, but the strongest differences are between the two fine-grained, exclusively soft-sediment siliciclastic environments on the one hand and the three environments containing hard substrata on the other. Experimental tests for rates and agents of damage, still in progress, indicate that the most critical environmental variables are exhumation cycles and burial rate. Bivalve death assemblages from Bocas del Toro demonstrate that damage levels in tropical fine-grained siliciclastic environments are much lower than in closely associated reefs and algal sands suggest a less filtered record of biological information.
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2000
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 2002
    In:  Geobios Vol. 35 ( 2002-12), p. 107-119
    In: Geobios, Elsevier BV, Vol. 35 ( 2002-12), p. 107-119
    Type of Medium: Online Resource
    ISSN: 0016-6995
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2002
    detail.hit.zdb_id: 2098288-4
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  • 5
    Online Resource
    Online Resource
    Geological Society of America ; 2002
    In:  Geology Vol. 30, No. 9 ( 2002), p. 803-
    In: Geology, Geological Society of America, Vol. 30, No. 9 ( 2002), p. 803-
    Type of Medium: Online Resource
    ISSN: 0091-7613
    Language: English
    Publisher: Geological Society of America
    Publication Date: 2002
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    detail.hit.zdb_id: 2041152-2
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  • 6
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 2001
    In:  Science Vol. 294, No. 5544 ( 2001-11-02), p. 1091-1094
    In: Science, American Association for the Advancement of Science (AAAS), Vol. 294, No. 5544 ( 2001-11-02), p. 1091-1094
    Abstract: Fossil assemblages of skeletal material are thought to differ from their source live communities, particularly in relative abundance of species, owing to potential bias from postmortem transport and time-averaging of multiple generations. However, statistical meta-analysis of 85 marine molluscan data sets indicates that, although sensitive to sieve mesh-size and environment, time-averaged death assemblages retain a strong signal of species' original rank orders. Naturally accumulated death assemblages thus provide a reliable means of acquiring the abundance data that are key to a new generation of paleobiologic and macroecologic questions and to extending ecological time-series via sedimentary cores.
    Type of Medium: Online Resource
    ISSN: 0036-8075 , 1095-9203
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    RVK:
    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2001
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    detail.hit.zdb_id: 2066996-3
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  • 7
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2002
    In:  The Paleontological Society Special Publications Vol. 11 ( 2002), p. 47-62
    In: The Paleontological Society Special Publications, Cambridge University Press (CUP), Vol. 11 ( 2002), p. 47-62
    Abstract: The term “fossil record” is used in two ways: to mean either the totality of fossils preserved in all rocks or the sum of human knowledge of those fossils. In both cases, the term carries the connotation also of the geologic context of the fossils—their distribution in time and space and their relationship to the enclosing rock. One of the primary scientific interests of the fossil record is what it can teach us about the history of life and the processes of large-scale transformation, or evolution, in the forms, diversities, and biological interactions of living things.
    Type of Medium: Online Resource
    ISSN: 2475-2622 , 2475-2681
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2002
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  • 8
    Online Resource
    Online Resource
    University of Chicago Press ; 2000
    In:  The Journal of Geology Vol. 108, No. 2 ( 2000-03), p. 131-154
    In: The Journal of Geology, University of Chicago Press, Vol. 108, No. 2 ( 2000-03), p. 131-154
    Type of Medium: Online Resource
    ISSN: 0022-1376 , 1537-5269
    RVK:
    Language: English
    Publisher: University of Chicago Press
    Publication Date: 2000
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  • 9
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2000
    In:  Paleobiology Vol. 26, No. sp4 ( 2000-12), p. 103-147
    In: Paleobiology, Cambridge University Press (CUP), Vol. 26, No. sp4 ( 2000-12), p. 103-147
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2000
    detail.hit.zdb_id: 2052186-8
    SSG: 12
    SSG: 13
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  • 10
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2000
    In:  Paleobiology Vol. 26, No. S4 ( 2000), p. 103-147
    In: Paleobiology, Cambridge University Press (CUP), Vol. 26, No. S4 ( 2000), p. 103-147
    Abstract: Taphonomy plays diverse roles in paleobiology. These include assessing sample quality relevant to ecologic, biogeographic, and evolutionary questions, diagnosing the roles of various taphonomic agents, processes and circumstances in generating the sedimentary and fossil records, and reconstructing the dynamics of organic recycling over time as a part of Earth history. Major advances over the past 15 years have occurred in understanding (1) the controls on preservation, especially the ecology and biogeochemistry of soft-tissue preservation, and the dominance of biological versus physical agents in the destruction of remains from all major taxonomic groups (plants, invertebrates, vertebrates); (2) scales of spatial and temporal resolution, particularly the relatively minor role of out-of-habitat transport contrasted with the major effects of time-averaging; (3) quantitative compositional fidelity; that is, the degree to which different types of assemblages reflect the species composition and abundance of source faunas and floras; and (4) large-scale variations through time in preservational regimes (megabiases), caused by the evolution of new bodyplans and behavioral capabilities, and by broad-scale changes in climate, tectonics, and geochemistry of Earth surface systems. Paleobiological questions regarding major trends in biodiversity, major extinctions and recoveries, timing of cladogenesis and rates of evolution, and the role of environmental forcing in evolution all entail issues appropriate for taphonomic analysis, and a wide range of strategies are being developed to minimize the impact of sample incompleteness and bias. These include taphonomically robust metrics of paleontologic patterns, gap analysis, equalizing samples via rarefaction, inferences about preservation probability, isotaphonomic comparisons, taphonomic control taxa, and modeling of artificial fossil assemblages based on modern analogues. All of this work is yielding a more quantitative assessment of both the positive and negative aspects of paleobiological samples. Comparisons and syntheses of patterns across major groups and over a wider range of temporal and spatial scales present a challenging and exciting agenda for taphonomy in the coming decades.
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2000
    detail.hit.zdb_id: 2052186-8
    SSG: 12
    SSG: 13
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