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  • Behrensmeyer, Anna K.  (8)
  • 1
    Online Resource
    Online Resource
    Elsevier BV ; 1988
    In:  Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 63, No. 1-3 ( 1988-2), p. 1-13
    In: Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier BV, Vol. 63, No. 1-3 ( 1988-2), p. 1-13
    Type of Medium: Online Resource
    ISSN: 0031-0182
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1988
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    detail.hit.zdb_id: 417718-6
    SSG: 12
    SSG: 13
    SSG: 14
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  • 2
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1993
    In:  Short Courses in Paleontology Vol. 6 ( 1993), p. 301-302
    In: Short Courses in Paleontology, Cambridge University Press (CUP), Vol. 6 ( 1993), p. 301-302
    Abstract: Figure 1 summarizes estimates for the time-scales over which fossil assemblages accumulate, based on the findings summarized by the various authors of this volume, and organized according to major taxonomic groups in terrestrial and marine environments. For each group, actualistic estimates are based primarily on field evidence for the durability of organic remains, either from time-lapse tracking of carcasses or from direct-dating of individuals in Recent death assemblages; other methods include extrapolating from known rates of sediment accumulation and rates and depths of mixing. Estimates from the fossil record are based almost exclusively on indirect evidence, such as bracketing of assemblages by biostratigraphic and other chronostratigraphic datums, and actualistic rates of formation for the kinds of beds and facies that contain assemblages. The reader should see individual chapters for details and original sources of data.
    Type of Medium: Online Resource
    ISSN: 2475-2630 , 2475-2673
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1993
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  • 3
    In: Paleobiology, Cambridge University Press (CUP), Vol. 31, No. 4 ( 2005-12), p. 607-623
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2005
    detail.hit.zdb_id: 2052186-8
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  • 4
    In: Paleobiology, Cambridge University Press (CUP), Vol. 37, No. 2 ( 2011), p. 303-331
    Abstract: Phanerozoic trends in shell and life habit traits linked to postmortem durability were evaluated for the most common fossil brachiopod, gastropod, and bivalve genera in order to test for changes in taphonomic bias. Using the Paleobiology Database, we tabulated occurrence frequencies of genera for 48 intervals of ∼11 Myr duration. The most frequently occurring genera, cumulatively representing 40% of occurrences in each time bin, were scored for intrinsic durability on the basis of shell size, reinforcement (ribs, folds, and spines), life habit, and mineralogy. Shell durability is positively correlated with the number of genera in a time bin, but durability traits exhibit different temporal patterns across higher taxa, with notable offsets in the timing of changes in these traits. We find no evidence for temporal decreases in durability that would indicate taphonomic bias at the Phanerozoic scale among commonly occurring genera. Also, all three groups show a remarkable stability in mean shell size through the Phanerozoic, an unlikely pattern if strong size-filtering taphonomic megabiases were affecting the fossil record of shelly faunas. Moreover, small shell sizes are attained in the early Paleozoic in brachiopods and in the latest Paleozoic in gastropods but are steady in bivalves; unreinforced shells are common to all groups across the entire Phanerozoic; organophosphatic and aragonitic shells dominate only the oldest and youngest time bins; and microstructures having high organic content are most common in the oldest time bins. In most cases, the timing of changes in durability-related traits is inconsistent with a late Mesozoic Marine Revolution. The post-Paleozoic increase in mean gastropod reinforcement occurs in the early Triassic, suggesting either an earlier appearance and expansion of durophagous predators or other drivers. Increases in shell durability hypothesized to be the result of increased predation in the late Mesozoic are not evident in the common genera examined here. Infaunal life habit does increase in the late Mesozoic, but it does not become more common than levels already attained during the Paleozoic, and only among bivalves does the elevated late Mesozoic level persist through the Holocene. These temporal patterns suggest control on the occurrence of durability-related traits by individual evolutionary histories rather than taphonomic megabiases. Our findings do not mean taphonomic biases are absent from the fossil record, but rather that their effects apparently have had little net effect on the relative occurrence of shell traits generally thought to confer higher preservation potential over long time scales.
    Type of Medium: Online Resource
    ISSN: 0094-8373 , 1938-5331
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2011
    detail.hit.zdb_id: 2052186-8
    SSG: 12
    SSG: 13
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  • 5
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1993
    In:  Short Courses in Paleontology Vol. 6 ( 1993), p. iii-iii
    In: Short Courses in Paleontology, Cambridge University Press (CUP), Vol. 6 ( 1993), p. iii-iii
    Type of Medium: Online Resource
    ISSN: 2475-2630 , 2475-2673
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1993
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  • 6
    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
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    SSG: 13
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  • 7
    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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  • 8
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1993
    In:  Short Courses in Paleontology Vol. 6 ( 1993), p. 1-8
    In: Short Courses in Paleontology, Cambridge University Press (CUP), Vol. 6 ( 1993), p. 1-8
    Abstract: Since their inception in 1978, the annual short courses sponsored by the Paleontological Society have aimed to broaden and to enhance the professional education of paleontologists, including students new to the field. The 1993 short course continues in that tradition, but differs from many previous courses in focussing not on a taxonomic group but on a broader aspect of the fossil record, namely the time resolution of fossil assemblages. This seemed an especially good topic for a short course because questions of absolute and relative time – how old? how fast? how synchronously? – pervade paleontology and historical geology in general.
    Type of Medium: Online Resource
    ISSN: 2475-2630 , 2475-2673
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1993
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