Bottjer, David J.
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David J. Bottjer
VIAF ID: 29716068 (Personal)
Permalink: http://viaf.org/viaf/29716068
Preferred Forms
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200 _ | ‡a Bottjer ‡b David J.
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100 1 _ ‡a Bottjer, David J
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Bottjer, David J
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Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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Bottjer, David J.
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100 1 _ ‡a Bottjer, David J.
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David J. Bottjer
4xx's: Alternate Name Forms (8)
5xx's: Related Names (1)
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University of Southern California
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https://d-nb.info/standards/elementset/gnd#relatedPlaceOrGeographicName
Works
| Title | Sources |
|---|---|
| Brachiopods and chemosymbiotic bivalves in Phanerozoic hydrothermal vent and cold seep environments |
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| Bryozoan paleoecology indicates mid-Phanerozoic extinctions were the product of long-term environmental stress |
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| Campanian/Maastrichtian stage boundary in southern California: Resolution and implications for large-scale depositional patterns |
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| Comment and Reply on “Abundant and diverse early Paleozoic infauna indicated by the stratigraphic record”: COMMENT |
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| Complex embryos displaying bilaterian characters from Precambrian Doushantuo phosphate deposits, Weng'an, Guizhou, China |
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| Complex marine bioturbation ecosystem engineering behaviors persisted in the wake of the end-Permian mass extinction |
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| Complexity and diversity of eyes in early Cambrian ecosystems |
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| Constraining carbonate chemistry at a potential ocean acidification event |
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| Depth transect of an Upper Triassic (Rhaetian) reef from Gosau, Austria: Microfacies and community ecology |
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| Dinosaur eggs and nesting behaviors: A paleobiological investigation |
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| Diversity and species abundance patterns of the Early Cambrian (Series 2, Stage 3) Chengjiang Biota from China |
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| The double mass extinction revisited: reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis (Late Permian) |
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| Early Cambrian animal diapause embryos revealed by X-ray tomography |
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| An Early Cambrian problematic fossil: Vetustovermis and its possible affinities |
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| The early evolution of animals. |
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| Early Triassic stromatolites as post-mass extinction disaster forms |
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| Echinoid concentration beds : two examples from the stratigraphic spectrum |
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| Echinoids from the Tesero Member (Werfen Formation) of the Dolomites (Italy): implications for extinction and survival of echinoids in the aftermath of the end-Permian mass extinction |
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| Ecological ranking of Phanerozoic biodiversity crises: The Serpukhovian (early Carboniferous) crisis had a greater ecological impact than the end-Ordovician |
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| Ecological signature of Lower Triassic shell beds of the western United States |
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| Eric Davidson's career as a paleontologist |
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| Evidence for seafloor microbial mats and associated metazoan lifestyles in Lower Cambrian phosphorites of Southwest China |
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| Evolutionary models in the Early Triassic marine realm |
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| Evolutionary paleoecology, 2000: |
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| The exaerobic zone, a new oxygen-deficient marine biofacies |
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| Exceptional fossil preservation : a unique view on the evolution of marine life |
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| The genome of the sea urchin Strongylocentrotus purpuratus |
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| Geochemistry. Life in the Early Triassic ocean |
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| Homology and Potential Cellular and Molecular Mechanisms for the Development of Unique Feather Morphologies in Early Birds |
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| Ichnofabric and Basin Analysis |
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| Ichnofabric of sandstones deposited in high-energy nearshore environments : measurement and utilization |
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| Juvenile skeletogenesis in anciently diverged sea urchin clades |
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| Late Cretaceous depositional ... 1982, c1981 |
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| Limestone concretion growth documented by trace-fossil relations |
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| Long-term faunal stasis without evolutionary coordination: Jurassic benthic marine paleocommunities, Western Interior, United States |
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| Lower Pennsylvanian (Bashkirian) echinoids from the Marble Falls Formation, San Saba, Texas, USA |
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| Magnetostratigraphy of displaced Upper Cretaceous strata in southern California |
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| Mat growth features |
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| Meroblastic cleavage identifies some Ediacaran Doushantuo (China) embryo-like fossils as metazoans |
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| The Mesozoic return of Paleozoic faunal constituents: A decoupling of taxonomic and ecological dominance during the recovery from the end-Permian mass extinction |
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| A microbial carbonate response in synchrony with the end-Triassic mass extinction across the SW UK |
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| Microbial framework in Upper Triassic (Carnian) patch reefs from Williston Lake, British Columbia, Canada |
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| Mid-Cretaceous amber inclusions reveal morphogenesis of extinct rachis-dominated feathers |
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| Mixed Siliciclastic/Carbonate Systems |
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| Mollusks : notes for a short course |
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| Neogene avian and mammalian tracks from Death Valley National Monument, California : their context, classification and preservation |
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| New concepts in the use of ... 1987 |
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| New probable cnidarian fossils from the lower Cambrian of the Three Gorges area, South China, and their ecological implications |
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| Ordovician increase in extent and depth of bioturbation: Implications for understanding early Paleozoic ecospace utilization |
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| Palaeoecological models, non-uniformitarianism, and tracking the changing ecology of the past |
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| Palaeoenvironmental trends in the history of trace fossils |
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| Paleoecology Past, Present and Future |
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| Paleogenomics of echinoids reveals an ancient origin for the double-negative specification of micromeres in sea urchins |
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| Paleomagnetic evidence that the central block of Salinia (California) is not a far-traveled terrane |
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| Peregrinella: an Early Cretaceous cold-seep-restricted brachiopod |
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| Permian marine paleoecology and its implications for large-scale decoupling of brachiopod and bivalve abundance and diversity during the Lopingian (Late Permian) |
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| Petrographic analysis of new specimens of the putative microfossil Vernanimalcula guizhouena (Doushantuo Formation, South China) |
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| Phanerozoic trends in the global diversity of marine invertebrates |
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| Phosphatized polar lobe-forming embryos from the Precambrian of southwest China |
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| Phylogenetic analysis of the Archaeocidaridae and Palaeozoic Miocidaridae (Echinodermata, Echinoidea) and the origin of crown group echinoids |
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| Platy coral patch reefs from eastern Panthalassa (Nevada, USA): Unique reef construction in the Late Triassic |
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| Precambrian animal life: probable developmental and adult cnidarian forms from Southwest China |
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| The prelude of the end-Permian mass extinction predates a postulated bolide impact |
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| Proliferation of Early Triassic wrinkle structures: Implications for environmental stress following the end-Permian mass extinction |
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| Prolonged Permian Triassic ecological crisis recorded by molluscan dominance in Late Permian offshore assemblages |
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| A Proposed Geobiology-Driven Nomenclature for Astrobiological Observations and Sample Analyses |
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| Quantitative analysis of substrate preference in Carboniferous stem group echinoids |
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| A quantitative study of benthic faunal patterns within the Pennsylvanian and Early Permian |
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| Raman spectra of a Lower Cambrian ctenophore embryo from southwestern Shaanxi, China |
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| Rapid carbonate depositional changes following the Permian-Triassic mass extinction: Sedimentary evidence from South China |
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| Recognising ocean acidification in deep time: An evaluation of the evidence for acidification across the Triassic-Jurassic boundary |
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| Reconstruction of Early Triassic ocean redox conditions based on framboidal pyrite from the Nanpanjiang Basin, South China |
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| Reorganization of sea urchin gene regulatory networks at least 268 million years ago as revealed by oldest fossil cidaroid echinoid |
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| Significance of Silurian stromatolite-sphinctozoan reefs: Comment and Reply |
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| Small bilaterian fossils from 40 to 55 million years before the cambrian |
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| Sponge grade body fossil with cellular resolution dating 60 Myr before the Cambrian |
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| Taphonomy : process and bias through time |
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| Trace-fossil model for reconstruction of paleo-oxygenation in bottom waters |
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| Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States |
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| Understanding mechanisms for the end-Permian mass extinction and the protracted Early Triassic aftermath and recovery |
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| Uppermost Triassic phosphorites from Williston Lake, Canada: link to fluctuating euxinic-anoxic conditions in northeastern Panthalassa before the end-Triassic mass extinction |
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| The use of shell beds as a tool for investigating ecological changes across mass extinction intervals |
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| Wrinkle structures: Microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition |
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