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GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Karoo Basin (1)
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Primary terms
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Africa
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Southern Africa
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Karoo Basin (1)
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South Africa
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Asia
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Cenozoic
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Tertiary
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middle Eocene (2)
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Paleocene
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Lebo Member (1)
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data processing (1)
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Europe
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Alps
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Limestone Alps
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Northern Limestone Alps (1)
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Central Europe
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Austria
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Lower Austria (1)
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Germany
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Geisel Valley (1)
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Hesse Germany
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Messel Germany (1)
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Saxony-Anhalt Germany
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Halle Germany (1)
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Northern Limestone Alps (1)
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-
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ichnofossils (5)
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Invertebrata
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Arthropoda
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Chelicerata
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Arachnida (1)
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Mandibulata
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Insecta
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Neoptera
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Palaeoptera
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Odonata (1)
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Trilobitomorpha
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Trilobita (2)
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Mesozoic
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Cretaceous
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Upper Cretaceous
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Rock Springs Formation (1)
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Jurassic
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Middle Jurassic
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Callovian (1)
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-
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Triassic
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Lower Triassic
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Permian-Triassic boundary (1)
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Upper Triassic
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Carnian (1)
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paleoclimatology (1)
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Paleozoic
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Permian
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Lower Permian
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Asselian (1)
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Upper Permian
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Permian-Triassic boundary (1)
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Plantae
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Pteridophyta
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Spermatophyta
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Angiospermae
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sedimentary rocks
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soils (1)
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South America
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Patagonia (1)
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sulfur (1)
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United States
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Montana
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Texas
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Baylor County Texas (1)
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Jack County Texas (1)
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King County Texas (1)
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Utah
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Uintah County Utah (1)
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Washington
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Ferry County Washington (2)
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Wisconsin (2)
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rock formations
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sedimentary rocks
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sedimentary rocks
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coal (1)
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sedimentary structures
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soils
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soils (1)
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Response by Conrad C. Labandeira for the presentation of the 2022 Paleontological Society Medal
Understanding the ecology of host plant–insect herbivore interactions in the fossil record through bipartite networks—Corrigendum
Understanding the ecology of host plant–insect herbivore interactions in the fossil record through bipartite networks
FOSSILIZATION OF THE EOCENE “MONKEYHAIR” LATICIFER TREE FROM GEISELTAL, GERMANY: A DEEPER UNDERSTANDING USING MICRO-CT AND PYROLYSIS GC/MS
A new taxon of a primitive moth (Insecta: Lepidoptera: Eolepidopterigidae) from the latest Middle Jurassic of northeastern China
The “Seeds” on Padgettia readi are Insect Galls: Reassignment of the Plant to Odontopteris , the Gall to Ovofoligallites N. Gen., and the Evolutionary Implications Thereof
Distinguishing Agromyzidae (Diptera) Leaf Mines in the Fossil Record: New Taxa from the Paleogene of North America and Germany and their Evolutionary Implications
Odonatan Endophytic Oviposition from the Eocene of Patagonia: The Ichnogenus Paleoovoidus and Implications for Behavioral Stasis
CRITICAL ISSUES OF SCALE IN PALEOECOLOGY
Fossil Insect Eggs and Ovipositional Damage on Bennettitalean Leaf Cuticles from the Carnian (Upper Triassic) of Austria
Fossil leaf economics quantified: calibration, Eocene case study, and implications
Assessing the Fossil Record of Plant-Insect Associations: Ichnodata Versus Body-Fossil Data
Abstract: Two basic approaches are used to assess the paleobiology of continental associations between insect herbivores and their host plants. First is a biological approach that emphasizes phylogeny of extant representatives of lineages with fossil records. Second is a paleobiological approach that provides intrinsic evaluation of fossil associational evidence, of which there are several types of studies. One type of study is intensive examination of single insect-herbivore associations that involve a continuum from generalists to specialists requiring detailed autecological deductions about life habits. Another tack is assessment of herbivore damage patterns from selected plant hosts through slices of time for understanding the ecological evolution of a component community. Alternatively, comprehensive analyses can be made of the feeding patterns within a single or a series of regional floras. The record of plant-insect associations has five advantages. Associational data (1) are typically present in deposits that lack insect body fossils; (2) often surpass in abundance and usefulness insect body fossils in the same deposit; (3) frequently antedate their respective insect body fossils; (4) provide invaluable behavioral data that are unavailable from body fossils; and (5) supply crucial data for testing hypotheses in paleobiology and evolutionary biology that otherwise are unachievable. Disadvantages involve difficulties in circumscribing insect culprits, absence of extant ecological data to which fossil data can be compared, and lack of attention by paleobotanists and botanists in collecting damaged specimens. An associational view of fossil land plants and insects provides a dynamic, process-oriented view of ecosystem evolution that is needed in paleobiology.