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      Arthropod and Pathogen Damage on Fossil and Modern Plants: Exploring the Origins and Evolution of Herbivory on Land

      1 , 2 , 3 , 4 , 5
      Annual Review of Entomology
      Annual Reviews

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          Abstract

          The use of the functional feeding group–damage type system for analyzing arthropod and pathogen interactions with plants has transformed our understanding of herbivory in fossil plant assemblages by providing data, analyses, and interpretation of the local, regional, and global patterns of a 420-Myr history. The early fossil record can be used to answer major questions about the oldest evidence for herbivory, the early emergence of herbivore associations on land plants, and later expansion on seed plants. The subsequent effects of the Permian–Triassic ecological crisis on herbivore diversity, the resulting formation of biologically diverse herbivore communities on gymnosperms, and major shifts in herbivory ensuing from initial angiosperm diversification are additional issues that need to be addressed. Studies ofherbivory resulting from more recent transient spikes and longer-term climate trends provide important data that are applied to current global change and include herbivore community responses to latitude, altitude, and habitat. Ongoing paleoecological themes remaining to be addressed include the antiquity of modern interactions, differential herbivory between ferns and angiosperms, and origins of modern tropical forests. The expansion of databases that include a multitude of specimens; improvements in sampling strategies; development of new analytical methods; and, importantly, the ability to address conceptually stimulating ecological and evolutionary questions have provided new impetus in this rapidly advancing field.

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          Organization of a Plant-Arthropod Association in Simple and Diverse Habitats: The Fauna of Collards (Brassica Oleracea)

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            betapart: an R package for the study of beta diversity

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              Transient floral change and rapid global warming at the Paleocene-Eocene boundary.

              Rapid global warming of 5 degrees to 10 degrees C during the Paleocene-Eocene Thermal Maximum (PETM) coincided with major turnover in vertebrate faunas, but previous studies have found little floral change. Plant fossils discovered in Wyoming, United States, show that PETM floras were a mixture of native and migrant lineages and that plant range shifts were large and rapid (occurring within 10,000 years). Floral composition and leaf shape and size suggest that climate warmed by approximately 5 degrees C during the PETM and that precipitation was low early in the event and increased later. Floral response to warming and/or increased atmospheric CO2 during the PETM was comparable in rate and magnitude to that seen in postglacial floras and to the predicted effects of anthropogenic carbon release and climate change on future vegetation.
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                Author and article information

                Journal
                Annual Review of Entomology
                Annu. Rev. Entomol.
                Annual Reviews
                0066-4170
                1545-4487
                January 23 2023
                January 23 2023
                : 68
                : 1
                : 341-361
                Affiliations
                [1 ]Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC, USA;
                [2 ]Department of Entomology, University of Maryland, College Park, Maryland, USA
                [3 ]College of Life Sciences and Academy for Multidisciplinary Studies, Capital Normal University, Beijing, China
                [4 ]Natural History Department, Hessisches Landesmuseum, Darmstadt, Germany;
                [5 ]Paleontology Section, Institute of Geosciences, Rheinische Friedrich-Wilhelms Universität Bonn, Bonn, Germany
                Article
                10.1146/annurev-ento-120120-102849
                36689301
                2e785af4-6f46-4709-a58a-11e8f9a647bc
                © 2023

                http://creativecommons.org/licenses/by/4.0/

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