The History of Associations between Plants and Animals

By C. Labandeira. 2002

200 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/60e9ec195066aaf3aa9ef3b6baf56bc31634f427

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1. C. Labandeira
2. E. Currano
3. A. Behrensmeyer
4. Y. Qiu
5. W. DiMichele
6. Libo Li
7. R. Prevec
8. C. Cleal

Citations in the corpus

• The Pollination of Mid Mesozoic Seed Plants and the Early History of Long-proboscid Insects1,2,3 (2010, background): “Fossil evidence indicates that palynophagy occurs significantly earlier than nectarivory (Labandeira, 1998, 2002a).”
• The Fossil Record of Plant-Insect Dynamics (2013, background): “The Parasitoid Revolution represented the emergence of a new feeding guild consisting principally of members of the Hymenoptera (small wasps) but also Diptera (brachyceran flies), which are parasitoids that feed largely on larval herbivorous insects (Labandeira 2002a).”
• Evidence of plant–insect interactions in the Upper Triassic Molteno Formation of South Africa (2004, background): “Although plant–arthropod interactions have been well documented in the Palaeozoic (Scott et al. 1992; Labandeira 1998a, 2002), the feeding of insects on plants is only first documented in the late Carboniferous (Scott & Taylor 1983; Scott 1992; Scott et al. 1992; Labandeira 1998a).”
• Speciation in fig wasps (2010, background): “E-mail: james.cook@reading.ac.uk Conflicts of interest: the authors have not declared any conflicts of interest. interact strongly through both herbivory and pollination and show contemporaneous diversification in the fossil record (Labandeira, 2002).”
• Long-Term Stasis in Ecological Assemblages: Evidence from the Fossil Record* (2004, background): “A broad spectrum of insect damage has been documented on various plant organs, especially leaves, throughout the post-Silurian terrestrial record (Labandeira 2002).”
• VERTEBRATE DISPERSAL OF SEED PLANTS THROUGH TIME (2004, background): “…contemporaneous biotic dispersal has received substantial attention (e.g., van der Pijl 1982, Herrera & Pellmyr 2002, Levey et al. 2002), its historical evolution has been less studied (e.g., Tiffney 1986a,b; Fleming & Lips 1991; Collinson & Hooker 2000; Eriksson et al. 2000a,b; Labandeira 2002).”
• Portrait of a Gondwanan ecosystem: A new late Permian fossil locality from KwaZulu-Natal, South Africa (2009, background): “In contrast to Mesozoic woods, some Palaeozoic woods have a central pith, a feature that is not always preserved.”
• Mouthparts of flower-visiting insects (2005, background): “This was preceded by evolution in the late Jurassic and early Cretaceous of angiosperm pollinating insects with generalized mouthparts (Labandeira, 1997, 2002).”
• The four phases of plant-arthropod associations in deep time (2006, background): “…plant host (paleobotanical), arthropod herbivore (paleoentomological), and associational (paleoecological) fossil records have been considered separate (Labandeira, 2002a), and have had minimal cross links for understanding how plants and arthropods actually have interacted in deep geologic time.”
• Brief history of the gymnosperms: classification, biodiversity, phytogeography and ecology (2007, background): “Thereafter, through some 12 my from the later Eocene to the start of the Miocene, an explosive phase of radiation across the full spectrum of herbivorous insects—Coleoptera, Diptera, Lepidoptera and Hymenoptera—occurs.”
• A Nonflowering Land Plant Phylogeny Inferred from Nucleotide Sequences of Seven Chloroplast, Mitochondrial, and Nuclear Genes (2007, background): “…of the organisms that coevolved with plants to establish the modern terrestrial ecosystems, e.g., animals (Banks and Colthart 1993; Edwards et al. 1995; Labandeira 1998, 2002; Dilcher 2000; Tiffney 2004) and fungi (Remy et al. 1994; Taylor et al. 1995, 2005; Brundrett 2002; Wang and Qiu 2006).”