THE FOUR PHASES OF PLANT-ARTHROPOD ASSOCIATIONS IN DEEP TIME
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dc.contributor.author | Labandeira C.C. | |
dc.date.accessioned | 2024-12-02T06:55:51Z | |
dc.date.available | 2024-12-02T06:55:51Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=14608974 | |
dc.identifier.citation | Geologica Acta, 2006, 4, 4, 409-438 | |
dc.identifier.issn | 1695-6133 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46756 | |
dc.description.abstract | Vascular-plant hosts, their arthropod herbivores, and associated functional feeding groups are distributed spatiotemporally into four major herbivore expansions during the past 420 m.y. They are: (1) a Late Silurian to Late Devonian (60 m.y.) phase of myriapod and apterygote, hexapod (perhaps pterygote) herbivores on several clades of primitive vascular-plant hosts and a prototaxalean fungus; (2) a Late Mississippian to end-Permian (85 m.y.) phase of mites and apterygote and basal pterygote herbivores on pteridophyte and basal gymnospermous plant hosts; (3) a Middle Triassic to Recent (245 m.y.) phase of mites, orthopteroids (in the broadest sense) and hemipteroid and basal holometabolan herbivores on pteridophyte and gymnospermous plant hosts; and (4) a mid Early Cretaceous to Recent (115 m.y.) phase of modern-aspect orthopteroids and derived hemipteroid and holometabolous herbivores on angiospermous plant hosts. These host-plant and herbivore associations are mediated by seven functional feeding groups: a) external foliage feeding, b) piercing-and-sucking, c) boring (Phase 1 origins); d) galling, e) seed predation, f) nonfeeding oviposition (Phase 2 origins); and leaf mining (early Phase 3 origin). Within about 20 m.y. of each herbivore expansion, there is a biota that expresses the nearly full spectrum of later plant-arthropod associations. These four associational phases may be linked to the paleoclimatologic variables of greenhouse/icehouse cycles and atmospheric O2 and CO2 levels by uncertain causes, although some relationship probably is present. The 7 functional feeding groups persist through most of the sampled interval but harbor host-plants and arthropod herbivores that are spatiotemporally ephemeral. Poor understanding of associations in Phases 1 to 3 is attributed to disproportionate focus on the angiosperm and holometabolan insect associations of Phase 4. © UB-ICTJA. | |
dc.subject | HERBIVORY FOSSIL-RECORD | |
dc.subject | INSECTS | |
dc.subject | LAND PLANTS | |
dc.subject | PALEOCLIMATE | |
dc.subject | PLANT-INSECT-ASSOCIATIONS | |
dc.subject | Cretaceous | |
dc.subject | Triassic | |
dc.subject | Permian | |
dc.subject | Devonian | |
dc.subject | Silurian | |
dc.subject | Mississippian | |
dc.title | THE FOUR PHASES OF PLANT-ARTHROPOD ASSOCIATIONS IN DEEP TIME | |
dc.type | Статья | |
dc.subject.age | Mesozoic::Cretaceous | |
dc.subject.age | Мезозой::Меловая | |
dc.subject.age | Mesozoic::Triassic | |
dc.subject.age | Мезозой::Триасовая | |
dc.subject.age | Paleozoic::Permian | |
dc.subject.age | Палеозой::Пермская | |
dc.subject.age | Paleozoic::Devonian | |
dc.subject.age | Палеозой::Девонская | |
dc.subject.age | Paleozoic::Silurian | |
dc.subject.age | Палеозой::Силурийская | |
dc.subject.age | Paleozoic::Carboniferous::Mississippian | |
dc.subject.age | Палеозой::Каменноугольная |
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