By Valentin Krassilov, Alexandr Rasnitsyn

ISBN-10: 9546423157

ISBN-13: 9789546423153

Paleontologists only in the near past opened their eyes at the wealth of fossil records correct to plant - arthropod interplay and are busy now gathering uncooked info within the first position. possibly the richest local choice of interplay lines got here from the mid-Cretaceous deposits of the Negev barren region, Israel, encompassing the time period of the increase and basal radiation of angiosperms - the flowering vegetation. The arthropods (insects and mites) placing their eggs within the leaves and making leaf mines and galls have been studying new percentages for endophytic existence that the flowering vegetation supplied. Their morphological disparity indicates a diversification race, during which the angiosperms did not override their leaf parasites.Only a small fraction of insect variety is represented by way of physique fossils that belong to 1 extinct and 9 extant households of beetles and cockroaches typically. simply because related constructions are produced on leaves by way of parasitic arthropods of other systematic alliances, a simply morphological class is labored out for the hint fossils, with yet tentative assignments to typical taxa, yet touching on distinctive varieties of parasitic habit. it truly is evolution of habit that's documented by means of the hint fossils. The physique fossils and parasitic lines signify the morphologies and behavioral features really complicated for his or her geological age. The expressiveness, abundance, co-occurrence, and host specialization of parasitic constructions, in addition to the marks of predation on mines and galls betray regulatory mechanisms of plant - arthropod interplay, analyzed within the wide context of environment evolution, paleogeography and weather switch.

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Extra info for Plant-Arthropod Interactions in the Early Angiosperm History: Evidence from the Cretaceous of Israel

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This complies with such features as: (1) The whole leaf area – whole depth mines (Holostigmonoma zebrina), some with epidermal windows (Holostigmonoma fenestrata). (2) The incidents of petiole to midrib (primary vein) mining causing leaf stunting and deformity (Ophionoma digitata on Eocercidiphyllites glandulosus). (3) The rarity of frass-less mines representative of epidermal sap feeders, in conjunction with (4) The absence of typical serpentine tracks, the most parsimonious mine construction in terms of the track length/area ratio (approached, but not typically represented by Ophiheliconoma resupinata and Troponoma curvitracta).

Yet for the leaf parasites, ecological relatedness of their host plants might have been as mandatory as the phylogeny. Ecologically, Nelumbites and Typhacites definitely came from aquatic/wetland communities of quite modern aspect (Chapter 5). N. aravensis had two types of leaves, floating and emergent, on rhizomes with ochreic prophylls, as in extant Nelumbo nucifera. Eocercidiphyllites glandulosus represents typical long-petiolate aspen-like leaf morphology typical of temperate deciduous trees and similar to those of extant Cercidiphyllum japonicum, a canopy tree in the mountain forests of eastern China and Japan.

10, c). This form of phyllostigmas declined in the Turonian, perhaps with the mainly tropical buprestids or their extinct ecological equivalents. ) of phyllostigmas are recognized in the trace assemblage of Gerofit. Their tentative taxonomic assignments suggest domination of cecidomyiids among the gall-makers, with aphids second in abundance, sawflies the third and the rest far less prominent (Fig. 11). Lepidoptera prevail in the mining community comprising more than half of all morphotypes, followed by Diptera and Hymenoptera, with Coleoptera as minor contributors (Fig.

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Plant-Arthropod Interactions in the Early Angiosperm History: Evidence from the Cretaceous of Israel by Valentin Krassilov, Alexandr Rasnitsyn


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