The insects of the Winterswijk Muschelkalk

This article describes the insect fossils found in the Muschelkalk of Winterswijk. Amongst these finds is a beetle elytron, which constitutes the oldest known beetle fossil from the Netherlands. The other insect fossils from the Muschelkalk of Winterswijk that are also briefly discussed, include a dragonfly wing fragment and a complete cockroach wing. These finds make Winterswijk unique amongst Muschelkalk outcrops, no other Muschelkalk site has yielded so many insect fossils. These insect fossils also help us to better reconstruct the depositional environment at Winterswijk: these fi nds indicate more terrestrial influx in the top section of the Winterswijk quarry

Plant-insect interactions in deep time

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Plant-insect interactions from Middle Triassic (late Ladinian) of Monte Agnello (Dolomites, N-Italy)-initial pattern and response to abiotic environmental pertubations

The Paleozoic-Mesozoic transition is characterized by the most massive extinction of the Phanerozoic. Nevertheless, an impressive adaptive radiation of herbivorous insects occurred on gymnosperm-dominated floras not earlier than during the Middle to Late Triassic, penecontemporaneous with similar events worldwide, all which exhibit parallel expansions of generalized and mostly specialized insect herbivory on plants, expressed as insect damage on a various plant organs and tissues. The flora from Monte Agnello is distinctive, due to its preservation in subaerially deposited pyroclastic layers with exceptionally preserved details. Thus, the para-autochthonous assemblage provides insights into environmental disturbances, caused by volcanic activity, and how they profoundly affected the structure and composition of herbivory patterns. These diverse Middle Triassic biota supply extensive evidence for insect herbivore colonization, resulting in specific and complex herbivory patterns involving the frequency and diversity of 20 distinctive damage types (DTs). These DT patterns show that external foliage feeders, piercer-and-suckers, leaf miners, gallers, and oviposition culprits were intricately using almost all tissue types from the dominant host plants of voltzialean conifers (e.g., Voltzia),horsetails, ferns (e.g., Neuropteridium, Phlebopteris, Cladophlebis and Thaumatopteris), seed ferns (e.g., Scytophyllum), and cycadophytes (e.g., Bjuvia and Nilssonia)

Miocene honey bees from the Randeck Maar of southwestern Germany (Hymenoptera, Apidae)

This is the publisher's version, also available electronically from http://www.pensoft.net.The Miocene Randeck Maar (southwestern Germany) is one of the only sites with abundant material of fossil honey bees. The fauna has been the focus of much scrutiny by early authors who recognized multiple species or subspecies within the fauna. The history of work on the Randeck Maar is briefly reviewed and these fossils placed into context with other Tertiary and living species of the genus Apis Linnaeus (Apinae: Apini). Previously unrecorded specimens from Randeck Maar were compared with earlier series in an attempt to evaluate the observed variation. A morphometric analysis of forewing venation angles across representative Recent and Tertiary species of Apis as well as various non-Apini controls was undertaken to evaluate the distribution of variation in fossil honey bees. The resulting dendrogram shows considerable variation concerning the wing venation of Miocene Apini, but intergradation of other morphological characters reveals no clear pattern of separate species. This suggests that a single, highly variable species was present in Europe during the Miocene. The pattern also supports the notion that the multiple species and subspecies proposed by earlier authors for the Randeck Maar honey bee fauna are not valid, and all are accordingly recognized as Apis armbrusteri Zeuner

The diversity of Odonata and their endophytic ovipositions from the Upper Oligocene Fossillagerstätte of Rott (Rhineland, Germany

A commented list of fossil Odonata from the Oligocene outcrop of Rott is given, together with descriptions of new traces of oviposition in plant tissues, very similar to ichnotaxa already known from the early Eocene Laguna del Hunco floras of Patagonia. The joint presences of odonatan larvae and traces of oviposition demonstrate the autochthony of these insects in the palaeolake of Rott, confirming the existence of a diverse and abundant aquatic entomofauna, a situation strikingly different to that in the contemporaneous Oligocene palaeolake of Céreste (France).Museo de La Plat

Wasp mimicry among Palaeocene reduviid bug from Svalbard

This is the publisher's version, also available electronically from http://www.app.pan.pl/article/item/app20110202.htmlThe enigmatic Svalbard Palaeocene fossil taxon Hymenopterites deperditus is revised, and is neither a wasp nor a plant seed, but turns out to be a bug hemelytra corresponding to the oldest described reduviid bug. It can be attributable to the “emesine−saicine clade”. The presence in the Svalbard Palaeocene of this insectivorous bug, showing possible mimicry of a wasp model, confirms the presence of diverse entomofauna and of rather warm palaeoclimatic conditions

Plant–insect interactions from the Late Pennsylvanian of the Iberian Peninsula (León, northern Spain)

We describe new evidences of plant-insect interactions from the Late Pennsylvanian of northern Iberian Peninsula (Leon, Spain). We document nine different Damage Types (DTs) among 216 fossil plant specimens. The interactions include four different Functional Feeding Groups (FFGs), including margin feeding (DT12 and DT13), hole feeding (DT09), galling (DT33, DT80, and DT116), and oviposition (DT67, DT100, and DT102) on Pteridophytes, Pteridospermatophytes, and Coniferophytes. Margin feeding and hole feeding were identified on different species of Polymorphopteris (P. polymorpha, P. cf. pseudobucklandii, and P. integra); galling on Mixoneura wagneri, Pecopteris apicalis, and Oligocarpia gutbieri; and oviposition on Polymorphopteris integra, Cordaites cf. angulostriatus and Polymorphopteris cf. integra. The oviposition scars represent the oldest record of oviposition from the Iberian Peninsula so far. In addition, it is the first evidence of plant-insect interactions on Oligocarpia and Polymorphopteris leaves in the area. These evidences reveal various ecological interactions between different groups of plants and insects in the Late Pennsylvanian forests of Spain, suggesting that these plants were a relevant source of food and lodge for a variety of arthropods (mainly insects). We also explore the possible culprits of these damages and the climatic implications.We appreciate the "Asociacion Paleontologica Alcarrena Nautilus" for the support received during the sampling works in open-cast mines in Leon. This work was supported by the project GRC2019/028 (ED431C-2019/28) of the Galician Government. Artai Santos is supported by a predoctoral fellowship from the Galician Government (Department of Culture, Education and University Planning) co-financed by the European Social Fund (Ref: ED481A-2019/243). Funding for open access charge: Universidade de Vigo/CISUG. We also thank the editors, Dr. Esther Pinheiro, and one anonymous reviewer for the constructive suggestions that have helped to improve the manuscript. All the samples are in the Museo de Ciencias Naturales de Alava (MCNA)

The diversity of Odonata and their endophytic ovipositions from the Upper Oligocene Fossillagerstätte of Rott (Rhineland, Germany

A commented list of fossil Odonata from the Oligocene outcrop of Rott is given, together with descriptions of new traces of oviposition in plant tissues, very similar to ichnotaxa already known from the early Eocene Laguna del Hunco floras of Patagonia. The joint presences of odonatan larvae and traces of oviposition demonstrate the autochthony of these insects in the palaeolake of Rott, confirming the existence of a diverse and abundant aquatic entomofauna, a situation strikingly different to that in the contemporaneous Oligocene palaeolake of Céreste (France).Museo de La Plat

Brood care in a 100-million-year-old scale insect

Behavior of extinct organisms can be inferred only indirectly, but occasionally rare fossils document particular behaviors directly. Brood care, a remarkable behavior promoting the survival of the next generation, has evolved independently numerous times among animals including insects. However, fossil evidence of such a complex behavior is exceptionally scarce. Here, we report an ensign scale insect (Hemiptera: Ortheziidae), Wathondara kotejai gen. et sp. nov., from mid-Cretaceous Burmese amber, which preserves eggs within a wax ovisac, and several freshly hatched nymphs. The new fossil is the only Mesozoic record of an adult female scale insect. More importantly, our finding represents the earliest unequivocal direct evidence of brood care in the insect fossil record and demonstrates a remarkably conserved egg-brooding reproductive strategy within scale insects in stasis for nearly 100 million years