The Khasurty locality (Lower Cretaceous of Transbaikalia, Russia) is one of the largest fossil insect sites in the region. Over the entire period of study, more than 6000 insect imprints have been collected here, representing 16 orders and 130 families. Dipterans, aphids and hymenopterans are the most common forms here, the most diverse taxa are Diptera, Hymenoptera, Coleoptera and Trichoptera. In addition to insects, remains of crustaceans, mosses, liverworts and vascular plants were found in Khasurty, as well as occasional finds of arachnids, bird feathers and fish scales. Two new families, 17 new genera and 21 new species of Trichoptera, two new species of Orthoptera, one new genus and species of Phasmatoptera, one new species of Reculida, three new genera and species of Hemiptera, a new genus and species of Thysanoptera, a new genus and species of Hymenoptera, a new subfamily, two new genera and six new species of Lepidoptera, three new genera and four new species of Neuroptera, as well as a new genus and species of liverworts are described. In terms of the composition of the fauna and flora, the Khasurty locality is very peculiar, it includes both Jurassic and Cretaceous taxa, but in general it can be attributed to the Jehol biota.

A new subfamily of ichneumonids, Palaeoichneumoninae, is described from the Lower Cretaceous of Transbaikalia (Baisa locality) and Mongolia (Bon Tsagan and Kholbotu Gol localities). The new subfamily is intermediate between the archaic subfamily Tanychorinae and the Recent Ichneumonidae. It includes 12 new species, described in three new genera: Palaeoichneumon freja gen. et sp. nov., P. ornatus sp. nov., P. danu sp. nov., P. micron sp. nov., P. mirabilis sp. nov., P. tenebrosus sp. nov., P. townesi sp. nov., Rudimentifera mora gen. et sp. nov., R. suspecta sp. nov., Dischysma maculata gen. et sp. nov., D. similis sp. nov., and D. ramulata sp. nov.

Two new species of Labenopimplinae, Labenopimpla orapa sp. n. and Rugopimpla botswana sp. n., are described from the Upper Cretaceous (Turanian) deposits of Orapa in Botswana. These are the first and only known Cretaceous Ichneumonidae from the southern hemisphere. The new species seem to be very similar to their relatives from the Cenomanian of the Russian Far East. This indicates a wide distribution of Ichneumonidae by the early Late Cretaceous at least.

Two new genera and seven new species of Madygellinae (Xyelidae) from the Middle-Upper Triassic of Kyrgyzstan (Madygen Formation, Dzhailoucho locality): Madygella levivenosa sp. nov., M. kurochkini sp. nov., M. aristovi sp. nov., M. bashkuevi sp. nov., S. ryzhkovae gen. et sp. nov., S. shmakovi sp. nov., Chubakka madygensis gen. et sp. nov. Improved diagnoses of the subfamily Madygellinae and genus Madygella and improved redescription of the species Madygella analoga Rasnitsyn, 1969 are given. The taxonomic position of madygellines within Hymenoptera and their relationships with Sepulcidae (Cephoidea) are discussed.

Ichneumonidae constitute one of the largest families of organisms, but their fossil record is severely understudied, which precludes inferences about their early evolutionary history. We here describe a new genus and two new species of ichneumonids from the Early Eocene Tadushi Formation (Russian Far East). The new taxa are Crusopimpla tadushensis gen. et sp. nov. and Dolichomitus? saxeus sp. nov. Pimpla rediviva (Brues) is redescribed and placed in the genus Crusopimpla. This new genus is unique within Pimplinae in having a completely developed propodeal carination and probably represents one of its most basal lineages. Using a phylogenetic hypothesis of the subfamily, we discuss potential pathways of morphological evolution in the group, which will provide a basis for future placement of pimpline fossil taxa.