


编号 1 (2025)
New radiolarian species Nordvikella plana sp. nov. from the Kimmeridgian deposits of Dyakovo Section (Kolomenskoye, Moscow)
摘要
New radiolarian species Nordvikella plana sp. nov. (Family Echinocampidae) is described from reworked Kimmeridgian phosphatic concretions from the basal horizon of Volgian Stage in Dyakovo Section (Kolomenskoye, Moscow). The presence of Echinocampidae is traced in the Upper Jurassic and Lower Cretaceous (from Oxfordian to Ryazanian) in Pan-Boreal paleobiogeographic realm.



New radiolarian species Pseudodictyomitra coronata sp. nov. from the coniacian–santonian deposits of Perapedhi formation, Cyprus
摘要
Numerous representatives of the Pseudodictyomitra Pessagno, 1977 were studied from the Upper Cretaceous deposits of Cyprus. Description of P. pseudomacrocephala (Squinabol, 1903), emend. nov. is emended. New species P. coronata sp. nov. is described. Stratigraphic ranges and phylogenetic relationships in the family Pseudodictyomitridae are detalized.



Howellella gonensis – a new species of Spiriferids (Brachiopoda) from the lower devonian beds of North-East Asia
摘要
A new species, Howellella gonensis sp. nov. (order Spiriferida) has been described from the Lower Prague beds of the Selennyakh Ridge (North-East Asia), and its ontogeny is considered.



New species of ostracods of the genus Aparchitellina from the yba formation (givetian?–frasnian) of Southern Timan (Djejimparma)
摘要
Two new species of ostracods of the genus Aparchitellina – A. lenis sp. nov. and A. reticulata sp. nov. from the carbonate shallow-shelf deposits of the Yba Formation (Givetian?–Frasnian) of the Southern Timan are described. The species A. lenis sp. nov. is restricted to its lower part of the section, while A. reticulata sp. nov. appears stratigraphically higher and is distributed almost throughout the section. The described species complete the biostratigraphic characterisation of the Givetian-Frasnian boundary interval in carbonate facies.



New data about evolution of the middle Jurassic ostracod genus Lophocythere Silvester-Bradley of the Russian Plate
摘要
Important for stratigraphy ostracods of the genus Lophocythere (family Progonocytheridae) from the Middle Jurassic strata of the Central European Russia (sections Mikhailovsky rudnik, boreholes № 4, № 7, Kursk region and Mikhailovcement, Ryazan region) were studied. This article provides an updated review of the evolution of this taxa, three evolutionary lineages reconstructed: L. batei Malz, 1975 → L. mosaica sp. nov., L. tuberculata sp. nov., L. karpinskyi (Mandelstam in Lyubimova, 1955); L. propinqua Malz, 1975 → L. scabra Triebel, 1951 → L. bucki Lutze, 1960; L. carinata Blaszyk, 1967 → L. interrupta Triebel, 1955 → ? → L. acrolophos Whatley, Ballent et Armitage, 2001. The evolution of the first lineage can be characterized as cladogenesis (the origin of three species from the common ancestor). The evolution of the other two lineage can be described as anagenesis (or phyletic evolution) (species successively replace each other over time). A new species Lophocythere tuberculata sp. nov. is described from the lower Callovian (Subpatruus and Koenigi ammonite zones) and upper Callovian (Athleta ammonite zone, Spinosum subzone) of the Kursk and Ryazan regions and L. mosaica sp. nov. is described from the lower Callovian (Gowerianus and Calloviense ammonite zones) of the Kursk region.



New Neurocythere and Terquemula (Ostracoda, Crustacea) from the Callovian of the Russian Plate
摘要
The new species Neurocythere margaritae, N. parva, and Terquemula pseudoflexicosta from Callovian of the Russian Plate are described. The first two form a stratigraphic sequence with N. margaritae occurring in the lower and middle Callovian in the Subpatruus – Jason zones and N. parva in the middle and upper Callovian, Coronatum – Lamberti zones. The morphology of both species is identical, but their sizes are different, which allows us to distinguish these taxa and prove their genetic relationship. The daughter N. parva originated from N. margaritae by gerontomorphosis with minification. The fact that the new species belong to a single lineage allows to establish new homonymous lineage zones for the lower-middle and middle-upper Callovian of the Russian Plate. The species T. pseudoflexicosta is known from the lower Callovian, Koenigi Zone.



A new caddisfly species Cladochorista uralica sp. nov. (Insecta, Trichoptera: Cladochoristidae) from the Upper Permian of Vyazovka, Orenburg Region, Russia
摘要
A new species of caddisfly, Cladochorista uralica sp. nov. (Cladochoristidae), is described based on the forewing from the Upper Permian locality Vyazovka-3 (Orenburg region, Russia). The stratigraphic and geographical distribution of the family Cladochoristidae is updated, and a brief overview of the insect composition at fossil localities 3 and 25 of the Vyazovka Ravine section is provided.



New late devonian species of conodonts from south of West Siberia
摘要
A new species of conodonts Polygnathus ovaliformis sp. nov. from the Upper Devonian deposits of the northeastern margins of the Kuznetsk Basin is described. This species is most closely related to the Late Frasnian species Po. brevis Miller et Youngquist and Po. costulatus Aristov.



To the revision of the middle Permian bolosaurids (Tetrapoda, Bolosaurida) of Eastern Europe
摘要
A re-examination of the holotype of Permotriturus herrei Tatarinov, 1968 (Tetrapoda, Bolosaurida) supplemented by a new specimen from the type locality Isheevo, Republic of Tatarstan, European Russia, supports the validity of the genus Belebey Ivakhnenko, 1973. The differences between the genera Belebey and Permotriturus were established in the relationships of elements forming the suborbital portion of the skull roof, features of tooth implantation, as well as in the pattern of vasculature of the jaw bones. In spite the specialized condition of the dental system of P. herrei and its upper-most (terminal Urzhumian) stratigraphic position in comparison with other bolosaurid species, the morphology of its cheek region exhibits more similarity with that of the lower Permian bolosaurids of North America other than members of the genus Belebey. The absence of clear diagnostic criteria allows no possibility for subdivision of the order Bolosaurida on taxa of the family rank based on its middle Permian representatives.



A tail vertebra of a giant sea turtle (Testudines: Chelonioidea) from the Upper Cretaceous deposits of the Malyy Prolom locality (Ryazan Province, Russia)
摘要
The article describes a tail vertebra of a giant sea turtle Chelonioidea indet. from the Upper Cretaceous Malyy Prolom locality (Ryazan Province, Russia; middle Cenomanian – middle Santonian). The tail vertebra, probably IV–X, with a preserved length of 3.8 cm belonged to a turtle comparable in size with the type specimen of the protostegid Archelon ischyros from the Campanian of USA. The proportions of the vertebral centrum suggest that it belonged to a female.



To the question about trophic adaptations of Ornithosuchids (Archosauria)
摘要
Ornithosuchidae differ from other carnivore archosaurs in the unique morphology of the jaw apparatus and postcranial skeleton. Various, often diametrically opposed, points of view have been expressed regarding their trophic adaptations – from carnivory and scavering to piscivory. The most reasonable hypothesis seems to be that ornithosuchids were hyperanisodont carnivorous macrophages in the middle size class. Moreover, there are some analogies between ornithosuchids and saber-toothed therapsids and mammals.



First data on the neopleistocene mammal fauna from Oldzho River locality (Upper Yana Region, Sakha Republic, Russia)
摘要
The article presents the first complete data on the finds of mammals of the mammoth fauna in the Upper Yana basin (Verkhoyansky Ulus, Oldzho River). A list of mammal species of the locality on the Oldzho River was compiled. 11 mammal species were identified. The snow sheep was noted for the Upper Yana area for the first time. The absolute age of the locality is over 49 thousand years. It was formed during the beginning of Karginsky interstadial (MIS 3). A small amount of remains of species adapted to the conditions of the Arctic zone (reindeer, musk ox) and the complete absence of such species as the arctic fox and wolverine, indicate significant differences between the fauna of Oldzho and the later typically Sartan Fauna. The geomorphology of the locality differs from the typical permafrost sections in the north of the Yana-Indigirka Lowland. In the Oldzho upper part of the section consist of edom loss-ice sediments. On Oldzho the ice thickness does not exceed 4–4.5 meters and it is confined the top of the 50 meters terrace. The base of the terrace is a sandstone and mudstone bedrock. Bones bed layer located under the ice in the loess-like loams with layers of peat and inclusions of plant detritus. Bones of bison, horse, woolly rhinoceros, red deer dominate quantitatively. All age groups of herbivorous mammals are provided. Predators (bear, cave lion, wolf) are represented only by adult individuals. Relatively common pathologies of the limb bones in herbivorous mammals caused by traumatic injuries have been noted.


