scholarly journals PRELIMINARY SURVEY OF THE GROUND-DWELLING ARTHROPODS OF THE FLOOD-PLAIN MEADOWS IN THE SOUTHEAST OF POLTAVA REGION (UKRAINE)

Author(s):  
N. Zhuravel ◽  
N. Polchaninova ◽  
I. Lezhenina ◽  
O. Drovgalenko ◽  
A. Putchkov

<p>A total number of 35 spider species and more than 170 insect species from five orders were recorded from the southeast of Poltava Region through the pitfall-trapping in the floodplain meadows. Six spider species, eight true bug species, and five beetle species are new for Poltava Region; one spider species (<em>Pardosa maisa</em>) and one fly species (<em>Aphanotrigonum</em><em> </em><em>brachypterum</em>) are new for Ukraine. For <em>A.</em><em> </em><em>brachypterum, </em>it is the first record from the East European Plain. Spider assemblages were the most abundant in the terms of species and individuals in a saline meadow while the beetles preferred mesic non-saline meadows. A checklist of collected species is given, and the geographic distribution of the rare species is discussed.</p>


2019 ◽  
Vol 12 (1) ◽  
Author(s):  
Rafael Tavares ◽  
Leonardo Sanchez ◽  
Jose Manuel Briceño

Abstract One specimen of the ragged-tooth shark, Odontaspis ferox, was caught by a commercial shark fishery to the north of Cape Codera (10° 56′ N, 66° 02′ W), northeastern Venezuela. The specimen (sex unidentified, ~ 180 cm TL, ~ 30 kg) was identified on the basis of its dry jaw and characteristic dentition: which comprise teeth moderately large, with prominent narrow cusps and two or three pairs of lateral cusplets. This is the first record of O. ferox in the Venezuelan Caribbean, and this finding complements the knowledge of geographic distribution of this rare species in the Western Central Atlantic.



Check List ◽  
2016 ◽  
Vol 12 (6) ◽  
pp. 2001 ◽  
Author(s):  
Olga S. Shiryaeva

Clitocybula lignicola is predominantly distributed in the Asian part of Russia. In Europe it was found only in the Urals (Komi Republic, Russia). Two new localities are situated in the northwestern part of Vologda Region (Russia). These are the first records of this species from the East European Plain, as well as the most western ones known in Europe. New records extend the geographic distribution of C. lignicola 1,204 km west of the closest site in the Urals. An updated distribution map for the species is presented and a detailed species description with illustrations based on studied collections is provided.



2020 ◽  
Vol 29 (1) ◽  
pp. 60-69
Author(s):  
V.N. Podshivalina ◽  
N.G. Sheveleva

The calanoid copepod species Sinodiaptomus sarsi (Rylov, 1923) is recorded from the East European Plain (the Sura River floodplain, Middle Volga Region, Russia) for the first time. A brief description and illustrations of the species are provided, and some differences between its European and Asian populations are revealed. The studied population of S. sarsi from the Sura River basin is mostly similar in morphological characters to populations from China and Japan.



Zoodiversity ◽  
2021 ◽  
Vol 55 (2) ◽  
pp. 95-112
Author(s):  
N Polchaninova ◽  
V. Gnelitsa ◽  
V. Terekhova ◽  
A. Iosypchuk

An annotated list of 31 spider species of 12 families collected in Northeasten, Easten and Southern Ukraine is presented. Four speceis, Marinarozelotes manychensis (Ponomarev & Tsvetkov, 2006), Turkоzelotes kazachstanicus (Ponomarev et Tsvetkov, 2006), Zelotes atrocaeruleus (Simon, 1878), and Z. puritanus Chamberlin, 1922, are recorded for the first time from Ukraine. For Micaria coarctata (Lucas, 1846), this is the first record from the East European Plain. Nine species were recorded for the first time from Left-Bank Ukraine. To date, 1081 spider species are known from Ukraine and 757 species from Left-Bank Ukraine. Bsed on recent data, the northern boundaries of the geographic ranges of Drassyllus crimeaensis Kovblyuk, 2003 and Bassanioides caperatus (Simon, 1875) run along the northern coast of the Sea of Azov. For Marinarozelotes manychensis and Turkоzelotes kazachstanicus the northwestern coast of the Sea of Azov is the westernmost known limits of their distiribution. The range of Heriaeus horridus Tyschchenko, 1965 is delimited in the west by the right bank of the Dnieper estuary. Thirteen species are illlustrted.



2017 ◽  
pp. 94-108 ◽  
Author(s):  
Yu. A. Semenishchenkov

Phytogeographical features of forest vegetation at the level of lower-rank syntaxa were being discussed in literature since the early 20th century (Cajander, 1903; Sukachev, 1926; Braun-Blanquet, 1964; Kral et al., 1975; Kleopov, 1990; Bulokhov, 2003; Ellenberg, 2009), however, phytocoenologists still have no uniform interpretation and geographical maintenance of lower classification units. Forest vegetation of the European part of Russia is well studied according to Braun-Blanquet approach with association as a system of geographical subassociations. The paper offers the approaches to the reflection of geographical variations of the natural forest vegetation in the basin of the Upper Dnieper (central part of the East European Plain) at the level of lower-rank syntaxa The xeromesophytic oak woods in the basin of the Upper Dnieper belong to the East European ass. Lathyro nigri–Quercetum roboris Bulokhov et Solomeshch 2003. Floristic differentiation of this association from the similar Central European ass. Potentillo-Quercetum is given. These two associations have large blocks of geographically significant differential species that does not allow to consider them as a part of one association. The suggested approach allows to define the chorological content of units of lower syntaxonomical ranks and make regional classification schemes comparable to each other.



2021 ◽  
Vol 4 (1) ◽  
Author(s):  
R. Dinnis ◽  
A. Bessudnov ◽  
N. Reynolds ◽  
T. Devièse ◽  
A. Dudin ◽  
...  

AbstractThe Streletskian is central to understanding the onset of the Upper Palaeolithic on the East European Plain. Early Streletskian assemblages are frequently seen as marking the Neanderthal-anatomically modern human (AMH) anthropological transition, as well as the Middle-to-Upper Palaeolithic archaeological transition. The age of key Streletskian assemblages, however, remains unclear, and there are outstanding questions over how they relate to Middle and Early Upper Palaeolithic facies. The three oldest Streletskian layers—Kostenki 1 Layer V, Kostenki 6 and Kostenki 12 Layer III—were excavated by A. N. Rogachev in the mid-20th century. Here, we re-examine these layers in light of problems noted during Rogachev’s campaigns and later excavations. Layer V in the northern part of Kostenki 1 is the most likely assemblage to be unmixed. A new radiocarbon date of 35,100 ± 500 BP (OxA- X-2717-21) for this assemblage agrees with Rogachev’s stratigraphic interpretation and contradicts later claims of a younger age. More ancient radiocarbon dates for Kostenki 1 Layer V are from areas lacking diagnostic Streletskian points. The Kostenki 6 assemblage’s stratigraphic context is extremely poor, but new radiocarbon dates are consistent with Rogachev’s view that the archaeological material was deposited prior to the CI tephra (i.e. >34.3 ka BP). Multiple lines of evidence indicate that Kostenki 12 Layer III contains material of different ages. Despite some uncertainty over the precise relationship between the dated sample and diagnostic lithic material, Kostenki 1 Layer V (North) therefore currently provides the best age estimate for an early Streletskian context. This age is younger than fully Upper Palaeolithic assemblages elsewhere at Kostenki. Other “Streletskian” assemblages and Streletskian points from younger contexts at Kostenki are briefly reviewed, with possible explanations for their chronostratigraphic distribution considered. We caution that the cultural taxon Streletskian should not be applied to assemblages based simply on the presence of bifacially worked artefacts.



2018 ◽  
Vol 51 (1) ◽  
pp. 66-72 ◽  
Author(s):  
A. T. Barabanov ◽  
S. V. Dolgov ◽  
N. I. Koronkevich ◽  
V. I. Panov ◽  
A. I. Petel’ko


Sign in / Sign up

Export Citation Format

Share Document