Gelechiaomelkoi sp. nov. – a new species from the Russian Altai Mountains related to the Nearctic Gelechiamandella Busck, 1904 (Lepidoptera, Gelechiidae), with a synopsis of Gelechia from the Altai Republic of Russia
Ontology highlight
ABSTRACT:
SUBMITTER: Bidzilya O
PROVIDER: S-EPMC8548287 | biostudies-literature |
REPOSITORIES: biostudies-literature
Similar Datasets
Project description:Eidophasia assmanni sp. nov., a new species of Plutellidae from the alpine zone of Russian Altai Mountains, is described from diagnostic morphology and DNA barcodes. Male adult and genitalia are illustrated, whereas the female sex remains unknown. The species inhabits alpine scree with patchy herbaceous plants and is considered as possible endemic species of the Altai Mountains. An updated checklist of the 13 global Eidophasia Stephens, 1842 species is provided. The likely polyphyly of the genus is discussed from molecular data of the barcode region of the mt COI gene.
| S-EPMC7442753 | biostudies-literature
Project description:Denisova Cave in southern Siberia uniquely contains evidence of occupation by a recently discovered group of archaic hominins, the Denisovans, starting from the middle of the Middle Pleistocene. Artefacts, ancient DNA and a range of animal and plant remains have been recovered from the sedimentary deposits, along with a few fragmentary fossils of Denisovans, Neanderthals and a first-generation Neanderthal-Denisovan offspring. The deposits also contain microscopic traces of hominin and animal activities that can provide insights into the use of the cave over the last 300,000 years. Here we report the results of a micromorphological study of intact sediment blocks collected from the Pleistocene deposits in the Main and East Chambers of Denisova Cave. The presence of charcoal attests to the use of fire by hominins, but other evidence of their activities preserved in the microstratigraphic record are few. The ubiquitous occurrence of coprolites, which we attribute primarily to hyenas, indicates that the site was visited for much of its depositional history by cave-dwelling carnivores. Microscopic traces of post-depositional diagenesis, bioturbation and incipient cryoturbation are observed in only a few regions of the deposit examined here. Micromorphology can help identify areas of sedimentary deposit that are most conducive to ancient DNA preservation and could be usefully integrated with DNA analyses of sediments at archaeological sites to illuminate features of their human and environmental history that are invisible to the naked eye.
| S-EPMC6763451 | biostudies-literature
Project description:The checklist of European Gelechiidae covers 865 species, belonging to 109 genera, with three species records which require confirmation. Further, it is the first checklist to include a complete coverage of proved synonyms of species and at generic level. The following taxonomic changes are introduced: Pseudosophronia constanti (Nel, 1998) syn. nov. of Pseudosophronia exustellus (Zeller, 1847), Metzneria expositoi Vives, 2001 syn. nov. of Metzneria aestivella (Zeller, 1839); Sophronia ascalis Gozmány, 1951 syn. nov. of Sophronia grandii Hering, 1933, Aproaerema incognitana (Gozmány, 1957) comb. nov., Aproaerema cinctelloides (Nel & Varenne, 2012) comb. nov., Aproaerema azosterella (Herrich-Schäffer, 1854) comb. nov., Aproaerema montanata (Gozmány, 1957) comb. nov., Aproaerema cincticulella (Bruand, 1851) comb. nov., Aproaerema buvati (Nel, 1995) comb. nov., Aproaerema linella (Chrétien, 1904) comb. nov., Aproaerema captivella (Herrich-Schäffer, 1854) comb. nov., Aproaerema semicostella (Staudinger, 1871) comb. nov., Aproaerema steppicola (Junnilainen, 2010) comb. nov., Aproaerema cottienella (Nel, 2012) comb. nov., Ptocheuusa cinerella (Chrétien, 1908) comb. nov., Pragmatodes melagonella (Constant, 1895) comb. nov., Pragmatodes albagonella (Varenne & Nel, 2010) comb. nov., Pragmatodes parvulata (Gozmány, 1953) comb. nov., Oxypteryx nigromaculella (Millière, 1872) comb. nov., Oxypteryx wilkella (Linnaeus, 1758) comb. nov., Oxypteryx ochricapilla (Rebel, 1903) comb. nov., Oxypteryx superbella (Zeller, 1839) comb. nov., Oxypteryx mirusella (Huemer & Karsholt, 2013) comb. nov., Oxypteryx baldizzonei (Karsholt & Huemer, 2013) comb. nov., Oxypteryx occidentella (Huemer & Karsholt, 2011) comb. nov., Oxypteryx libertinella (Zeller, 1872) comb. nov., Oxypteryx gemerensis (Elsner, 2013) comb. nov., Oxypteryx deserta (Piskunov, 1990) comb. nov., Oxypteryx unicolorella (Duponchel, 1843) comb. nov., Oxypteryx nigritella (Zeller, 1847) comb. nov., Oxypteryx plumbella (Heinemann, 1870) comb. nov., Oxypteryx isostacta (Meyrick, 1926) comb. nov., Oxypteryx helotella (Staudinger, 1859) comb. nov., Oxypteryx parahelotella (Nel, 1995) comb. nov., Oxypteryx graecatella (Šumpich & Skyva, 2012) comb. nov.; Aproaerema genistae (Walsingham, 1908) comb. rev., Aproaerema thaumalea (Walsingham, 1905) comb. rev.; Dichomeris neatodes Meyrick, 1923 sp. rev.; Caryocolum horoscopa (Meyrick, 1926) stat. rev.; Ivanauskiella occitanica (Nel & Varenne, 2013) sp. rev.; Apodia martinii Petry, 1911 sp. rev.; Caulastrocecis cryptoxena (Gozmány, 1952) sp. rev. Following Article 23.9.2 ICZN we propose Caryocolum blandella (Douglas, 1852) (Gelechia) nom. protectum and Caryocolum signatella (Eversmann, 1844) (Lita) nom. oblitum.
| S-EPMC7109147 | biostudies-literature
Project description:In this article, we report and discuss the results obtained from a survey of plants, microorganisms (bacteria and fungi), and soil elements along a chronosequence in the first 600 m of the Maliy Aktru glacier's forefront (Altai Mountains, Russia). Many glaciers of the world show effects of climate change. Nonetheless, except for some local reports, the ecological effects of deglaciation have been poorly studied and have not been quantitatively assessed in the Altai Mountains. Here, we studied the ecological changes of plants, fungi, bacteria, and soil elements that take the form of a primary ecological succession and that took place over the deglaciated soil of the Maliy Aktru glacier during the last 50 year. According to our measurements, the glacier lost about 12 m per year during the last 50 years. Plant succession shows clear signs of changes along the incremental distance from the glacier forefront. The analysis of the plant ?- and ?-diversity confirmed an expected increase of them with increasing distance from the glacier forefront. Moreover, the analysis of ?-diversity confirmed the hypothesis of the presence of three main stages of the plant succession: (a) initial (pioneer species) from 30 to 100 m; (b) intermediate (r-selected species) from 110 to 120-150 m; and (c) final (K-selected species) from 150 to 550. Our study also shows that saprotrophic communities of fungi are widely distributed in the glacier retreating area with higher relative abundances of saprotroph ascomycetes at early successional stages. The evolution of a primary succession is also evident for bacteria, soil elements, and CO 2 emission and respiration. The development of biological communities and the variation in geochemical parameters represent an irrefutable proof that climate change is altering soils that have been long covered by ice.
| S-EPMC6106165 | biostudies-other
Project description:We present a high-quality genome sequence of a Neanderthal woman from Siberia. We show that her parents were related at the level of half-siblings and that mating among close relatives was common among her recent ancestors. We also sequenced the genome of a Neanderthal from the Caucasus to low coverage. An analysis of the relationships and population history of available archaic genomes and 25 present-day human genomes shows that several gene flow events occurred among Neanderthals, Denisovans and early modern humans, possibly including gene flow into Denisovans from an unknown archaic group. Thus, interbreeding, albeit of low magnitude, occurred among many hominin groups in the Late Pleistocene. In addition, the high-quality Neanderthal genome allows us to establish a definitive list of substitutions that became fixed in modern humans after their separation from the ancestors of Neanderthals and Denisovans.
| S-EPMC4031459 | biostudies-literature
Project description:In this research, the complete mitochondrial genome (mitogenome) of Phthorimaea operculella was sequenced and annotated. The mitogenome of P. operculella is 15,269 bp in length and contains 13 protein-coding genes (PCGs), 22 transfer RNA (tRNA) genes, 2 ribosome RNA (12s and 16srRNA) genes and 1 control region. In addition, we used Endoclita signifier as the outgroup to analyze phylogenetic relationship, and the phylogenetic tree showed the sister relationship between P. operculella and Tuta absoluta.
| S-EPMC8221163 | biostudies-literature
Project description:The phenomenon of "tree waves" (hedges and ribbons) formation within the alpine ecotone in Altai Mountains and its response to observed air temperature increase was considered. At the upper limit of tree growth Siberian pine (Pinus sibirica) forms hedges on windward slopes and ribbons on the leeward ones. Hedges were formed by prevailing winds and oriented along winds direction. Ribbons were formed by snow blowing and accumulating on the leeward slope and perpendicular to the prevailing winds, as well as to the elevation gradient. Hedges were always linked with microtopography features, whereas ribbons were not. Trees are migrating upward by waves and new ribbons and hedges are forming at or near tree line, whereas at lower elevations ribbons and hedges are being transformed into closed forests. Time series of high-resolution satellite scenes (from 1968 to 2010) indicated an upslope shift in the position ribbons averaged 155±26 m (or 3.7 m yr-1) and crown closure increased (about 35-90%). The hedges advance was limited by poor regeneration establishment and was negligible. Regeneration within the "ribbon zone" was approximately 2.5 times (5060 vs 2120 ha-1) higher then within the "hedges zone". During the last four decades, Siberian pine in both hedges and ribbons strongly increased its growth increment and recent tree growth rate for 50 year old trees was about twice higher than recorded for similarly aged trees at the beginning of the 20th century. Hedges and ribbons are phenomena that are widespread within the southern and northern Siberian Mountains.
| S-EPMC6039980 | biostudies-literature
Project description:The current study investigated the impacts of temperature on the development and reproductivity of the sweet potato leaf folder, Brachmia macroscopa (Lepidoptera: Gelechiidae), in sweet potato leaves under laboratory conditions. We determined developmental time of B. macroscopa larval, pupal, and pre-adult stage at different temperatures. Male and female longevity, male and female lifespan, mortality of immature stages, oviposition period of B. macroscopa were also investigated under six constant temperatures (21°C, 24°C, 27°C, 30°C, 33°C, 36°C), based on age-stage, two-sex life tables. The results revealed that eggs in 36°C were unable to hatch. At temperatures between 21°C -33°C, the duration of the pre-adult period, as well as the adult lifespan both for males and females, were shortened by increasing temperatures. The lowest larval mortality rate (15.33%) occurred at 27°C. The age-stage-specific fecundity rates with the greatest number were, in order, 30°C, 27°C, 21°C, 24°C and 33°C. The results show that B. macroscopa population levels could reach highest at the temperature of 27?.
| S-EPMC5333877 | biostudies-literature
Project description:Located in the intermediate zone between the taiga forests in Siberian Plain and the deserts in Central Asia, the Altai Mountains are of scientific concern about Holocene climate change in the past decades. However, researches about modern climate changes are relatively scarce in the Altai Mountains. In this study, temporal- spatial changes of air temperature and precipitation were investigated systematically in the Altai Mountains based on fifteen meteorological records over the period of 1970-2015. The Altai Mountains experienced a rapid warming trend with a rate of 0.41°C/decade and an insignificantly wetting trend at a rate of 4.82 mm/decade during 1970-2015. The magnitude of temperature trend was negatively correlated with elevation in cold season (spring and winter), whereas that was positively correlated with elevation in warm season (summer and autumn). The cyclonic anomalies to the northwest and an anticyclonic anomalies to the southeast blocked the southward cold air and then provided the favorable condition for an increasing precipitation via the southwesternly wind in the Altai Mountains.
| S-EPMC7077806 | biostudies-literature
Project description:The taxonomic status and biogeography of the North American Raphia species is reviewed using adult morphology, larval host plants, geographic phenotypic variation, and variation of mtDNA COI barcode sequences. Lack of diagnostic morphological differences, combined with relatively low mtDNA barcode divergences and clinal phenotypic variation in key geographic regions indicate that the six previously recognized species of North American Raphia are best interpreted as parapatric subspecies. Raphia frater abrupta Grote, stat. n., R. f. coloradensis Putnam-Cramer, stat. r., R. f. piazzi Hill, stat. n., and R. f. elbea Smith, stat. n., are accordingly revised to subspecies of R. frater Grote. Type locality restrictions are provided for Raphia abrupta and Raphia frater and a neotype is designated for Raphia frater var. coloradensis.
| S-EPMC4109472 | biostudies-literature