Middle Asia

Author(s):  
Barakatullo Ashurov ◽  
Barakatullo Ashurov ◽  
Chiara Barbati ◽  
George D. Chryssides ◽  
Dagikhudo Dagiev ◽  
...  
Keyword(s):  
Author(s):  
М.Г. ПИМЕНОВ ◽  
E.V. KLJUYKOV ◽  
G.V. DEGTJAREVA

New material on a rare species Silaum saxatilis (Umbelliferae) from southern limit of the Dzungarian Alatau (South-Eastern Kazakhstan) allowed to describe the structure of its fruits. The species is assigned to a distinct monotypic genus Tschulaktavia, the generic name was proposed by M. S. Bajtenov and validated here. Another speciens described by Bajtenov, Stenotaenia iliensis, is synonymized with Hyalolaena tshuiliensis. The genus Stenotaenia does not occus in Kazakhstan and the Middle Asia. 658


2021 ◽  
Author(s):  
Arkadiusz Nowak ◽  
Sebastian Świerszcz ◽  
Sylwia Nowak ◽  
Marcin Nobis

AbstractThis paper presents the results of phytosociological research on scree vegetation of the Pamir and south-western Tian Shan. We collected 222 phytosociological relevés during field studies conducted in 2015–2019, applying the Braun-Blanquet approach. We identified 21 plant communities on mobile and stabilized screes of colluvial cones, aprons and fans, inhabiting mainly the montane and alpine belts in several ranges (e.g. Peter the First, Alichur, Shugnan, Shachdarian, Darvaz, Rushan, Vanch, Fergana, Kyrgyz and Terskey ranges). As a result we provide the first comprehensive hierarchical syntaxonomic synopsis of scree communities at montane and alpine elevations in the eastern Middle Asia. The collected vegetation relevés represent the majority of the variation among the phytocoenoses of gravel, pebble, cobble and rock block slides and screes in the montane and alpine belts. As a result of field studies and Twinspan analyses, nine associations were identified on screes of the Pamir and western Tian Shan. All these communities were assigned to the Sileno brahuicae-Lactucetalia orientalis Nowak et al. 2021. Additionally, within the nitrophilous compact gravel screes one subassociation of Corydalidetum kashgaricae trigonelletosum gontscharovii was distinguished. In the most arid zone two additional plant associations and one subassociation were identified in gravelly semi-deserts zone. The main factors determining the species composition of the studied associations are scree mobility, rock particle size, elevation above sea level and slope inclination. Our research revealed considerable diversity of scree habitats of montane and alpine belts what might be astonishing regarding harsh environment of this mountainous territory. However, a great number of lineages that evolved here and particularly rich species pool of this habitat in Middle Asia facilitate remarkable diversity among vegetation of taluses and screes. The distinctiveness of species composition is additionally enhanced by high degree of endemism of chasmophytic habitats in the eastern part of Middle Asia. Despite recent developments, the prominent chasmophytic vegetation of Middle Asia still needs thorough studies focused on its relationship to semi-desert, tall-forb and petrophytic communities of high mountains of the Pamir, Hindu-Kush, Kunlun and Central Tian Shan.


Author(s):  
Viktoria Wagner ◽  
Tatyana M. Bragina ◽  
Arkadiusz Nowak ◽  
Ilya E. Smelansky ◽  
Kim André Vanselow
Keyword(s):  

2007 ◽  
Vol 16 (2) ◽  
pp. 285-288
Author(s):  
S.V. Baryshnikova

Bucculatrix malivorella sp. n. from Middle Asia and B. pectinifera sp. n. from the Far East of Russia are described.


2015 ◽  
Author(s):  
Igor Danilov ◽  
Ekaterina Obraztsova ◽  
Vladimir Sukhanov

Background. This report reviews data on taxonomic diversity and paleobiogeography of Late Cretaceous (K2) non-marine turtles of Asia accumulated since latest reviews in 2000s. K2 non-marine turtles of Asia are known from four main geographical areas: Middle Asia-Kazakhstan (MAK), Mongolia (MO), China (CH) and Japan (JA). Methods. We critically reviewed composition of non-marine turtle assemblages of the K2 for each of the mentioned geographical area to make estimates of taxonomic diversity for different ages of the K2. Based on these data we analyzed temporal distribution of taxa of non-marine turtles and change in taxonomic diversity of turtle assemblages. Results. K2 turtles of MAK are represented by eight suprageneric taxa – Adocidae (Ad), Carettochelyidae (Ca), Lindholmemydidae (Li), Macrobaenidae (Ma), Nanhsiungchelyidae (Na), Trionychidae (Tr), Eucryptodira indet. (Eu), and Testudines indet. (Te), of which Ad, Li, Ma and Tr are known from the Cenomanian(CE) – early Campanian(CA), whereas other taxa only from the CE-early Turonian(TU). Taxonomic diversity changes from 10–12 species and genera, 6–8 suprageneric taxa in the CE to 7 species and genera, 4 families in the late TU early CA. K2 turtles of MO are represented by seven suprageneric taxa – Ad, Ca, Li, Ma, Meiolaniformes (Me), Na, and Tr, of which Li, Na and Tr are known from the CE-Maastrichtian(MA), Ad, Ca, and Ma, from the CE-Santonian(SA), and Me, only from the MA. Taxonomic diversity changes from 12 species, 10 genera, 6 families in the CE – SA, 8–9 species, 7–9 genera, 3 families in the CA, and 9 species, 7–8 genera, and 4 suprageneric taxa in the MA. K2 turtles of CH are represented by three suprageneric taxa (Li, Na, and Tr), but their precise temporal distribution is poorly known. Taxonomic diversity in the K2 is 12 species, 11–12 genera, and 3 families. K2 turtles of JA are represented by six suprageneric taxa (Ad, Ca, Na, Tr, Eu, and Te), of which Na are known from the CE-SA, Tr from the Coniacian(CO)-CA, and other taxa from the CO-SA. Taxonomic diversity changes from 1 species, genus, and family in the CE-TU to 7 species and genera, and 5–6 suprageneric taxa in the CO-SA. Discussion. In MAK, most significant transformation of turtle assemblages occurred in the CE-TU, whereas transformation in the SA-CA was less significant. On the contrary, in MO, most significant transformation occurred in the SA-CA, and less significant in the CA-MA.The patterns of transformation of the K2 turtle assemblages of CH and JA are not clear. The differences in the patterns of diversity and transformations of the K2 turtle assemblages in different geographical areas of Asia may be explained by different environmental conditions in these areas at that time and influence of such factors as transgressions in coastal areas (MAK and JA) and cooling and aridizations in inland areas (MO and CH).


2009 ◽  
Vol 11 (2) ◽  
pp. 119
Author(s):  
Wahyudin Darmalaksana

<p>This paper intends to explore the historical aspect of Mamalik dynasty. It was associated with Daulah Islamiyah in Mesir which lead by slave group (Mamalik) from 13th century up to 16th A.D that became one of unique Islamic political faces. At that time, civil society can form themselves as military power driven by slavers. Retired slavers emerged as political elite and bodyguard of Sultan. Mamalik group divided into two groups. First, Mamalik Bahriyah coming from middle Asia, especially Turkey Qipsaq. Second, Mamalik Burjiyah coming from Sirkasia race in·Kaukasus (East Europe). Historically, Mamalik Dynasty in Mesir classified into three periods. First, the period of Mamalik government formation which was "oligarchy". Second, the period of development in which Mamalik group cooperated with Mogol and Europe country. Third, the period of saturation or the decrease of Mamalik dynasty in Mesir which was caused by the attack of Turkey Utsmani, disease epidemic, and corruption.</p><p> </p><p>Makalah ini bermaksud untuk mengeksplorasi aspek historis dinasti Mamalik. Itu terkait dengan Daulah Islamiyah di Mesir yang dipimpin oleh kelompok budak (Mamalik) dari abad ke-13 hingga 16. yang menjadi salah satu wajah politik Islam yang unik. Saat itu, masyarakat dapat membentuk diri mereka sebagai kekuatan militer yang dikendalikan oleh budak.<br />Mantan budak muncul sebagai elit politik dan pengawal Sultan. Kelompok Mamalik dibagi menjadi dua kelompok. Pertama, Mamalik Bahriyah yang berasal dari Asia tengah, terutama Turki Qipsaq. Kedua, Mamalik Burjiyah berasal dari ras Sirkasia di Kaukasia (Timur Eropa). Secara historis, Dinasti Mamalik di Mesir digolongkan ke dalam tiga periode. Pertama, periode pembentukan pemerintahan Mamalik<br />yang merupakan "oligarki". Kedua, periode perkembangan di mana Kelompok Mamalik bekerja sama dengan Mongolia dan negara Eropa. Ketiga, periode kejenuhan atau penurunan dinasti Mamalik di Mesir yang disebabkan oleh serangan Turki Utsmani, epidemi penyakit, dan korupsi.</p>


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