scholarly journals A newCampanula(Campanulaceae) from east Anatolia, Turkey

2007 ◽  
Vol 25 (1-2) ◽  
pp. 53-57 ◽  
Author(s):  
Ali Kandemir
Keyword(s):  
Crustaceana ◽  
2014 ◽  
Vol 87 (3) ◽  
pp. 328-339 ◽  
Author(s):  
Hui Ming Li ◽  
Bo Ping Han ◽  
Fei Fei Guo ◽  
Henri J. Dumont

In 1964 and 1965, Shen & Tai described two species of calanoids, which they classified in the South American genus Argyrodiaptomus. We examined new material from the terra typica, South China, and show that both species belong in the Asian genus Sinodiaptomus. A biogeographic anomaly is thus corrected. Moreover, the two appear to be sister species and males are morphologically well separable. No intermediate morphotypes have so far been detected. S. cavernicolax (Shen & Tai, 1965), known only from the type locality, was claimed to be cavernicolous, but shows no stygobitic adaptations, and has eyes. It may have been pushed back into the cave environment by its congener S. ferus (Shen & Tai, 1964) with which it coexists in the same lake system. So far, four species of Sinodiaptomus have been found in China: the two mentioned above, i.e., S. cavernicolax only in Longyan Cave of Zhaoqing City, and S. ferus at about five locations, but its range is limited to a small part of Guangdong Province. All five other species of Sinodiaptomus, among which the other two that occur (also) in China, also occupy small to very small ranges, with the type species (S. chaffanjoni Richard, 1897) only living in North China, and S. indicus Kiefer, 1936 and S. mahanandiensis Reddy & Radhakrishna, 1980 confined to South India (Reddy & Radhakrishna, 1980). S. valkanovi Kiefer, 1938 from Japan is invasive (Ueda & Ohtsuka, 1998; Makino et al., 2010). S. sarsi Rylov, 1923, distributed in Japan, China, and most of Mongolia, is separated by a wide disjunction from a group of populations in Iran, the Caucasus, and East Anatolia. This western group of populations might be a separate species and deserves more study.


2007 ◽  
Vol 25 (1-2) ◽  
pp. 58-63 ◽  
Author(s):  
Gülay Ecevit Genç ◽  
Ali Kandemir ◽  
İlker Genç

Quaternary ◽  
2021 ◽  
Vol 4 (3) ◽  
pp. 29
Author(s):  
Nurcan Avşin ◽  
Mehmet Korhan Erturaç ◽  
Eren Şahiner ◽  
Tuncer Demir

The paper describes climatic and tectonic effects on fluvial processes of East Anatolia. This study from the Muş Basin contains three alluvial terrace levels (T3-T1) ranging from 30–35 m to 3–5 m above the present Murat River in its middle section. In order to provide a chronology for the evaluation of the significant, effects of climatic changes and tectonic uplift, we used optically stimulated luminescence (OSL) dating of the river deposits of the youngest (T3) and medium terrace (T2). The ages from these terrace deposits show that the T3 has formed approximately 6.5 ka ago, i.e., during the last part of the Holocene (MIS 1) and T2 has formed nearly 25 ka ago, i.e., during MIS 2 at the ending of the last glacial period. According to these results, it appears that the Murat River established its terrace sequences both in cold and warm periods. The variations in climate oriented fluvial evolution between the East Anatolia fluvial system and the temperate-periglacial fluvial systems in Europe may be the conclusion of different vegetation cover and melting thicker snow coverings in cold periods.


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