Plankton biostratigraphy and magnetostratigraphy of the Santonian–Campanian boundary interval in the Mudurnu–Göynük Basin, northwestern Turkey

2018 ◽  
Vol 87 ◽  
pp. 296-311 ◽  
Author(s):  
Erik Wolfgring ◽  
Michael Wagreich ◽  
Jaume Dinarès-Turell ◽  
Ismail Omer Yilmaz ◽  
Katharina Böhm
Keyword(s):  
1998 ◽  
Vol 25 (14) ◽  
pp. 2733-2736 ◽  
Author(s):  
Horasan Gündüz ◽  
Kaşlilar-Özcan Ayşe ◽  
Boztepe-Güney Aysun ◽  
Türkelli Niyazi

Microbiology ◽  
2003 ◽  
Vol 149 (9) ◽  
pp. 2539-2544 ◽  
Author(s):  
Ece S. Güner ◽  
Naoya Hashimoto ◽  
Teruki Kadosaka ◽  
Yasuyuki Imai ◽  
Toshiyuki Masuzawa

A novel, fast-growing spirochaete was isolated from the hard tick Hyalomma aegyptium (family Ixodidae, subfamily Metastriata) using Barbour–Stoenner–Kelly (BSK) II medium. Tick samples were taken during the summer of 2000 from the Istanbul area in northwestern Turkey. Sixty-seven of 153 adults (44 %) and 72 of 185 nymphs (39 %) were infected with the novel spirochaete, whereas none of the 20 larvae examined were infected. The optimal growth temperature of the spirochaete in BSK II medium was 34–37 °C, and it could grow at 39 °C. Doubling times at 34 and 37 °C were 5·3 and 5·1 h, respectively. Six pure cultures of the spirochaete were obtained and characterized by microscopic observation, sequence analysis of the flagellin gene (flaB), SDS-PAGE and Western blotting. The spirochaete was morphologically similar to those of the genus Borrelia and contained a 41 kDa protein reactive with mAb H9724 specific to the flagellin of a Borrelia species. Polyclonal antibody raised to this spirochaete reacted with several antigen bands, whereas no bands were detected with Borrelia burgdorferi, Borrelia hermsii, Borrelia turicatae and Borrelia parkeri. The flaB sequences of the six isolates showed high similarity, with sequence similarity values ranging from 99·2 to 100 %; however, the similarity of the isolates' flaB sequences to those of the Lyme-disease-related Borrelia and relapsing-fever-associated Borrelia species was less than 90 %. These findings suggest that the unique spirochaete is a member of the genus Borrelia, and differs from previously described Borrelia species.


2006 ◽  
Vol 6 (6) ◽  
pp. 999-1006 ◽  
Author(s):  
Y. Altınok ◽  
B. Alpar

Abstract. The long-term seismicity of the Marmara Sea region in northwestern Turkey is relatively well-recorded. Some large and some of the smaller events are clearly associated with fault zones known to be seismically active, which have distinct morphological expressions and have generated damaging earthquakes before and later. Some less common and moderate size earthquakes have occurred in the vicinity of the Marmara Islands in the west Marmara Sea. This paper presents an extended summary of the most important earthquakes that have occurred in 1265 and 1935 and have since been known as the Marmara Island earthquakes. The informative data and the approaches used have therefore the potential of documenting earthquake ruptures of fault segments and may extend the records kept on earthquakes far before known history, rock falls and abnormal sea waves observed during these events, thus improving hazard evaluations and the fundamental understanding of the process of an earthquake.


2020 ◽  
Author(s):  
Nurşen Çördük ◽  
Cüneyt Aki

Digitalis trojana Ivanina is a member of the Plantaginaceae family and known by its common name, Helen of Troy foxglove. It is perennial endemic to Çanakkale and Balıkesir, northwestern Turkey. In order to develop an efficient shoot regeneration protocol, the leaf explants of D. trojana were cultured on Murashige and Skoog (MS) medium containing 6-benzyl adenine (0.1, 0.5, 1.0, 3.0, 5.0 mg/L) and α-naphthalene acetic acid (0.1, 0.5, 1.0 mg/L), 3% (w/v) sucrose and 0.8% (w/v) agar. The highest number of regenerated shoots was obtained from leaf explants that were cultured on MS medium with 3.0 mg/L BA+0.1 mg/L NAA. Regenerated shoots were rooted on MS medium without plant growth regulators. Rooted plants (2–3 cm) were separately transferred to pots containing a mixture of peat and perlite (2:1 v/v) and acclimatized successfully in a growth chamber.


1972 ◽  
Author(s):  
Herbert Samuel Jacobson ◽  
F. Ozelci ◽  
Durmaz Yazgan ◽  
N. Hatay ◽  
Hamit Karahacioglu
Keyword(s):  

2012 ◽  
Vol 57 (1) ◽  
pp. 142-146 ◽  
Author(s):  
Matthias Olthoff ◽  
Dietmar Ikemeyer
Keyword(s):  
Peat Bog ◽  

Solid Earth ◽  
2019 ◽  
Vol 10 (3) ◽  
pp. 785-807 ◽  
Author(s):  
Ershad Gholamrezaie ◽  
Magdalena Scheck-Wenderoth ◽  
Judith Bott ◽  
Oliver Heidbach ◽  
Manfred R. Strecker

Abstract. The Sea of Marmara, in northwestern Turkey, is a transition zone where the dextral North Anatolian Fault zone (NAFZ) propagates westward from the Anatolian Plate to the Aegean Sea Plate. The area is of interest in the context of seismic hazard of Istanbul, a metropolitan area with about 15 million inhabitants. Geophysical observations indicate that the crust is heterogeneous beneath the Marmara basin, but a detailed characterization of the crustal heterogeneities is still missing. To assess if and how crustal heterogeneities are related to the NAFZ segmentation below the Sea of Marmara, we develop new crustal-scale 3-D density models which integrate geological and seismological data and that are additionally constrained by 3-D gravity modeling. For the latter, we use two different gravity datasets including global satellite data and local marine gravity observation. Considering the two different datasets and the general non-uniqueness in potential field modeling, we suggest three possible “end-member” solutions that are all consistent with the observed gravity field and illustrate the spectrum of possible solutions. These models indicate that the observed gravitational anomalies originate from significant density heterogeneities within the crust. Two layers of sediments, one syn-kinematic and one pre-kinematic with respect to the Sea of Marmara formation are underlain by a heterogeneous crystalline crust. A felsic upper crystalline crust (average density of 2720 kg m−3) and an intermediate to mafic lower crystalline crust (average density of 2890 kg m−3) appear to be cross-cut by two large, dome-shaped mafic high-density bodies (density of 2890 to 3150 kg m−3) of considerable thickness above a rather uniform lithospheric mantle (3300 kg m−3). The spatial correlation between two major bends of the main Marmara fault and the location of the high-density bodies suggests that the distribution of lithological heterogeneities within the crust controls the rheological behavior along the NAFZ and, consequently, maybe influences fault segmentation and thus the seismic hazard assessment in the region.


2020 ◽  
Vol 725 ◽  
pp. 138227
Author(s):  
Naama Lang-Yona ◽  
Fatma Öztürk ◽  
Daniella Gat ◽  
Merve Aktürk ◽  
Emre Dikmen ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document