AIM： To detect distribution and relative frequency of endocrine cells in gastrointestinal tract of flower fish （Pseudophoxinus antalyae）. METHODS： The intestinal tract of flower fish was divided into four portions...AIM： To detect distribution and relative frequency of endocrine cells in gastrointestinal tract of flower fish （Pseudophoxinus antalyae）. METHODS： The intestinal tract of flower fish was divided into four portions from proximal to distal; the enlarged area after oesophagus and anterior, middle and posterior intestine. Immunohistochemical method using the peroxidase anti-peroxidase complex was employed. All antisera between four portions of flower fish were compared using ANOVA. RESULTS： Eleven types of gut endocrine cells were determined; they were immunoreactive for calcitonin gene related peptide, substance P, vasoactive intestinal peptide, bombesin, somatostatin-14, secretin, TrkA, TrkB, TrkC, neurotensin, neuropeptide Y, which were found in almost all portions of the gastrointestinal tract. CONCLUSION： The regional frequency of immunoreactive distribution and relative cells in the flower fish, Pseudophoxinus antalyae, are essentially similar to those of other fish.展开更多
March 3,2015 Antalya,Turkey An Expert Forum on Disaster Risk Reduction（DRR）in a Changing Climate:Lessons Learned about Lessons Learned,was convened by USAID,CCB/CU,WMO and TSMS with the support of NOAA and GFDRR** i...March 3,2015 Antalya,Turkey An Expert Forum on Disaster Risk Reduction（DRR）in a Changing Climate:Lessons Learned about Lessons Learned,was convened by USAID,CCB/CU,WMO and TSMS with the support of NOAA and GFDRR** in Antalya,Turkey,10 to 13 February 2015.展开更多
DüzlerçamıWildlife Reserve Area(WRA)is the last natural habitat of fallow deer(Dama dama)in the world.Fallow deer is native to Turkey,however,its geographical range is currently confined to Düzlerç...DüzlerçamıWildlife Reserve Area(WRA)is the last natural habitat of fallow deer(Dama dama)in the world.Fallow deer is native to Turkey,however,its geographical range is currently confined to DüzlerçamıWRA,Antalya.To date,a detailed habitat investigation of fallow deer dis-tribution has not been conducted.This study is vital for the last surviving populations of fallow deer in Turkey.There-fore,we studied the habitat suitability and utilization of fal-low deer in the DüzlerçamıWRA.Vegetation and wildlife inventory was surveyed across a total of 304 sample areas between 2015 and 2017.Plant species were recorded accord-ing to the Braun-Blanquet method and wildlife surveys were based on footprints,feces,and other signs of fallow deer.Classification and regression tree techniques,as well as MAXENT,were used to model vegetation and fallow deer habitat.Topographic position index,terrain ruggedness index,roughness index,elevation,and bedrock formation were also calculated and included in the models.Based on our results,we drafted a habitat protection map for fallow deer.To ensure sustainability of habitats where populations of fallow deer are found in Turkey,we developed recommen-dations such as closuring human access of the 1st-degree Protection Area and reintroduction of the species to other potential habitats.展开更多
The Antalya Complex within the Isparta Angle(IA)in the southwest of Türkiye includes various rock types formed in different geodynamic settings and contains important data that shed light on the geodynamic evolut...The Antalya Complex within the Isparta Angle(IA)in the southwest of Türkiye includes various rock types formed in different geodynamic settings and contains important data that shed light on the geodynamic evolution of the Eastern Mediterranean region.In this study,source rocks and tectonic settings of ancient sedimentary basins within the IA have been interpreted using geochemical contents of siliciclastic rocks in different ages.In this regard,whole-rock major,trace and rare earth element(REE)analyses have been conducted on the Cenozoic turbiditic sandstones(from the Eocene Isparta Formation and the Miocene Güneyce Formation in the north of the IA)and integrated with the available data of the Trias sic shales from the east and Upper Cretaceous sandstones from the southwest of the IA.The results indicate that Cenozoic sandstone samples are calcium-rich(CaO,30.54-43.87wt%,average 37.63 wt%),comparable to those of Upper Cretaceous sandstones(CaO,average 24.92 wt%)and Late Triassic(CaO,range between 11.27-26.71 wt%)shales.They demonstrate an excellent carbonate dilution effect on the majority of major oxides.In contrast to the Late Trias sic shales with close affinity to Post-Archean Average Archean Shale(PAAS),Cenozoic and Upper Cretaceous ophiolite-related clastic sediments display strike depletions in Nb-Ta,Th,Rb,Zr and Hf and enrichments in Ni,Co and Cr,suggesting mafic and ultramafic rocks in a source region.Notable enrichments of Cr(average 80.5 ppm),V(average 105.5 ppm),Ni(average 42.3 ppm)and Co(average13.9 ppm)in Late Triassic shales can be attributed to the influences of Triassic OIB-like basaltic rift magmatism in their source regions.In general,their igneous source rocks were derived from mixed sources,e.g.,(1)predominantly continental felsic and lesser rift-related basaltic mafic source rocks for Late Triassic shales,(2)mainly ophiolitic maficultramafic and lesser continental felsic source rocks for Upper Cretaceous sandstones and(3)primarily continental felsic and lesser ophiolitic mafic-ultramafic source rocks for Cenozoic sandstones.These inferences also imply that the distinct parent rock compositions of the Late Triassic,Upper Cretaceous and Cenozoic aged siliciclastic rock samples reflect their distinct tectonic settings such as the passive rift setting of Late Triassic shales,an SSZ setting for the Upper Cretaceous sandstones and a collisional setting of the Cenozoic sandstones,respectively.展开更多
文摘AIM： To detect distribution and relative frequency of endocrine cells in gastrointestinal tract of flower fish （Pseudophoxinus antalyae）. METHODS： The intestinal tract of flower fish was divided into four portions from proximal to distal; the enlarged area after oesophagus and anterior, middle and posterior intestine. Immunohistochemical method using the peroxidase anti-peroxidase complex was employed. All antisera between four portions of flower fish were compared using ANOVA. RESULTS： Eleven types of gut endocrine cells were determined; they were immunoreactive for calcitonin gene related peptide, substance P, vasoactive intestinal peptide, bombesin, somatostatin-14, secretin, TrkA, TrkB, TrkC, neurotensin, neuropeptide Y, which were found in almost all portions of the gastrointestinal tract. CONCLUSION： The regional frequency of immunoreactive distribution and relative cells in the flower fish, Pseudophoxinus antalyae, are essentially similar to those of other fish.
文摘March 3,2015 Antalya,Turkey An Expert Forum on Disaster Risk Reduction（DRR）in a Changing Climate:Lessons Learned about Lessons Learned,was convened by USAID,CCB/CU,WMO and TSMS with the support of NOAA and GFDRR** in Antalya,Turkey,10 to 13 February 2015.
基金This work was supported by the Scientific and Technological Research Council of Turkey(TÜBİTAK)with a Grant Number of 214O248.
文摘DüzlerçamıWildlife Reserve Area(WRA)is the last natural habitat of fallow deer(Dama dama)in the world.Fallow deer is native to Turkey,however,its geographical range is currently confined to DüzlerçamıWRA,Antalya.To date,a detailed habitat investigation of fallow deer dis-tribution has not been conducted.This study is vital for the last surviving populations of fallow deer in Turkey.There-fore,we studied the habitat suitability and utilization of fal-low deer in the DüzlerçamıWRA.Vegetation and wildlife inventory was surveyed across a total of 304 sample areas between 2015 and 2017.Plant species were recorded accord-ing to the Braun-Blanquet method and wildlife surveys were based on footprints,feces,and other signs of fallow deer.Classification and regression tree techniques,as well as MAXENT,were used to model vegetation and fallow deer habitat.Topographic position index,terrain ruggedness index,roughness index,elevation,and bedrock formation were also calculated and included in the models.Based on our results,we drafted a habitat protection map for fallow deer.To ensure sustainability of habitats where populations of fallow deer are found in Turkey,we developed recommen-dations such as closuring human access of the 1st-degree Protection Area and reintroduction of the species to other potential habitats.
基金funded by the Scientific Research Projects Unit of Suleyman Demirel University(project no.2436-YL-10)(Isparta,Türkiye)。
文摘The Antalya Complex within the Isparta Angle(IA)in the southwest of Türkiye includes various rock types formed in different geodynamic settings and contains important data that shed light on the geodynamic evolution of the Eastern Mediterranean region.In this study,source rocks and tectonic settings of ancient sedimentary basins within the IA have been interpreted using geochemical contents of siliciclastic rocks in different ages.In this regard,whole-rock major,trace and rare earth element(REE)analyses have been conducted on the Cenozoic turbiditic sandstones(from the Eocene Isparta Formation and the Miocene Güneyce Formation in the north of the IA)and integrated with the available data of the Trias sic shales from the east and Upper Cretaceous sandstones from the southwest of the IA.The results indicate that Cenozoic sandstone samples are calcium-rich(CaO,30.54-43.87wt%,average 37.63 wt%),comparable to those of Upper Cretaceous sandstones(CaO,average 24.92 wt%)and Late Triassic(CaO,range between 11.27-26.71 wt%)shales.They demonstrate an excellent carbonate dilution effect on the majority of major oxides.In contrast to the Late Trias sic shales with close affinity to Post-Archean Average Archean Shale(PAAS),Cenozoic and Upper Cretaceous ophiolite-related clastic sediments display strike depletions in Nb-Ta,Th,Rb,Zr and Hf and enrichments in Ni,Co and Cr,suggesting mafic and ultramafic rocks in a source region.Notable enrichments of Cr(average 80.5 ppm),V(average 105.5 ppm),Ni(average 42.3 ppm)and Co(average13.9 ppm)in Late Triassic shales can be attributed to the influences of Triassic OIB-like basaltic rift magmatism in their source regions.In general,their igneous source rocks were derived from mixed sources,e.g.,(1)predominantly continental felsic and lesser rift-related basaltic mafic source rocks for Late Triassic shales,(2)mainly ophiolitic maficultramafic and lesser continental felsic source rocks for Upper Cretaceous sandstones and(3)primarily continental felsic and lesser ophiolitic mafic-ultramafic source rocks for Cenozoic sandstones.These inferences also imply that the distinct parent rock compositions of the Late Triassic,Upper Cretaceous and Cenozoic aged siliciclastic rock samples reflect their distinct tectonic settings such as the passive rift setting of Late Triassic shales,an SSZ setting for the Upper Cretaceous sandstones and a collisional setting of the Cenozoic sandstones,respectively.
