Objective:To identify Leishman{u using PCR.Methods:This studs was conducted from April2009 to March 2011 in order to identify Leishmania species in a new endemic area of CL in Lorestan.Iran.Samples were taken from 62 ...Objective:To identify Leishman{u using PCR.Methods:This studs was conducted from April2009 to March 2011 in order to identify Leishmania species in a new endemic area of CL in Lorestan.Iran.Samples were taken from 62 patients that referred to the health centers in different cities of Lorestan province,the presence of Leishmcania was confirmed using direct smear and then grown in NNN media and mass cultured in RPM!1640 medium supplemented with 10%heat-inactivated fetal bovine serum.DNA was extracted from cultured promastigotes and used in P15-PCR.Results:45(72.6%)samples out of 62 showed a hand in the range of 485 hp and 17(27.4%)with a hand in the range of 626 hp which were similar to standard strains of Leichmania tropica(L.tropical and Leishnrania major(L.major),respectively.50(65.80%)of samples were collected from people with no history of travel in at least a year prior to the onset which shows that indigenous source of infection.Conclusions:Since the vector and reservoir of the two species are different.so precise and extensive control and prevention methods should be designed and earned out.展开更多
In recent year,desertification has become one of the most important environmental hazards all over the world,especially in developing countries such as Iran.Understanding the factors impacting on desertification and i...In recent year,desertification has become one of the most important environmental hazards all over the world,especially in developing countries such as Iran.Understanding the factors impacting on desertification and identifying the regions with high desertification potential are essential to control this phenomenon(i.e.,desertification).The life cycle assessment(LCA)method is essential in assessing the desertification of ecosystems,especially for susceptible ecosystems with high degradation risks.The aim of the present study was to evaluate the desertification potential of Lorestan Province,Iran,based on the LCA method.We selected aridity,fire and dust as three indicators of desertification and collected data from 2000 to 2015.We divided the study area into 6 types of ecoregions according to the climate types(arid,semi-arid and dry sub-humid)and dominant species(Quercus brantii and Astragalus adscendens),and calculated the characteristic factor(CF)of each indicator(aridity,fire and dust)by combining the indicator layers and ecoregion layer of the study area.In a given ecoregion,the sum of CF values of aridity,dust and fire indicators represents the life cycle inventory(LCI)desertification value(the higher the LCI value,the greater the desertification potential).Then,we obtained the desertification potential map by combining and overlapping the ecoregions and the normalized indicators based on the LCA method.Aridity and fire exhibit significant impacts on desertification in the study area compared with dust.In the study area,semi-arid ecoregion with Quercus brantii as the dominant species is the largest ecoregion,while arid ecoregion with Quercus brantii as the dominant species is the smallest ecoregion.Arid ecoregion with Astragalus adscendens as the dominant species(LCI desertification value of 1.99)and dry sub-humid ecoregion with Quercus brantii as the dominant species(LCI desertification value of 0.79)show the highest and lowest desertification potentials,respectively.Furthermore,arid ecoregion with Quercus brantii as the dominant species also has a higher LCI desertification value(1.89),showing a high desertification potential.These results suggest the necessity of proper management and appropriate utilization in these ecoregions.In general,assessing desertification potential using the LCA method on a local and regional scale can possibly provide a new methodology for identifying and protecting areas with high degradation risks.展开更多
In this paper, Biostratigraphy of Asmari formation to San oligo-Myocene was studied in North Mamulan, South West Lorestan Province. In this region, Shahbazan-Asmari carbonate formation is located between Kashkan forma...In this paper, Biostratigraphy of Asmari formation to San oligo-Myocene was studied in North Mamulan, South West Lorestan Province. In this region, Shahbazan-Asmari carbonate formation is located between Kashkan formation beneath and evaporative formation of Gachsaran as old as lower Miocene in the form of disconformity above. From 180 m real thickness observed in this study, 23 genera and 15 species of benthic foraminifera were identified and studied. These foraminifera were found in four assemblage zones suggesting that this formation dates back to Oligocene (Chattian-Rupelian) and early Miocene (Aquitanian-Burdigalian). Moreover, based on microscopic studies and visual observations, nine microfacies were identified that were deposited in three zones: lagoon, dam, and shallow open marine.展开更多
The Shahbazan Formation was deposited in the foreland basin in southwestern Iran( Lorestan Basin). In this research,microbiostratigraphy and depositional environmental implications related to the Shahbazan Formation a...The Shahbazan Formation was deposited in the foreland basin in southwestern Iran( Lorestan Basin). In this research,microbiostratigraphy and depositional environmental implications related to the Shahbazan Formation at the northern flank of Chenaerh anticline are discussed. Carbonate sequences of the Shahbazan Formation consist mainly of large benthic foraminifera along with other skeletal and non-skeletal components.Two biozones have been recognized by distribution of large foraminifera in the studied area that indicate middle Eocene age( Lutetian). Based on analysis of large benthic foraminiferal assemblages and microfacies features,7 different microfacies have been recognized,which can be grouped into three depositional environments: inner,middle and outer ramps.展开更多
基金funded by a grant from Lorestan University of Medical Sciences (11/19/2008No.1121)
文摘Objective:To identify Leishman{u using PCR.Methods:This studs was conducted from April2009 to March 2011 in order to identify Leishmania species in a new endemic area of CL in Lorestan.Iran.Samples were taken from 62 patients that referred to the health centers in different cities of Lorestan province,the presence of Leishmcania was confirmed using direct smear and then grown in NNN media and mass cultured in RPM!1640 medium supplemented with 10%heat-inactivated fetal bovine serum.DNA was extracted from cultured promastigotes and used in P15-PCR.Results:45(72.6%)samples out of 62 showed a hand in the range of 485 hp and 17(27.4%)with a hand in the range of 626 hp which were similar to standard strains of Leichmania tropica(L.tropical and Leishnrania major(L.major),respectively.50(65.80%)of samples were collected from people with no history of travel in at least a year prior to the onset which shows that indigenous source of infection.Conclusions:Since the vector and reservoir of the two species are different.so precise and extensive control and prevention methods should be designed and earned out.
文摘In recent year,desertification has become one of the most important environmental hazards all over the world,especially in developing countries such as Iran.Understanding the factors impacting on desertification and identifying the regions with high desertification potential are essential to control this phenomenon(i.e.,desertification).The life cycle assessment(LCA)method is essential in assessing the desertification of ecosystems,especially for susceptible ecosystems with high degradation risks.The aim of the present study was to evaluate the desertification potential of Lorestan Province,Iran,based on the LCA method.We selected aridity,fire and dust as three indicators of desertification and collected data from 2000 to 2015.We divided the study area into 6 types of ecoregions according to the climate types(arid,semi-arid and dry sub-humid)and dominant species(Quercus brantii and Astragalus adscendens),and calculated the characteristic factor(CF)of each indicator(aridity,fire and dust)by combining the indicator layers and ecoregion layer of the study area.In a given ecoregion,the sum of CF values of aridity,dust and fire indicators represents the life cycle inventory(LCI)desertification value(the higher the LCI value,the greater the desertification potential).Then,we obtained the desertification potential map by combining and overlapping the ecoregions and the normalized indicators based on the LCA method.Aridity and fire exhibit significant impacts on desertification in the study area compared with dust.In the study area,semi-arid ecoregion with Quercus brantii as the dominant species is the largest ecoregion,while arid ecoregion with Quercus brantii as the dominant species is the smallest ecoregion.Arid ecoregion with Astragalus adscendens as the dominant species(LCI desertification value of 1.99)and dry sub-humid ecoregion with Quercus brantii as the dominant species(LCI desertification value of 0.79)show the highest and lowest desertification potentials,respectively.Furthermore,arid ecoregion with Quercus brantii as the dominant species also has a higher LCI desertification value(1.89),showing a high desertification potential.These results suggest the necessity of proper management and appropriate utilization in these ecoregions.In general,assessing desertification potential using the LCA method on a local and regional scale can possibly provide a new methodology for identifying and protecting areas with high degradation risks.
文摘In this paper, Biostratigraphy of Asmari formation to San oligo-Myocene was studied in North Mamulan, South West Lorestan Province. In this region, Shahbazan-Asmari carbonate formation is located between Kashkan formation beneath and evaporative formation of Gachsaran as old as lower Miocene in the form of disconformity above. From 180 m real thickness observed in this study, 23 genera and 15 species of benthic foraminifera were identified and studied. These foraminifera were found in four assemblage zones suggesting that this formation dates back to Oligocene (Chattian-Rupelian) and early Miocene (Aquitanian-Burdigalian). Moreover, based on microscopic studies and visual observations, nine microfacies were identified that were deposited in three zones: lagoon, dam, and shallow open marine.
文摘The Shahbazan Formation was deposited in the foreland basin in southwestern Iran( Lorestan Basin). In this research,microbiostratigraphy and depositional environmental implications related to the Shahbazan Formation at the northern flank of Chenaerh anticline are discussed. Carbonate sequences of the Shahbazan Formation consist mainly of large benthic foraminifera along with other skeletal and non-skeletal components.Two biozones have been recognized by distribution of large foraminifera in the studied area that indicate middle Eocene age( Lutetian). Based on analysis of large benthic foraminiferal assemblages and microfacies features,7 different microfacies have been recognized,which can be grouped into three depositional environments: inner,middle and outer ramps.
