首页> 外文期刊>Journal of Science and Technology of Agriculture and Natural Resources >Evidences of Climate Change Recorded in Quaternary Paleosols from Isfahan and Emam-Gheis (Chaharmahal & Bakhtiary)
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Evidences of Climate Change Recorded in Quaternary Paleosols from Isfahan and Emam-Gheis (Chaharmahal & Bakhtiary)

机译:伊斯法罕和伊玛目-盖伊斯(Chaharmahal&Bakhtiary)的第四纪古土壤记录的气候变化证据

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Investigation of paleosols plays a great role in paleoecological and paleoclimatological studies. They are also important in soil survey and planning, as they exhibit characteristics different from younger soils. Paleosols are those soils which formed under conditions different from present ones, and are either buried within sedimentary sequences or those which lie on persisting surfaces. Although such soils are widespread in central Iran and Zagros Zone, they have not been studied adequately. Paleosols are identified by different parameters such as morphological, physical, chemical, mineralogical, and micromorphological characteristics. In this study, morphological, physical, and chemical properties of three paleosols from Isfahan and Chaharmahal & Bakhtiary provinces were investigated. The profiles were on different landforms including alluvial fan, dissected old plain, and old lagoonal deposits. Soil profile in Segzi site, on old lagoonal deposits, had a very dark and thick layer at a depth of 45-60 cm containing some macrofossil shells. This shows that this area was covered by brackish water during the early Holocene. In Sepahanshahr profile, presence of strong clay coating and high concentrations of CaCO3 indicates a wetter environment in the past than the present conditions with a precipitation of only 100 mm. In Emam-Gheis profile, a buried paleosol was identified with strong clay coating and free CaCO3 horizons that shows more humid conditions. Evidences obtained from the three paleosols studied indicate that effective moisture in central Iran and Zagros regions during Late Pleistocene had been higher than its present levels. Keywords: Paleosols, Macrofossil, Pleistocence, Physical and chemical properties. Full-Text Type of Study: Research | Subject: Ggeneral Received: 2008/01/9 Related Websites Scientific Publications Commission - Health Ministry Scientific Publications Commission - Science Ministry Yektaweb Company Site Keywords ?????, Academic Journal, Scientific Article, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ????? ??, ???? ?? Vote ? 2015 All Rights Reserved | JWSS - Isfahan University of Technology
机译:古土壤研究在古生态学和古气候学研究中起着重要作用。它们在土壤调查和规划中也很重要,因为它们具有不同于年轻土壤的特征。古土壤是在不同于当前土壤条件下形成的土壤,或者被埋在沉积层序中,或者被埋藏在持久的表面上。尽管这类土壤在伊朗中部和扎格罗斯地区普遍分布,但尚未对其进行充分研究。古土壤通过不同的参数进行识别,例如形态,物理,化学,矿物学和微观形态特征。在这项研究中,调查了伊斯法罕省,恰哈马哈尔省和巴赫克蒂州的三种古土壤的形态,物理和化学性质。剖面位于不同的地形上,包括冲积扇,解剖的旧平原和旧的泻湖沉积物。在旧泻湖沉积物上的塞格齐(Segzi)遗址上,土壤剖面在45-60厘米深处有一个非常深色且厚实的层,其中含有一些大化石壳。这表明,在全新世早期,该地区被微咸水覆盖。在Sepahanshahr剖面中,存在坚固的粘土涂层和高浓度的CaCO3,表明过去的环境比现在的条件更湿润,只有100 mm的降水。在Emam-Gheis剖面中,发现了一个埋有古土壤的土壤,该土壤具有坚固的粘土涂层和自由的CaCO3层,显示出更多的潮湿条件。从所研究的三种古土壤获得的证据表明,晚更新世期间伊朗中部和扎格罗斯地区的有效水分高于当前水平。关键词:古土壤,大型化石,更新世,理化性质。全文研究类型:研究|主题:一般收稿日期:2008/01/9相关网站科学出版物委员会-卫生部科学出版物委员会-科学部Yektaweb公司网站关键字??????,Academic Journal,Scientific Article,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ?????? ??,???? ??投票吗? 2015版权所有| JWSS-伊斯法罕工业大学

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