پديد آورندگان :
رضايي, ناصر پژوهشگاه ميراث فرهنگي و گردشگري تهران - گروه ميراث طبيعي , درفشي, خه بات پژوهشگاه ميراث فرهنگي و گردشگري تهران - گروه ميراث طبيعي , اميني, صارم شركت زمين‌ريزكاوان تهران - گروه پژوهشي زمين‌باستان‌شناسي , جهاني, ولي اداره كل ميراث فرهنگي، صنايع دستي و گردشگري استان گيلان
كليدواژه :
ميكرومورفولوژي رسوب‌شناسي , زمين‌باستان‌شناسي , قطعات آهكي , برش رسوبي - باستاني گسكرك , رودبار
چكيده فارسي :
در زمين باستان شناسي با تشخيص و بررسي محتواي رسوبي و چينه نگاري لايه ها و مواد باستان شناسي، مي توان درك كامل و صحيحي از پيشينه هاي باستاني به دست آورد. نوشتار حاضر گزارشي از مطالعات زمين شناختي و رسوب شناختي در محل برش رسوبي - باستاني گسكرك واقع در شهرستان رودبار است كه به منظور بازسازي شرايط محيطي ديرينه انجام گرفته است. برش گسكرك شامل دو لايه رسوب آبرفتي - واريزه اي ريزدانه، با تمايز رنگ مشخص مي باشد كه مرز زيرين آن ها محدود به سنگ بستر رسوبي و مرز بالايي آن ها توسط نهشته هاي استقراري جديدتر پوشيده شده است. رسوبات طبيعي تشكيل دهنده اين دو لايه را ذرات در حد سيلت شامل مي شود كه تراكم بالايي را نشان مي دهد. لايه پاييني (لايه I) عمدتا از رسوبات ريزدانه سيلتي با ناخالصي مواد آهكي تشكيل شده است كه درون آن قطعات آهكي به صورت پراكنده مشاهده مي شود. لايه II كه در مرز بالايي خود توسط نهشته هاي طبيعي فرهنگي عصر مفرغ پوشيده شده است با وجود خرده هاي زغالي مشخص مي شود كه آن را از لايه زيرين خود متمايز مي كند. مطالعه نمونه هاي عهد حاضر شرايط آب و هوايي خشك تا نيمه خشك را براي تشكيل افق هاي كربناتي شده در خاك پيشنهاد مي كند. محتواي كم مواد كربناتي، رنگ قرمز- قهوه اي و همچنين وجود خرده هاي زغالي در لايه II كه متمايز از لايه I مي باشد، شرايط ديرينه محيطي متفاوتي را براي لايه II پيشنهاد مي كند كه به نظر مي رسد با تغيير شرايط آب و هوايي، افزايش بارندگي و رطوبت و گسترش پوشش گياهي جنگلي در منطقه همزمان بوده است.
چكيده لاتين :
IntroductionGeoarchaeology is a new and interdisciplinary concept that studies the past of human history using geological methods. In geoarchaeology, a complete and accurate understanding of ancient records can be obtained by identifying and examining the sedimentary content and stratigraphy of archeological layers and materials. Geology has been available to archaeologists over the past two decades as a basic tool for reconstructing ancient environments and understanding the long-term climatic and anthropogenic conditions and interactions of pre-historic human and surrounding environments. These studies are particularly influential in understanding the Pleistocene and Holocene archaeological and geological backgrounds and materials. Meanwhile, geoarchaeological studies of Iran are practically linked to Paleolithic observations and exploration and the use of geological methods such as sedimentology to describe the details of ancient records in caves and rock shelters. Geoarchaeology is an interdisciplinary specialty between geological sciences and archeology that examines the role of geological factors in the formation, continuation, and weakening of ancient settlements. In this field, techniques and methods common in earth science such as aerial photography and satellite imagery, sampling, microscopic studies, chemical analysis, etc. are used to solve archaeological problems. On the other hand, often referred to as archaeo-geology, archaeological data are used to solve geological problems, particularly in relation to dating of Quaternary deposits, ancient seismological studies, and ancient mining. Large-scale archaeologists study most of the natural landforms and anthropogenic structures and small-scale archaeologists study the soil, natural sediments, and anthropogenic deposits. Archaeo-geology also occasionally covers other interdisciplinary studies such as pottery petrography, ancient mineralogy, ancient metallurgy, dating, etc. and so-called archaeometry.Materials and methodsIn order to determine the frequency of sediment grains based on their size and to investigate the pattern of particle size distribution to determine the textural properties, the sorting of grains and the sedimentary abundances of two natural sediment layers I and II were extracted from Gaskarak section and analyzed by laser particle size analyzer. Organic matter and carbonate bind the sediment particles to each other and therefore, to determine the true distribution of particle size, they must be removed prior to analysis of the samples to separate the sediment particles. The mixing and rotating system of the device will cause the particle to move and be exposed to the laser beam. So after the laser light from a high voltage source is exposed to the sample, the laser beam will reflect from the sample surface and then pass through it. The size of the deposited particles is directly proportional to the magnitude of the reflected laser light and to the angle of refraction of the laser beam to the surface of the particle, so that with increasing diameter of the deposited particles, the intensity of the reflected laser light increases, but its angle of failure decreases.Results and discussionGaskarak section consists of two layers of fine-grained alluvial-debris sediment, with distinct color which their lower boundary is confined to the sedimentary bedrock and their upper boundary is covered by more recent deposits. The natural sediments that form these two layers are silty particles that show high density. The lower layer (I) is mainly composed of silty fine-grained sediments with calcareous fragments. Layer II, covered at its upper bound by the natural and cultural deposits of the Bronze Age is characterized by a charcoal inclination that distinguishes it from its lower layer. Study of the recent samples suggests dry to semi-arid climatic conditions for the formation of carbonated horizons in the soil. Low carbonate content, reddish-brown color, as well as the presence of charcoal fragments in layer II, which is distinct from layer I, suggest a different environmental condition for layer II that seems it has been facing simultaneous climate changes, such as increasing rainfall and humidity and expanding forest vegetation in the region.ConclusionField evidence and results of laboratory studies indicate that the natural deposits of the Gaskarak section probably formed as abnormal sediments on ancient hillslope surfaces of sedimentary bedrock. As the morphology and slope of the sedimentary layers show a valley-like position, the eroded material accumulates from sections with higher topography within it. The natural sediments of the Gaskarak section are distinguished by two distinct layers (I and II) that show distinct differences in color, carbonate content, and mineral and organic fragments.
