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نوسانات آب دریای مازندران از هزارۀ سوم ق.م تا هزارۀ اخیر و تأثیر آن بر پراکنش مراکز استقراری در جنوب شرق دریای مازندران | ||
| پژوهش های جغرافیای طبیعی | ||
| مقاله 3، دوره 47، شماره 1، فروردین 1394، صفحه 37-56 اصل مقاله (1.01 M) | ||
| نوع مقاله: مقاله کامل | ||
| شناسه دیجیتال (DOI): 10.22059/jphgr.2015.53677 | ||
| نویسندگان | ||
| محمد قمری فتیده1؛ حامد وحدتی نسب* 2؛ سید مهدی موسوی2 | ||
| 1استادیار گروه باستان‌شناسی، دانشگاه غیردولتی مارلیک | ||
| 2دانشیار گروه باستان‌شناسی، دانشگاه تربیت مدرس | ||
| چکیده | ||
| دریای مازندران بزرگ‌ترین دریاچۀ روی زمین است و به‌دلیل بسته بودن حوضۀ آبریز، در طول زمان نوسانات زیادی داشته است. از بدو شکل‌گیری این دریا تا کنون، کمینۀ سطح آب آن به 113- متر و بیشینۀ آن به 50+ متر رسیده است. در خلال هر پیش‌روی و پس‌روی، اراضی زیادی از آب خارج شده و منابع جدیدی اضافه شده یا منابعی به زیر آب می‌روند. پس‌روی و پیش‌روی آب دریای مازندران در پژوهش‌های متعددی بررسی شده که بیشتر بر مبنای مطالعه و سن‌سنجی رسوبات مغزه‌های استخراج‌شده و در برخی موارد تلفیق این اطلاعات با دانسته‌های تاریخی است. بر مبنای این یافته‌ها و تلفیق آن با شواهد باستان‌شناختی موجود، اطلاعات پیش رو استخراج شده است. در واقع، در این مقاله با بررسی دقیق مقدار نوسانات آب دریای مازندران از هزارۀ سوم ق.م تا کنون و تلفیق آن با اطلاعات باستان‌شناسی، نشان داده شده که این نوسانات و به‌ویژه آخرین پیش‌روی عمدة دریای مازندران در 1300 میلادی، مهم‌ترین عامل مدفون شدن استقرارگاه‌های انسانی در زیر رسوبات در برخی نواحی جنوب شرق دریای مازندران است. این در حالی است که پیش‌تر، ترک منطقه را مهم‌ترین عامل این خلأ اطلاعاتی می‌پنداشتند. | ||
| کلیدواژه‌ها | ||
| دریای مازندران؛ عصر مفرغ؛ محوطه‌های باستانی؛ نوسانات سطح دریا | ||
| عنوان مقاله [English] | ||
| Fluctuations of Caspian Sea Level and Its Impacts on Distribution of Archaeological Sites in Southeastern Coasts (1st to 3rd Millennium BC) | ||
| نویسندگان [English] | ||
| Mohammad Ghamari Fatideh1؛ Hamed Vahdati Nasab2؛ Seyed Mehdi Mousavi Kouhpar2 | ||
| 1Assistant Professor of Archaeology, Non-governemnt University of Marlik | ||
| 2Associate Professor of Archaeology, Tarbiat Modares University | ||
| چکیده [English] | ||
| Introduction Iranian northern plain is surrounded by the Caspian Sea in North and part of the Alborz Mountains in South. These two geomorphologically distinct features have created unique climatic conditions. A plain lush with abundant rainfall is result of the proximity of these two distinct geographical regions. As a consequence, the Iranian Northern plain has been in use by human populations since the prehistoric times. The significance of coastal regions for human occupations has been documented all over the world. Abundance of food resources, access to the fresh water (rivers), and having clear landmarks have all made the coastal regions ideal geographical zones for human populations. In addition to that, proximity to the major water sources (big lakes, seas, and oceans) would regulate the climatic changes, and prohibits drastic alternations of the environment. Archaeological data have shown that coastal regions have also been used for human movements through prehistoric and historic times. Repeated exodus out of Africa is among such events. Caspian Sea is the largest lake on the earth. Due to its closed drainage basin, Caspian Sea has experienced distinctive fluctuations over time. Paleoclimatic data have shown that the minimum water level of the Caspian Sea was -113 m and the maximum reached +50 m. During each fluctuation episode vast areas have been revealed and large land resources were r concealed. Archaeological Research on the Southeastern Part of the Caspian Sea: The Southeastern areas of the Caspian Sea have witnessed archaeological research since the mid twenty century. Since the time, numerous archaeological surveys and excavations have been conducted at this region. The researches have provided clear understanding of the settlement patterns during many archaeological periods. Among such periods, Bronze Age (3rd millennium B.C. to 500 B.C.) has received the most attention by researchers. It has been proven that the Southeastern areas of the Caspian Sea hosted some of the most well-known Bronze Age archaeological sites of Iran. Among them, Gohar Tepe, Yarim Tepe, Shah Tepe, and Tepe Kelar have experienced several archaeological field missions to reveal tremendous amount of data concerning the socioeconomic structure of the people during the Bronze Age. What did really take place after this period is relatively unknown because the size and type of the archaeological settlements were drastically decreased. Some have claimed migrations to or out of the region and some have even proposed a clear change in the life style due to the apparent shift in the climatic conditions. Climatic data indicates that during the Bronze Age, the Caspian Sea level was more or less stable in was -35 m. The sea level elevated only 1m during a 500 year period. This implies a stable climatic condition. Around 700 AD, the sea level dropped dramatically to -42 m and finally around 1300 AD the region witnessed the largest sea advancement (-22.5m). There is no enough archaeological evidence prior to 1300 A.D. as ever reported from the immediate coastal regions and their adjacent areas at the Southeastern Caspian Sea. For years, many archaeologists interpreted this gap as an evidence of abounding the region because of some unknown causes. Materials and Methods After reviewing the Caspian Sea fluctuations, this paper attempts to reconstruct the coastline at the lowest and highest variability. The lines needed for this study were calculated using topographic maps and hydrographic basin of the Caspian Sea with the help of "National Center for Caspian Studies". After preparation of the GIS maps, the greatest regressions were marked on them. The maps indicate that the coastlines at the beginning of 3000 BC have been situated far behind the contemporary shore lines. Conclusion By combining the climatic and archaeological data, this research has shown that in contrast to the former claims concerning the absence of archaeological settlements at the Southeastern the Caspian Sea, majority of archaeological settlements have been buried under the sediments left by the periodic fluctuations of the Caspian Sea. Among these flactuations, the 1300 A.D. advancement has had the most effective. The Purpose of this research is that all archaeological surveys at the mentioned region must take the sea fluctuations into account prior to the actual field work. | ||
| کلیدواژه‌ها [English] | ||
| archaeological sites, Bronze Age, Caspian Sea, sea level fluctuations | ||
| مراجع | ||
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