A. Khosravichenar, M. Fattahi, A. Karimi, Hassan Fazeli Nashli, H. von Suchodoletz
{"title":"A first outline of the Quaternary landscape evolution of the Kashaf Rud River basin in the drylands of northeastern Iran","authors":"A. Khosravichenar, M. Fattahi, A. Karimi, Hassan Fazeli Nashli, H. von Suchodoletz","doi":"10.5194/EGQSJ-70-145-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-145-2021","url":null,"abstract":"Azra Khosravichenar1,2, Morteza Fattahi3, Alireza Karimi4, Hassan Fazeli Nashli5, and Hans von Suchodoletz2 1Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, 04103 Leipzig, Germany 2Department of Geography, Leipzig University, 04103 Leipzig, Germany 3Institute of Geophysics, University of Tehran, Tehran 14155-6466, Iran 4Department of Soil Science, Faculty of Agriculture, Ferdowsi University of Mashhad, Mashhad 917794-8974, Iran 5Department of Archaeology, University of Tehran, Tehran 14155-6466, Iran","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"112 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-06-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123535023","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Sandhills, sandbanks, waterways, canals and sacred lakes at Sais in the Nile Delta","authors":"P. Wilson, H. Ghazala","doi":"10.5194/EGQSJ-70-129-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-129-2021","url":null,"abstract":"Abstract. The paper explores the relationship between the archaeological zones of the ancient city of Sais at Sa el-Hagar, Egypt, and the natural landscape of the western central Nile Delta and, in particular,\u0000the extent to which the dynamic form of the landscape was an element in the\u0000choice of settlement location. Furthermore, settlement at Sais has been\u0000determined to have existed at several locations in the immediate environs of the current archaeological zones from the Neolithic period, around 4000 BCE (Before Common Era),\u0000to the modern day, suggesting that the local environment was conducive to\u0000sustainable settlement, culminating in the establishment of a capital city\u0000in the 7th century BCE. The nature of the settlement, its immediate environs and waterway systems will, thus, be described, based on correlation of geological, geophysical, remote sensing and archaeological data, in order to establish if and when human interactions in the landscape can be determined to be reactive or proactive.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"56 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-05-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122578364","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
J. García, C. Lüthgens, Rodrigo Vega, Á. Rodés, A. Hein, S. Binnie
{"title":"A composite 10Be, IR-50 and 14C chronology of the pre-Last Glacial Maximum (LGM) full ice extent of the western Patagonian Ice Sheet on the Isla de Chiloé, south Chile (42° S)","authors":"J. García, C. Lüthgens, Rodrigo Vega, Á. Rodés, A. Hein, S. Binnie","doi":"10.5194/EGQSJ-70-105-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-105-2021","url":null,"abstract":"Abstract. Unanswered questions about the glacier and climate history preceding the\u0000global Last Glacial Maximum (LGM) in the southern temperate latitudes\u0000remain. The Marine Isotope Stage (MIS) 3 is normally understood as a global\u0000interstadial period; nonetheless its climate was punctuated by conspicuous\u0000variability, and its signature has not been resolved beyond the polar realms. In this paper, we compile a 10Be depth profile, single grain infrared (IR) stimulated luminescence dating and 14C samples to derive a new glacier record for the principal outwash plain complex, deposited by the western Patagonian Ice Sheet (PIS) during the last glacial period (Llanquihue Glaciation) on the Isla de Chiloe, southern Chile (42 ∘ S). In this region, the Golfo de Corcovado Ice Lobe\u0000left a distinct geomorphic and stratigraphic imprint, suitable for\u0000reconstructing former ice dynamics and timing of past climate change. Our data\u0000indicate that maximum glaciation occurred by 57.8±4.7 ka without\u0000reaching the Pacific Ocean coast. Ice readavanced and buttressed against the\u0000eastern side of the Cordillera de la Costa again by 26.0±2.9 ka. Our\u0000data further support the notion of a large ice extent during parts of the MIS 3 in Patagonia and New Zealand but appear to contradict near contemporaneous\u0000interstadial evidence in the southern midlatitudes, including\u0000Chiloe. We propose that the PIS expanded to its full-glacial Llanquihue\u0000moraines, recording a rapid response of southern mountain glaciers to the\u0000millennial-scale climate stadials that punctuated the MIS 3 at the poles and elsewhere.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"16 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131996776","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Significant depositional changes offshore the Nile Delta in late third millennium BCE: relevance for Egyptology","authors":"J. Stanley, Sarah E. Wedl","doi":"10.5194/EGQSJ-70-83-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-83-2021","url":null,"abstract":"Abstract. No environmental factor has been as critically important for Egypt's ancient society through time as sufficiently high annual flood levels of the Nile River, the country's major source of fresh water. However, interpretation of core analysis shows reduced depositional accumulation rates and altered compositional attributes of the sediment facies deposited seaward of the Nile Delta during a relatively brief period in the late third millennium BCE. These changes record the effects of displaced climatic belts, decreased rainfall, lower Nile flows, and modified oceanographic conditions offshore in the Levantine Basin, primarily from 2300 to 2000 BCE, taking place at the same time as important geological changes identified by study of cores collected in the Nile Delta. It turns out that integrated multi-disciplinary Earth science and archaeological approaches at dated sites serve to further determine when and how such significant changing environmental events had negative effects in both offshore and landward areas. This study indicates these major climatically induced effects prevailed\u0000concurrently offshore and in Nile Delta sites and at about the time Egypt\u0000abandoned the Old Kingdom's former political system and also experienced\u0000fragmentation of its centralized state. In response, the country's\u0000population would have experienced diminished agricultural production leading to altered societal, political, and economic pressures during the late Old Kingdom to First Intermediate Period at ca. 2200 to 2050 BCE.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"6 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-02-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122842959","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Implications of geoarchaeological investigations for the contextualization of sacred landscapes in the Nile Delta","authors":"Eva Lange-Athinodorou","doi":"10.5194/EGQSJ-70-73-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-73-2021","url":null,"abstract":"Abstract. Key elements of sacred landscapes of the Nile Delta were\u0000lakes, canals and artificial basins connected to temples, which were built\u0000on elevated terrain. In the case of temples of goddesses of an ambivalent,\u0000even dangerous, nature, i.e. lioness goddesses and all female deities who\u0000could appear as such, the purpose of sacred lakes and canals exceeded their\u0000function as a water resource for basic practical and religious needs. Their\u0000pleasing coolness was believed to calm the goddess' fiery nature, and during\u0000important religious festivals, the barques of the goddesses were rowed on\u0000those waters. As archaeological evidence was very rare in the past, the\u0000study of those sacred waters was mainly confined to textual sources.\u0000Recently applied geoarchaeological methods, however, have changed this\u0000situation dramatically: they allow in-depth investigations and\u0000reconstructions of these deltaic sacred landscapes. Exploring these newly\u0000available data, the paper presented here focuses on the sites of Buto, Sais\u0000and Bubastis, by investigating the characteristics of their sacred lakes,\u0000canals and marshes with respect to their hydrogeographical and\u0000geomorphological context and to their role in ancient Egyptian religion and\u0000mythology as well.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"41 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-02-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122258364","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Western Mareotis lake(s) during the Late Holocene (4th century BCE–8th century CE): diachronic evolution in the western margin of the Nile Delta and evidence for the digging of a canal complex during the early Roman period","authors":"Mael Crépy, Marion Boussac","doi":"10.5194/EGQSJ-70-39-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-39-2021","url":null,"abstract":"Abstract. Lake Mareotis (modern Mariut), located near the Mediterranean\u0000coast of Egypt west of the Nile Delta, is bordered by ancient sites dating\u0000from the New Kingdom (end of the 2nd millennium BCE) to the Medieval period (8th\u0000century CE), the most famous one being Alexandria. In its western part (wadi\u0000Mariut), several sites are equipped with harbour structures, but they also have\u0000structures contemporaneous with them that are not compatible with the lake\u0000level required for the operation of the harbour. Between the 1990s and 2010,\u0000several sedimentological studies tried to solve this paradox without\u0000completely succeeding. To go further, this study is based on the reassessment\u0000of geoarchaeological data and on the analysis of early scholars' accounts\u0000(1800–1945), maps (1807–1958) and satellite photographs (Corona). It\u0000allows us to reconstruct the extension of the lake(s) at different periods in\u0000wadi Mariut. During the 1st millennium BCE, the Mariut lagoon experienced a\u0000drawdown in its western part, and several distinct lakes formed, followed by\u0000building operations in some emerged areas during the Hellenistic period\u0000(332–30 BCE). During the early Roman period (30 BCE–284 CE), the digging\u0000of several canals in the 2nd century CE to connect the sites of the wadi Mariut\u0000to the eastern part of the Mariut basin reconfigured the lake(s).","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"150 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-01-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128421336","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Moritz Nykamp, Jacob Hardt, P. Hoelzmann, J. May, T. Reimann
{"title":"Towards timing and stratigraphy of the Bronze Age burial mound royal tomb (Königsgrab) of Seddin (Brandenburg, northeastern Germany)","authors":"Moritz Nykamp, Jacob Hardt, P. Hoelzmann, J. May, T. Reimann","doi":"10.5194/EGQSJ-70-1-2021","DOIUrl":"https://doi.org/10.5194/EGQSJ-70-1-2021","url":null,"abstract":"Abstract. This study uses an integrated multi-method\u0000geoarcheological and geochronological approach to contribute to the\u0000understanding of the timing and stratigraphy of the monumental burial mound royal tomb (Konigsgrab) of Seddin. We show that the hitherto\u0000established radiocarbon-based terminus post quem time frame for the\u0000construction of the burial mound of 910–800 BCE is supported by optically\u0000stimulated luminescence (OSL) dating. The radiocarbon samples were obtained\u0000from a substrate directly underneath the burial mound which supposedly\u0000represents the late glacial/Holocene soil that was buried below the\u0000structure. We use sedimentological (grain-size analyses) and geochemical\u0000analyses (element analyses, carbon, pH, and electric conductivity\u0000determinations) to reassess and confirm this hypothesis. In addition to the\u0000burial age associated with the last anthropogenic reworking during\u0000construction of the burial mound, the OSL dating results provide new\u0000insights into the primary deposition history of the original substrates used\u0000for the structure. In combination with regional information about the middle\u0000and late Quaternary development of the environment, our data allow us to\u0000provide a synoptic genetic model of the landscape development and the\u0000multiphase stratigraphy of the royal tomb of Seddin within the Late Bronze\u0000Age cultural group “Seddiner Gruppe” of northern Germany. Based on our\u0000initial experiences with OSL dating applied to the sediments of a burial\u0000mound – to the best of our knowledge the first attempt in Europe – we\u0000propose a minimal invasive approach to obtain datable material from burial\u0000mounds and discuss related opportunities and challenges.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"21 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-01-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131101865","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Editorial: E&G Quaternary Science Journal – almost 70 years and going stronger than ever","authors":"C. Lüthgens, D. Sauer, M. Zech","doi":"10.5194/egqsj-69-261-2021","DOIUrl":"https://doi.org/10.5194/egqsj-69-261-2021","url":null,"abstract":"<jats:p>\u0000 </jats:p>","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"57 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2021-01-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125841955","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
T. Ullmann, Leon Nill, R. Schiestl, Julian Trappe, Eva Lange-Athinodorou, R. Baumhauer, J. Meister
{"title":"Mapping buried paleogeographical features of the Nile Delta (Egypt) using the Landsat archive","authors":"T. Ullmann, Leon Nill, R. Schiestl, Julian Trappe, Eva Lange-Athinodorou, R. Baumhauer, J. Meister","doi":"10.5194/egqsj-69-225-2020","DOIUrl":"https://doi.org/10.5194/egqsj-69-225-2020","url":null,"abstract":"Abstract. The contribution highlights the use of Landsat spectral-temporal metrics (STMs) for the detection of surface anomalies that are potentially related to buried near-surface paleogeomorphological deposits in the Nile Delta (Egypt), in particular for a buried river branch close to Buto. The processing was completed in the Google Earth Engine (GEE) for the entire Nile Delta and for selected seasons of the year (summer/winter) using Landsat data from 1985 to 2019. We derived the STMs of the tasseled cap transformation (TC), the Normalized Difference Wetness Index (NDWI), and the Normalized Difference Vegetation Index (NDVI). These features were compared to historical topographic maps of the Survey of Egypt, CORONA imagery, the digital elevation model of the TanDEM-X mission, and modern high-resolution satellite imagery. The results suggest that the extent of channels is best revealed when differencing the median NDWI between summer (July/August) and winter (January/February) seasons ( ΔNDWI ). The observed difference is likely due to lower soil/plant moisture during summer, which is potentially caused by coarser-grained deposits and the morphology of the former levee. Similar anomalies were found in the immediate surroundings of several Pleistocene sand hills (“geziras”) and settlement mounds (“tells”) of the eastern delta, which allowed some mapping of the potential near-surface continuation. Such anomalies were not observed for the surroundings of tells of the western Nile Delta. Additional linear and\u0000meandering ΔNDWI anomalies were found in the eastern Nile Delta in the immediate surroundings of the ancient site of Bubastis (Tell Basta), as well as several kilometers north of Zagazig. These anomalies might indicate former courses of Nile river branches. However, the ΔNDWI does not provide an unambiguous delineation.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"87 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2020-12-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132138822","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Kerstin Pasda, M. L. Correa, P. Stojakowits, Bernhard Häck, J. Prieto, Najat al-Fudhaili, C. Mayr
{"title":"Cave finds indicate elk (Alces alces) hunting during the Late Iron Age in the Bavarian Alps","authors":"Kerstin Pasda, M. L. Correa, P. Stojakowits, Bernhard Häck, J. Prieto, Najat al-Fudhaili, C. Mayr","doi":"10.5194/egqsj-69-187-2020","DOIUrl":"https://doi.org/10.5194/egqsj-69-187-2020","url":null,"abstract":"Abstract. The finding of a partially preserved elk skeleton from the Bavarian Alps is reported. Remnants of an adult male were found, together with skeletal elements of juvenile moose calves, at the base of a talus cone in the pit cave Stiefelschacht, next to Lenggries (southern Germany). The adult's bones exhibited anthropogenic traces like cut marks and were radiocarbon-dated to the Late Iron Age. A projectile hole in the left\u0000shoulder blade and cut marks on the bones are indicative of hunting and\u0000meat usage. The elk remains were associated with several wild and domestic\u0000species such as ungulates and hare but were not, however, accompanied by\u0000archaeological artefacts. Other archaeological sites of the Late Iron Age\u0000are so far not known within a distance of less than 30 km to the\u0000Stiefelschacht. While the presence of elk during prehistoric times in the\u0000Alps has already been known before, the finds and the\u0000location are unique in that they are the first evidence of elk hunting\u0000during the Late Iron Age in the northern Alps.","PeriodicalId":227489,"journal":{"name":"EG Quaternary Science Journal","volume":"71 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2020-10-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125633528","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}