- I am currently working at the Institute of Geography and Geology, University of Würzburg, as a Junior Professor for Geoarchaeology and Quaternary Science.edit
In ancient Egypt, lakes, canals, and other water bodies were an essential part of the sacred landscape in which temples were embedded. In recent years, geoarchaeological research at the site of the Temple of Bastet at Bubastis in the... more
In ancient Egypt, lakes, canals, and other water bodies were an essential part of the sacred landscape in which temples were embedded. In recent years, geoarchaeological research at the site of the Temple of Bastet at Bubastis in the southeastern Nile Delta has proven the existence of two water canals surrounding the temple. It has now been investigated whether these canals were connected to the Temple of Pepi I (2300 – 2250 B.C.E.), located approximately 100 m to the west of theTemple of
Bastet. To explore the Holocene landscape genesis of the Temple of Pepi I, 15 drillings and six geoelectrical profile lines were performed in the surroundings of the temple in spring 2022. The results show loamy to clayey sediments in deeper sections of all drillings with a maximum thickness of 1.70 m, indicating a marshy or swampy depositional environment. Based on the recovered sediment sequences and
archaeological remains in the vicinity of the Temple of Pepi I, the marshy or swampy area existed before the Fourth Dynasty. During the Old Kingdom (ca. 2850 – 2180 B.C.E.), the former marshland either dried up through natural processes or was intentionally drained and filled with sediments for subsequent use for occupation. Regarding the original research question, there is as yet no evidence for a direct connection to the canals of the Temple of Bastet.
Bastet. To explore the Holocene landscape genesis of the Temple of Pepi I, 15 drillings and six geoelectrical profile lines were performed in the surroundings of the temple in spring 2022. The results show loamy to clayey sediments in deeper sections of all drillings with a maximum thickness of 1.70 m, indicating a marshy or swampy depositional environment. Based on the recovered sediment sequences and
archaeological remains in the vicinity of the Temple of Pepi I, the marshy or swampy area existed before the Fourth Dynasty. During the Old Kingdom (ca. 2850 – 2180 B.C.E.), the former marshland either dried up through natural processes or was intentionally drained and filled with sediments for subsequent use for occupation. Regarding the original research question, there is as yet no evidence for a direct connection to the canals of the Temple of Bastet.
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Collection of conference abstracts presented at the vDEUQUA2021 (2021-09-30 to 2021-09-01), the virtual meeting of the German Quaternary Association (DEUQUA).
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This study investigates the surroundings of Munigua (municipium Flavium Muniguense), a small Roman town in the ancient province of Hispania Baetica (SW Spain). The city's economy was based primarily on copper and iron mining, which... more
This study investigates the surroundings of Munigua (municipium Flavium Muniguense), a small Roman town in the ancient province of Hispania Baetica (SW Spain). The city's economy was based primarily on copper and iron mining, which brought financial prosperity to its citizens. Local production of agricultural goods is thought to have been of little importance, as the regional soil conditions do not seem to be suitable for extensive agriculture.
The German Society for Geomorphology (GSG) (Deutsche Gesellschaft für Geomorphologie: DGGM) evolved out of the German Working Group for Geomorphology in 2021, reflecting the widened scope of relevant topics and involved disci-The German... more
The German Society for Geomorphology (GSG) (Deutsche Gesellschaft für Geomorphologie: DGGM) evolved out of the German Working Group for Geomorphology in 2021, reflecting the widened scope of relevant topics and involved disci-The German Working Group for Geomorphology (GWGG) (Deutscher Arbeitskreis für Geomorphologie) started 1974 with its first annual meeting: 'Relief generations in different climates', hosted by Julius Büdel in Würzburg. The GWGG has since then organized annual national and international conferences (programmes are accessible at https://www.ak-geomorphologie.de/?lang=en) and has been presided
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A complex and sustainable watershed management strategy was implemented in Sri Lanka during the ancient Anuradhapura period, from the 5th century BC to the 11th century AD. Like modern watershed management strategies, it focused on flood... more
A complex and sustainable watershed management strategy was implemented in Sri Lanka during the ancient Anuradhapura period, from the 5th century BC to the 11th century AD. Like modern watershed management strategies, it focused on flood prevention, soil erosion control, water quality control and water storage for irrigation. Tank cascade systems were the key element of these ancient watershed management installations. The wewas investigated were constructed in valleys characterised by fluvial accumulation. Sedimentological analyses of these tank cascade systems show that a precise age determination and the reconstruction of sediment and water f luxes as triggered by human-environment interactions are difficult. This is caused by the shallow character of the wewas leading to the steady redeposition of the tank sediments by wave motions during the wet season and agricultural use of the desiccated wewas during the dry season. Beyond, the sediments analysed allow to distinguish between...
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In this study, we investigated the stability and reactivation of preexisting Tonghua landslide deposits in China, including the adjacent stable slope. We used an integrated approach, combining a multichannel analysis of surface waves... more
In this study, we investigated the stability and reactivation of preexisting Tonghua landslide deposits in China, including the adjacent stable slope. We used an integrated approach, combining a multichannel analysis of surface waves (MASW) and electrical resistivity tomography (ERT). We used ERT to determine groundwater seepage paths, weathering conditions, water content, and the depth to bedrock. High-resolution two-dimensional (2D) shear-wave velocity MASW images, on the other hand, played an essential role in detecting both horizontal and vertical compositions, disjointedness, and sliding surfaces related to lithological borders. Based on seismic models, we considered four geological layers encountered in the stable slope, including fractured (gravel) and weathered (phyllite) materials, as a sliding mass. We combined the 2D resistivity profiles obtained to create pseudo-three-dimensional ERT images to estimate water-saturated and unsaturated masses. From the tomography results, we identified different preexisting deposits, including buried arable clay deposits, old accumulated earthflow deposits, a water accumulation zone, and a fissure runoff. Based on the resistivity results, the bottom of the earthflow deposits is susceptible to water, and oversaturation can reactivate the earthflow.
Within the Spessart low mountain range in central Germany, numerous castle ruins of the 13th century CE exist. Their construction and destruction were often deter- mined by the struggle for political and economic supremacy in the region... more
Within the Spessart low mountain range in central Germany, numerous castle ruins
of the 13th century CE exist. Their construction and destruction were often deter-
mined by the struggle for political and economic supremacy in the region and for
control over the Spessart ’ s natural resources. Wahlmich Castle is located in a rela-
tively uncommon strategic and geomorphological position, characterized by a fairly
remote position and atypical rough relief. In order to reconstruct the local relief
development and possible human impact, a multi-method approach was applied com-
bining two-dimensional geoelectrical measurements, geomorphological mapping and
stratigraphic-sedimentological investigations. This provides new insights into the
influence of landscape characteristics on choices of castle locations.
The combined geoelectrical, geomorphological and stratigraphic-sedimentological
data show that the rough relief is of natural origin and influenced by regional faulting,
which triggered sliding and slumping as well as weathering and dissection of the sur-
face deposits. The rough relief and the lithology permitted intensive land use and
building activities. However, the location of the castle offered access to and possibly
control over important medieval traffic routes and also represented certain owner-
ship claims in the Aschaff River valley.
The economic situation combined with rivalry between different elites led to the cas-
tle being built in a geomorphological challenging and strategically less valuable loca-
tion. Focusing on castles located in rare and challenging geomorphological positions
may therefore lead to a better understanding of castle siting in the future.
of the 13th century CE exist. Their construction and destruction were often deter-
mined by the struggle for political and economic supremacy in the region and for
control over the Spessart ’ s natural resources. Wahlmich Castle is located in a rela-
tively uncommon strategic and geomorphological position, characterized by a fairly
remote position and atypical rough relief. In order to reconstruct the local relief
development and possible human impact, a multi-method approach was applied com-
bining two-dimensional geoelectrical measurements, geomorphological mapping and
stratigraphic-sedimentological investigations. This provides new insights into the
influence of landscape characteristics on choices of castle locations.
The combined geoelectrical, geomorphological and stratigraphic-sedimentological
data show that the rough relief is of natural origin and influenced by regional faulting,
which triggered sliding and slumping as well as weathering and dissection of the sur-
face deposits. The rough relief and the lithology permitted intensive land use and
building activities. However, the location of the castle offered access to and possibly
control over important medieval traffic routes and also represented certain owner-
ship claims in the Aschaff River valley.
The economic situation combined with rivalry between different elites led to the cas-
tle being built in a geomorphological challenging and strategically less valuable loca-
tion. Focusing on castles located in rare and challenging geomorphological positions
may therefore lead to a better understanding of castle siting in the future.
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Sacred water canals or lakes, which provided water for all kinds of purification rites and other activities, were very specific and important features of temples in ancient Egypt. In addition to the longer-known textual record,... more
Sacred water canals or lakes, which provided water for all kinds of purification rites and other activities, were very specific and important features of temples in ancient Egypt. In addition to the longer-known textual record, preliminary geoarchaeological surveys have recently provided evidence of a sacred canal at the Temple of Bastet at Bubastis. In order to further explore the location, shape, and course of this canal and to find evidence of the existence of a second waterway, also described by Herodotus, 34 drillings and five 2D geoelectrical measurements were carried out in 2019 and 2020 near the temple. The drillings and 2D ERT surveying revealed loamy to clayey deposits with a thickness of up to five meters, most likely deposited in a very low energy fluvial system (i.e., a canal), allowing the reconstruction of two separate sacred canals both north and south of the Temple of Bastet. In addition to the course of the canals, the width of about 30 m fits Herod-otusʹ description of the sacred waterways. The presence of numerous artefacts proved the anthropogenic use of the ancient canals, which were presumably connected to the Nile via a tributary or canal located west or northwest of Bubastis.
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How to cite: Ullmann, T., Nill, L., Schiestl, R., Trappe, J., Lange-Athinodorou, E., Baumhauer, R., and Meister, J.: Mapping buried paleogeographical features of the Nile Delta (Egypt) using the Landsat archive, E&G Quaternary Sci. J.,... more
How to cite: Ullmann, T., Nill, L., Schiestl, R., Trappe, J., Lange-Athinodorou, E., Baumhauer, R., and Meister, J.: Mapping buried paleogeographical features of the Nile Delta (Egypt) using the Landsat archive, E&G Quaternary Sci. J., 69, 225-245, https://doi.org/10.5194/egqsj-69-225-2020, 2020. 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 (Jan-uary/February) seasons (NDWI). 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 meandering NDWI 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 NDWI does not provide an unambiguous delineation. Kurzfassung: Die Rekonstruktion der Paläotopographie und-hydrographie des Nildeltas spielt für landschaft-sarchäologische Fragestellungen eine zentrale Rolle, da die antike Siedlungsaktivität stark von der Dynamik des antiken Flussnetzes beeinflusst war. Für viele Bereiche des Deltas ist die Lage antiker Flussarme jedoch unbekannt, da diese im Laufe der Zeit verlandet und heute nicht mehr eindeutig im Landschaftsbild erkennbar sind. In diesem Kontext erlauben moderne Fernerkundungsdaten eine Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 226 T. Ullmann et al.: Paleogeographical features of the Nile Delta flächendeckende Untersuchung und ermöglichen Anomalien der Landbedeckung und Diskontinu-itäten der Oberflächenmorphologie zu identifizieren, wodurch wertvolle Hinweise zur paläogeomor-phologischen Situation gewonnen werden können. Zur Detektion solcher Anomalien wird in diesem Beitrag das Landsat Archiv genutzt, wobei verschiedene spektrale und zeitlich-räumliche Metriken für das gesamte Nildelta (Ägypten) für den Zeitraum 1985 bis 2019 in der Google Earth Engine berech-net wurden. Die Merkmale der Merkmale der Tasseled Cap Transformation (TC), des Normalized Difference Wetness Index (NDWI) und des Normalized Difference Vegetation Index (NDVI) wur-den analysiert und mit historischen topographischen Karten des Survey of Egypt, CORONA-Bildern, dem digitalen Höhenmodell der TanDEM-X-Mission und modernen Satellitenbildern verglichen. Die Ergebnisse der Zeitserienanalyse zeigen die Lage eines verlandeten Flussarms in der Nähe von Buto, der durch den Vergleich der Medianwerte des NDWI zwischen Sommer-(Juli/August) und Wintersai-son (Januar/Februar) (NDWI) deutlich zu erkennen ist. Der beobachtete Unterschied ist wahrschein-lich auf eine geringere Boden-und/oder Pflanzenfeuchtigkeit während des Sommers zurückzuführen, welche möglicherweise durch grobkörnige Ablagerungen im Untergrund bedingt wird. Ähnliche Anomalien wurden in der unmittelbaren Umgebung mehrerer pleistozäner Sandhügel (Geziras) und Siedlungshügel (Tells) des östlichen Nildeltas gefunden, was die Kartierungen der potentiellen ober-flächennahen Fortsetzung ermöglichte. Weitere lineare und mäandrierende NDWI Anomalien wur-den im östlichen Nildelta in der unmittelbaren Umgebung der antiken Stätte von Bubastis (Tell Basta) sowie einige Kilometer nördlich der Stadt Zagazig gefunden. Diese Anomalien weisen vermutlich auf frühere Verläufe von Flussarmen des Nils in diesem Bereich des Deltas hin.
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An integrated approach using contextual, use-wear, scientific and experimental methods was used to analyze the role of stone troughs of up to 165 l capacity at the Early Neolithic site Göbekli Tepe in the context of other stone containers... more
An integrated approach using contextual, use-wear, scientific and experimental methods was used to analyze the role of stone troughs of up to 165 l capacity at the Early Neolithic site Göbekli Tepe in the context of other stone containers found there. Around 600 (mostly fragmentary) vessels from the site constitute the largest known assemblage from the Pre-Pottery Neolithic of the Near East. Besides the large limestone troughs, it encompasses middle-sized, coarsely made limestone vessels, finely executed platters and ‘greenstone’ vessels. All lines of evidence taken together indicate the use of limestone troughs for the cooking of cereals.
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This paper aims to reconstruct Middle Bronze Age (MBA; 1600–1250 BCE) land use practices in the northwestern Alpine foreland (SW Germany, Hegau). We used a multi-proxy approach including the analysis of biogeochemical proxies from... more
This paper aims to reconstruct Middle Bronze Age (MBA; 1600–1250 BCE) land use practices in the northwestern Alpine foreland (SW Germany, Hegau). We used a multi-proxy approach including the analysis of biogeochemical proxies from colluvial deposits and buried topsoils in the surroundings of the well-documented settlement site of Anselfingen and off-site pollen data from two peat bogs. This approach allowed for in-depth insights into the MBA subsistence economy and shows that the MBA in the northwestern Alpine foreland was a period of establishing settlements with sophisticated land management and land use practices. The reconstruction of phases of colluvial deposition was based on ages from optically stimulated luminescence (OSL) and radiocarbon (AMS14C) dating from multi-layered colluvial deposits and supports the local archaeological record with the first phase of major colluvial deposition occurring during the MBA followed by phases of colluvial deposition during the Iron Age, the Medieval period and modern times. The on-site deposition of charred archaeobotanical remains and animal bones from archaeological features, as well as polycyclic aromatic hydrocarbons (PAHs), charcoal spectra, phytoliths, soil microstructure, urease enzymatic activity, microbial biomass carbon (Cmic) and heavy metal contents from colluvial deposits, were used as proxies for on-site and near-site land use practices. The charcoal spectra indicate MBA forest management which favored the dominance of Quercus in the woodland vegetation in the surrounding area north of the settlement site. Increased levels of 5β stanols (up to 40 %) and the occurrence of pig bones (up to 14 %) support the presence of a forest pasture mainly used for pig farming. In the surrounding area south of the settlement, an arable field with a buried MBA plow horizon (2Apb) could be verified by soil micromorphological investigations and high concentrations of grass phytoliths from leaves and stems. Agricultural practices (e.g., plowing) focussed on five staple crops (Hordeum distichon/vulgare, Triticum dicoccum, Triticum monococcum, Triticum spelta, Triticum aestivum/turgidum), while the presence of stilted pantries as storage facilities and of heat stones indicate post-harvest processing of cereal crops and other agrarian products within the settlement. In the area surrounding the settlement, increased levels of urease activity, compared to microbial biomass carbon (up to 2.1 µg N µg C−1mic), and input of herbivorous and omnivorous animal faeces indicate livestock husbandry on fallow land. The PAH suites and their spatial distribution support the use of fire for various purposes, e.g., for opening and maintaining the landscape, for domestic burning and for technical applications. The off-site palynological data support the observed change in on-site and near-site vegetation as well as the occurrence of related land use practices. During the Early and Middle Bronze Age, fire played a major role in shaping the landscape (peak of micro-charcoal during the MBA), and anthropogenic activities promoted Quercus-dominated forest ecosystems at the expense of natural beech forests. This indicates a broader regional human influence in the northwestern Alpine foreland at low- and mid-altitude inland sites during the Middle Bronze Age.
Phytoliths are plant microfossils commonly used as qualitative archive markers in archaeological and paleoecological studies. Their potential uniqueness to the vegetation cover, robustness to weathering, and lack of chemical alteration... more
Phytoliths are plant microfossils commonly used as qualitative archive markers in archaeological and paleoecological studies. Their potential uniqueness to the vegetation cover, robustness to weathering, and lack of chemical alteration along the transport paths make them potentially suitable tracers for quantitative erosion studies. In this pilot study, we explore the potential of phytoliths in a sediment fingerprinting study in the Ceguera catchment (28 km2) in NE Spain. The phytolith concentrations and morphologies of four land cover classes (agricultural land, badland, forest, and shrubland) were analysed, and their contributions to four natural sediment mixture samples along the river course were modelled. Phytolith concentrations allowed us to discriminate sources sufficiently, albeit with limited sample size. The performance of the phytoliths as tracer was tested by reproducing the sources of artificial sediment mixture samples with satisfactory recall ratio. Results identified badlands to be the main contributor, with 84–96% of the sediment load to the sinks, followed by shrublands (median 5%) and agricultural lands (median 2%). These major findings can be reproduced by other conventional erosion studies from this area, indicating that phytoliths are suited to quantifying erosion patterns in mesoscale catchments.
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In 2013 and 2014 fieldwork was carried out in the Widawa valley near Namysłów (Opole voivodeship) to investigate sites with iron smelting slag assumed to belong to Przeworsk culture. It was supposed that these surface sites dated back to... more
In 2013 and 2014 fieldwork was carried out in the Widawa valley near Namysłów (Opole voivodeship) to investigate sites with iron smelting slag assumed to belong to Przeworsk culture. It was supposed that these surface sites dated back to the late pre-Roman Iron Age (phases A 1-a 3) and thus belonged to the earliest Przeworsk culture. To verify this chronological classification, we conducted surveys at various sites and investigated the structure of iron smelting and especially its chronological position at the Pielgrzymowice site (municipality Wilków) by trial trenching. This paper presents the results of geophysical and archaeological as well as archaeobotanical investigations. Our studies in Pielgrzymowice show that iron smelting was carried out during the middle to late Roman period and under no circumstances during the late pre-Roman period. This unambiguous result is based on radiocarbon data from the lowest charcoal layer of a furnace and is supported by further absolute data from features in the surrounding area. The furnaces are those with a 'very big' slag pit, which are typical for the Roman period in Silesia and are themselves a relative means for chronological classification.
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This contribution highlights recent findings of geomorphological and geophysical investigations that were un-dertaken at the excavation site of Bubastis (Eastern Nile Delta, Egypt) in order to find evidence of the existence and location... more
This contribution highlights recent findings of geomorphological and geophysical investigations that were un-dertaken at the excavation site of Bubastis (Eastern Nile Delta, Egypt) in order to find evidence of the existence and location of the sacred canals of Bubastis that were described by Herodotus in the 5th century BCE. None of the preceding archaeological missions have reported remains of these canals. Drilling and sediment analyses in 2018 revealed clayey/silty deposits in the centre of the site at depths below 2.5 m above sea level, close to the northern enclosure of the Temple of Bastet. The recovered sediments, with a thickness of at least four metres, were situated below the floor level of the Temple of Bastet of the 1st mill. BCE and contained fragments of pottery as well. Conducted DCR (direct current resistivity) and 2D electrical surveying confirmed the drilling results. These geophysical investigations indicated trench-formed layers of low resistivity values adjunct to the northern enclosure of the Temple of Bastet. The recovered deposits were therefore interpreted as infills that were most likely accumulated in a fluvial system of very low energy, e.g. an ox-bow lake, (abandoned) channel or lake. Presumptively, this waterway was prone to refilling, but also to infilling, by a tributary situated north or northwest of the Temples of Bastet and Pepi I.
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We analyze the processing of cereals and its role at Early Neolithic Göbekli Tepe, southeastern Anatolia (10th / 9th millennium BC), a site that has aroused much debate in archaeological discourse. To date, only zooarchaeological evidence... more
We analyze the processing of cereals and its role at Early Neolithic Göbekli Tepe, southeastern Anatolia (10th / 9th millennium BC), a site that has aroused much debate in archaeological discourse. To date, only zooarchaeological evidence has been discussed in regard to the subsistence of its builders. Göbekli Tepe consists of monumental round to oval buildings, erected in an earlier phase, and smaller rectangular buildings, built around them in a partially contemporaneous and later phase. The monumental buildings are best known as they were in the focus of research. They are around 20 m in diameter and have stone pillars that are up to 5.5 m high and often richly decorated. The rectangular buildings are smaller and–in some cases–have up to 2 m high, mostly undecorated, pillars. Especially striking is the number of tools related to food processing, including grinding slabs/bowls, handstones, pestles, and mortars, which have not been studied before. We analyzed more than 7000 artifacts for the present contribution. The high frequency of artifacts is unusual for contemporary sites in the region. Using an integrated approach of formal, experimental, and macro- / microscopical use-wear analyses we show that Neolithic people at Göbekli Tepe have produced standardized and efficient grinding tools, most of which have been used for the processing of cereals. Additional phytolith analysis confirms the massive presence of cereals at the site, filling the gap left by the weakly preserved charred macro-rests. The organization of work and food supply has always been a central question of research into Göbekli Tepe, as the construction and maintenance of the monumental architecture would have necessitated a considerable work force. Contextual analyses of the distribution of the elements of the grinding kit on site highlight a clear link between plant food preparation and the rectangular buildings and indicate clear delimitations of working areas for food production on the terraces the structures lie on, surrounding the circular buildings. There is evidence for extensive plant food processing and archaeozoological data hint at large-scale hunting of gazelle between midsummer and autumn. As no large storage facilities have been identified, we argue for a production of food for immediate use and interpret these seasonal peaks in activity at the site as evidence for the organization of large work feasts.
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In the dry zone of Sri Lanka, human-made reservoirs have served for the collection, storage and distribution of rainfall and runoff and provide irrigation water for the cultivation of paddy for 2000 years. This paper introduces the layout... more
In the dry zone of Sri Lanka, human-made reservoirs have served for the collection, storage and distribution of rainfall and runoff and provide irrigation water for the cultivation of paddy for 2000 years. This paper introduces the layout and function of four traditional village tank cascade systems in the hinterland of Anuradhapura, located in the North Central Province in Sri Lanka. In contrast to large-scale tanks, these systems are managed and maintained by local villagers. Sedimentological data from two tanks provide information about processes leading to the formation of these deposits and their post-sedimentary, partly human-induced alterations. The presented data support the hypothesis, that the decentral managed tanks were not affected by severe erosion after the abandonment of the ancient capital Anuradhapura in the 11th century CE, a period that was characterized by socio-economic instability and increased climatic fluctuations. Presented results underline the significance of small-scale tank cascades systems to buffer the effects of climatic fluctuations and point to their potential as a cornerstone in coping with future climate change in the dry zone of Sri Lanka.
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Northeastern Jordan is one of the few remaining regions in the Middle East where pastoral nomadism is still practiced. In this desert region, pastoral mobility is an adapted land use able to cope with low rainfall rates, great seasonal... more
Northeastern Jordan is one of the few remaining regions in the Middle East where pastoral nomadism is still practiced. In this desert region, pastoral mobility is an adapted land use able to cope with low rainfall rates, great seasonal and annual rainfall variations and thus heterogeneous vegetation and water availability. During winter, herders and their livestock move into the desert; in summer they move to the desert margins to places with perennial water supply. First traces of mobile pastoralism date back to the beginning of the Late Neolithic.
Within the basaltic region of northeastern Jordan, there is a dense distribution of archaeological remains; some of them can be linked to pastoral groups due to the herders' ancient practice of building agglomerations of sub-circular enclosures ('clustered enclosures') made of basalt boulders for corralling their flocks and domestic activities. These features provide an excellent opportunity to investigate a landscape that shows traces of pastoral activity since eight to nine Millennia.
In this study, 9118 clustered enclosures in the northeastern Jordanian basalt desert have been systematically recorded using satellite imagery. In order to investigate potential migration or communication routes, grazing lands and social interactions of former pastoralists, we examine their first- and second-order characteristics using distance and density based approaches of point pattern analyses by integrating geomorphometric and geomorphological site properties. The results of this spatial analysis are combined with available archaeological data and a review on traditional herding practices in northeastern Jordan. Overall, the results demonstrate that the observed spatial distribution of clustered enclosures is influenced locally by natural characteristics but regionally by cultural practices.
Within the basaltic region of northeastern Jordan, there is a dense distribution of archaeological remains; some of them can be linked to pastoral groups due to the herders' ancient practice of building agglomerations of sub-circular enclosures ('clustered enclosures') made of basalt boulders for corralling their flocks and domestic activities. These features provide an excellent opportunity to investigate a landscape that shows traces of pastoral activity since eight to nine Millennia.
In this study, 9118 clustered enclosures in the northeastern Jordanian basalt desert have been systematically recorded using satellite imagery. In order to investigate potential migration or communication routes, grazing lands and social interactions of former pastoralists, we examine their first- and second-order characteristics using distance and density based approaches of point pattern analyses by integrating geomorphometric and geomorphological site properties. The results of this spatial analysis are combined with available archaeological data and a review on traditional herding practices in northeastern Jordan. Overall, the results demonstrate that the observed spatial distribution of clustered enclosures is influenced locally by natural characteristics but regionally by cultural practices.
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Located in the basalt desert of northeastern Jordan, Early Bronze Age (EBA) Jawa is regarded as one of the major settlements in the Middle East during the 4th millennium BCE. In addition to a sophisticated water storage system, the... more
Located in the basalt desert of northeastern Jordan, Early Bronze Age (EBA) Jawa is regarded as one of the major settlements in the Middle East during the 4th millennium BCE. In addition to a sophisticated water storage system, the existence of three complex agricultural terrace systems based on runoff and floodwater irrigation in the close vicinity was recently revealed.
This paper investigates the impact of these water management strategies on harvest yields and the scale of the ‘on-site’ crop production at Jawa by applying a crop simulation model (CropSyst). Simulations for the cultivation of winter barley, winter wheat and lentils were performed for the period from 1983 to 2014. To simulate the different runoff irrigation schemes, a curve-number-based rainfall-runoff model was applied. To estimate the number of people that could have been supplied by the local food production, simple calculations based on metabolic calorie requirements and agricultural and pastoral production rates were conducted.
This study shows that the runoff farming systems of EBA Jawa are relatively effective under current rainfall conditions. Even during dryer seasons, the simulated crop yields are much higher under runoff irrigation/floodwater irrigation than under non-irrigated conditions. On average the crop yields increase by 1.5 to 6 times, depending on crop type and runoff irrigation level. Moreover, a marked decrease in crop failures could be observed. The total crop and animal production could have satisfied the nutritional requirements of about 500 to 1000 persons per year. Considering the estimated maximum population for EBA Jawa, ranging from 3400 to 5000 people (Helms, 1981), local production did not meet the basic needs of all inhabitants. This indicates that trade might have been an important branch of Jawa's economy in order to supplement food resources. Moreover, former population estimates for ancient Jawa might be overstated.
This paper investigates the impact of these water management strategies on harvest yields and the scale of the ‘on-site’ crop production at Jawa by applying a crop simulation model (CropSyst). Simulations for the cultivation of winter barley, winter wheat and lentils were performed for the period from 1983 to 2014. To simulate the different runoff irrigation schemes, a curve-number-based rainfall-runoff model was applied. To estimate the number of people that could have been supplied by the local food production, simple calculations based on metabolic calorie requirements and agricultural and pastoral production rates were conducted.
This study shows that the runoff farming systems of EBA Jawa are relatively effective under current rainfall conditions. Even during dryer seasons, the simulated crop yields are much higher under runoff irrigation/floodwater irrigation than under non-irrigated conditions. On average the crop yields increase by 1.5 to 6 times, depending on crop type and runoff irrigation level. Moreover, a marked decrease in crop failures could be observed. The total crop and animal production could have satisfied the nutritional requirements of about 500 to 1000 persons per year. Considering the estimated maximum population for EBA Jawa, ranging from 3400 to 5000 people (Helms, 1981), local production did not meet the basic needs of all inhabitants. This indicates that trade might have been an important branch of Jawa's economy in order to supplement food resources. Moreover, former population estimates for ancient Jawa might be overstated.
Located in the arid basalt desert of northeastern Jordan, the settlement of Jawa is by far the largest and best-preserved archaeological site in the region. The Early Bronze Age (EBA) settlement phase of Jawa (3500–3000 BCE) is... more
Located in the arid basalt desert of northeastern Jordan, the settlement of Jawa is by far the largest and best-preserved archaeological site in the region. The Early Bronze Age (EBA) settlement phase of Jawa (3500–3000 BCE) is characterized by a highly sophisticated water storage system made of a series of pools, dams, and canals. In addition, recent archaeological and geoarchaeological surveys have uncovered agricultural terrace systems in the nearby vicinity.
In this study, four of these runoff terrace systems were investigated by detailed mapping. Additionally, thirteen sediment profiles from inside and outside the terrace systems were recorded and sampled. The examined samples were analyzed for bulk chemistry, texture, phytoliths, diatoms, and dung spherulites to supply information on the environmental and depositional conditions. The terrace systems were dated using optically stimulated luminescence (OSL).
Ancient terrace agriculture was practiced on slopes, small plateaus, and valleys close to Jawa through the use of surface canals, which collected and diverted floodwater from nearby wadis or runoff from adjacent slopes. The terraced fields were usually arranged in cascades and comprised a system of risers, canals, and spillways. The terrace fills investigated yield OSL ages of around 3300 BCE, indicating that the terraces were constructed in the Early Bronze Age. The terrace fill sequences are composed of mixed unstratified fine sediments of local origin, reflecting low-energy fluvial deposition regimes. The phytolith record is dominated by Pooid grasses that include the most common Near Eastern cereals, such as wheat and barley. Increased phytolith concentrations in terrace fill sediments, as compared to samples from non-terrace deposits nearby, suggest increased plant growth and water availability within the terraces. Whether the terrace systems were used for growing food crops only or whether they were additionally used for grazing cannot be ascertained. Overall, quantitative phytolith analyses in arid environments are well suited to investigate temporal and spatial distributions of plant microfossil concentrations and their relation to human activity or paleoenvironmental conditions.
In this study, four of these runoff terrace systems were investigated by detailed mapping. Additionally, thirteen sediment profiles from inside and outside the terrace systems were recorded and sampled. The examined samples were analyzed for bulk chemistry, texture, phytoliths, diatoms, and dung spherulites to supply information on the environmental and depositional conditions. The terrace systems were dated using optically stimulated luminescence (OSL).
Ancient terrace agriculture was practiced on slopes, small plateaus, and valleys close to Jawa through the use of surface canals, which collected and diverted floodwater from nearby wadis or runoff from adjacent slopes. The terraced fields were usually arranged in cascades and comprised a system of risers, canals, and spillways. The terrace fills investigated yield OSL ages of around 3300 BCE, indicating that the terraces were constructed in the Early Bronze Age. The terrace fill sequences are composed of mixed unstratified fine sediments of local origin, reflecting low-energy fluvial deposition regimes. The phytolith record is dominated by Pooid grasses that include the most common Near Eastern cereals, such as wheat and barley. Increased phytolith concentrations in terrace fill sediments, as compared to samples from non-terrace deposits nearby, suggest increased plant growth and water availability within the terraces. Whether the terrace systems were used for growing food crops only or whether they were additionally used for grazing cannot be ascertained. Overall, quantitative phytolith analyses in arid environments are well suited to investigate temporal and spatial distributions of plant microfossil concentrations and their relation to human activity or paleoenvironmental conditions.