@article{UllmannMoellerBaumhaueretal.2022,
  author    = {Ullmann, Tobias and M{\"o}ller, Eric and Baumhauer, Roland and Lange-Athinodorou, Eva and Meister, Julia},
  title     = {A new Google Earth Engine tool for spaceborne detection of buried palaeogeographical features - examples from the Nile Delta (Egypt)},
  series = {E\&G Quaternary Science Journal},
  volume    = {71},
  journal   = {E\&G Quaternary Science Journal},
  number    = {2},
  doi       = {10.5194/egqsj-71-243-2022},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-300164},
  pages     = {243-247},
  year      = {2022},
  abstract  = {No abstract available.},
  language  = {en}
}
@article{StanleyUllmannLangeAthinodorou2021,
  author    = {Stanley, Jean-Daniel and Ullmann, Tobias and Lange-Athinodorou, Eva},
  title     = {Holocene aridity-induced interruptions of human activity along a fluvial channel in Egypt's northern delta},
  series = {Quaternary},
  volume    = {4},
  journal   = {Quaternary},
  number    = {4},
  issn      = {2571-550X},
  doi       = {10.3390/quat4040039},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-250285},
  year      = {2021},
  abstract  = {Geoarchaeological information presented here pertains to a subsidiary Nile channel that once flowed west of the main Sebennitic distributary and discharged its water and sediments at Egypt's then north-central deltaic coast. Periodical paleoclimatic episodes during the later Middle and Upper Holocene included decreased rainfall and increased aridity that reduced the Nile's flow levels and thus likely disrupted nautical transport and anthropogenic activity along this channel. Such changes in this deltaic sector, positioned adjacent to the Levantine Basin in the Eastern Mediterranean, can be attributed to climatic shifts triggered as far as the North Atlantic to the west, and African highland source areas of the Egyptian Nile to the south. Of special interest in a study core recovered along the channel are several sediment sequences without anthropogenic material that are interbedded between strata comprising numerous potsherds. The former are interpreted here as markers of increased regional aridity and reduced Nile flow which could have periodically disrupted the regional distribution of goods and nautical activities. Such times occurred ~5000 years B.P., ~4200-4000 years B.P., ~3200-2800 years B.P., ~2300-2200 years B.P., and more recently. Periods comparable to these are also identified by altered proportions of pollen, isotopic and compositional components in different radiocarbon-dated Holocene cores recovered elsewhere in the Nile delta, the Levantine region to the east and north of Egypt, and in the Faiyum depression south of the delta.},
  language  = {en}
}
@article{MeisterLangeAthinodorouUllmann2021,
  author    = {Meister, Julia and Lange-Athinodorou, Eva and Ullmann, Tobias},
  title     = {Preface: Special Issue "Geoarchaeology of the Nile Delta"},
  series = {E\&G Quarternary Science Journal},
  volume    = {70},
  journal   = {E\&G Quarternary Science Journal},
  doi       = {10.5194/egqsj-70-187-2021},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-261195},
  pages     = {187-190},
  year      = {2021},
  abstract  = {No abstract available.},
  language  = {en}
}
@article{MeisterGarbeTrappeetal.2021,
  author    = {Meister, Julia and Garbe, Philipp and Trappe, Julian and Ullmann, Tobias and Es-Senussi, Ashraf and Baumhauer, Roland and Lange-Athinodorou, Eva and El-Raouf, Amr Abd},
  title     = {The Sacred Waterscape of the Temple of Bastet at Ancient Bubastis, Nile Delta (Egypt)},
  series = {Geosciences},
  volume    = {11},
  journal   = {Geosciences},
  number    = {9},
  issn      = {2076-3263},
  doi       = {10.3390/geosciences11090385},
  url       = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-246129},
  year      = {2021},
  abstract  = {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 Herodotus' 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.},
  language  = {en}
}