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  • 303-U1307A; 303-U1307B; Comment; Corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp303; Individuals; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 251; Melonis barleeanus, δ13C; Melonis barleeanus, δ18O; Melonis pompilioides, δ13C; Melonis pompilioides, δ18O; North Atlantic Climate 1; Sample code/label; δ13C, standard deviation; δ18O, adjusted/corrected; δ18O, standard deviation  (1)
  • 311016224; Bavaria; Cobra percussion corer; CPERC; Direct push applications in wetland (geo)archaeology; Driving cores; floodplain; Hand drill; HDRILL; Holocene; Late Neolithic; Loosbach valley, Pestenacker, Germany; PA_UL_GEO; PA_UL_GEO_RK1; PA_UL_GEO_RK10; PA_UL_GEO_RK11; PA_UL_GEO_RK12; PA_UL_GEO_RK13; PA_UL_GEO_RK14; PA_UL_GEO_RK15; PA_UL_GEO_RK16; PA_UL_GEO_RK2; PA_UL_GEO_RK3; PA_UL_GEO_RK6; PA_UL_GEO_RK7; PA_UL_GEO_RK8; PA_UL_GEO_RK9; PA_UL_GEO_S1; PA_UL_GEO_S10; PA_UL_GEO_S11; PA_UL_GEO_S12; PA_UL_GEO_S13; PA_UL_GEO_S14; PA_UL_GEO_S15; PA_UL_GEO_S16; PA_UL_GEO_S17; PA_UL_GEO_S18; PA_UL_GEO_S19; PA_UL_GEO_S2; PA_UL_GEO_S20; PA_UL_GEO_S3; PA_UL_GEO_S4; PA_UL_GEO_S5; PA_UL_GEO_S6; PA_UL_GEO_S7; PA_UL_GEO_S8; PA_UL_GEO_S9; Pestenacker; RK1; RK10; RK11; RK12; RK13; RK14; RK15; RK16; RK2; RK3; RK6; RK7; RK8; RK9; S1; S10; S11; S12; S13; S14; S15; S16; S17; S18; S19; S2; S20; S3; S4; S5; S6; S7; S8; S9; South Germany; UNESCO world Heritage; wetlands  (1)
  • 551  (1)
  • Aeolian sediments  (1)
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  • 1
    Publication Date: 2023-09-13
    Description: The soilscapes along the southern and western coast of Crete (Greece) are dominated by coarse-grained reddish-brown slope sediments whose natural (pre-anthropogenic) configuration and properties are difficult to reconstruct due to the long history of intense land use. As a consequence, datable terrestrial sediment archives of pre-anthropogenic genesis are scarce. We present preliminary results of a study performed on an accumulation within an alluvial fan south of Stomio Bay in southwestern Crete. The studied profile is located in a small depression and is composed of a sequence of sandy to silty yellowish-brown calcareous sediments overlying coarse-grained slope sediments, including a fossil topsoil horizon. Based on macroscopic, micromorphological, geochemical, geophysical and mineralogical analysis, we interpret the fine-grained sediments to have a local aeolian origin. OSL dating indicates a final deposition phase during the early Holocene. Considering the scarcity of early Holocene terrestrial archives in Crete, the analysed profile provides valuable data for the reconstruction of landscape dynamics and paleoecological conditions as well as soil-sediment configurations during this time period. Additional research is needed to address the specific source area(s) as well as the ages of the deposition of slope sediments and formation of the fossil topsoil.
    Description: Freie Universität Berlin (1008)
    Keywords: ddc:551.3 ; Aeolian sediments ; Fossil soil ; Early Holocene ; Crete ; Eastern Mediterranean
    Language: English
    Type: doc-type:article
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  • 2
    Publication Date: 2023-06-27
    Keywords: 303-U1307A; 303-U1307B; Comment; Corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp303; Individuals; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 251; Melonis barleeanus, δ13C; Melonis barleeanus, δ18O; Melonis pompilioides, δ13C; Melonis pompilioides, δ18O; North Atlantic Climate 1; Sample code/label; δ13C, standard deviation; δ18O, adjusted/corrected; δ18O, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 939 data points
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  • 3
    Publication Date: 2024-04-20
    Description: In 2018 and 2019, 14 driving cores and 20 hand drillings were carried out to reconstruct the Holocene deposition history of the Loosbach valley at Pestenacker, an UNESCO world heritage site of Late Neolithic wetland occupation. A hand-held Cobra Pro (Atlas Copco) driving core drilling system and 60 mm diameter open corer recovered sediments. The achieved segments of each 1 m lengths were accessed on site towards sediment features and colours according to AG Boden (2005) and Munsell Colour Chart. The geochemical findings were classified into sedimentological units. The detailed descriptions of the geochemical data are given in the document „Geochemical data of recovered cores from the Loosbach valley at Pestenacker“.
    Keywords: 311016224; Bavaria; Cobra percussion corer; CPERC; Direct push applications in wetland (geo)archaeology; Driving cores; floodplain; Hand drill; HDRILL; Holocene; Late Neolithic; Loosbach valley, Pestenacker, Germany; PA_UL_GEO; PA_UL_GEO_RK1; PA_UL_GEO_RK10; PA_UL_GEO_RK11; PA_UL_GEO_RK12; PA_UL_GEO_RK13; PA_UL_GEO_RK14; PA_UL_GEO_RK15; PA_UL_GEO_RK16; PA_UL_GEO_RK2; PA_UL_GEO_RK3; PA_UL_GEO_RK6; PA_UL_GEO_RK7; PA_UL_GEO_RK8; PA_UL_GEO_RK9; PA_UL_GEO_S1; PA_UL_GEO_S10; PA_UL_GEO_S11; PA_UL_GEO_S12; PA_UL_GEO_S13; PA_UL_GEO_S14; PA_UL_GEO_S15; PA_UL_GEO_S16; PA_UL_GEO_S17; PA_UL_GEO_S18; PA_UL_GEO_S19; PA_UL_GEO_S2; PA_UL_GEO_S20; PA_UL_GEO_S3; PA_UL_GEO_S4; PA_UL_GEO_S5; PA_UL_GEO_S6; PA_UL_GEO_S7; PA_UL_GEO_S8; PA_UL_GEO_S9; Pestenacker; RK1; RK10; RK11; RK12; RK13; RK14; RK15; RK16; RK2; RK3; RK6; RK7; RK8; RK9; S1; S10; S11; S12; S13; S14; S15; S16; S17; S18; S19; S2; S20; S3; S4; S5; S6; S7; S8; S9; South Germany; UNESCO world Heritage; wetlands
    Type: Dataset
    Format: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, 102.9 kBytes
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  • 4
    Publication Date: 2021-07-04
    Description: Sediment budgeting concepts serve as quantification tools to decipher the erosion and accumulation processes within a catchment and help to understand these relocation processes through time. While sediment budgets are widely used in geomorphological catchment‐based studies, such quantification approaches are rarely applied in geoarchaeological studies. The case of Charlemagne's summit canal (also known as Fossa Carolina) and its erosional collapse provides an example for which we can use this geomorphological concept and understand the abandonment of the Carolingian construction site. The Fossa Carolina is one of the largest hydro‐engineering projects in Medieval Europe. It is situated in Southern Franconia (48.9876°N, 10.9267°E; Bavaria, southern Germany) between the Altmühl and Swabian Rezat rivers. It should have bridged the Central European watershed and connected the Rhine–Main and Danube river systems. According to our dendrochronological analyses and historical sources, the excavation and construction of the Carolingian canal took place in AD 792 and 793. Contemporary written sources describe an intense backfill of excavated sediment in autumn AD 793. This short‐term erosion event has been proposed as the principal reason for the collapse and abandonment of the hydro‐engineering project. We use subsurface data (drillings, archaeological excavations, and direct‐push sensing) and geospatial data (a LiDAR digital terrain model (DTM), a pre‐modern DTM, and a 3D model of the Fossa Carolina] for the identification and sediment budgeting of the backfills. Dendrochronological findings and radiocarbon ages of macro remains within the backfills give clear evidence for the erosional collapse of the canal project during or directly after the construction period. Moreover, our quantification approach allows the detection of the major sedimentary collapse zone. The exceedance of the manpower tipping point may have caused the abandonment of the entire construction site. The spatial distribution of the dendrochronological results indicates a north–south direction of the early medieval construction progress. © 2020 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd
    Description: The sediment budgeting concept as erosion and accumulation quantification tool helps in understanding the abrupt backfilling of excavated material in the construction pit, which may have forced the abandonment of the Carolingian canal in southern Germany at the end of the year AD 793. The backfill sediments could be dated precisely through radiocarbon dating of macro remains and dendrochronology of excavated timbers. These timbers recovered in three different archaeological excavation trenches reveal a Carolingian construction progress from North to South.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: 551 ; Sediment budgeting ; Geomorphological modelling ; Backfill processes ; Geoarchaeology ; Fossa Carolina ; Early Middle Ages ; South Germany
    Type: article
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