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  • Meer  (2)
  • 303-U1307A; 303-U1307B; Cassidulina teretis, δ13C; Cassidulina teretis, δ18O; Comment; Corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp303; Gyroidinoides sp., δ13C; Gyroidinoides sp., δ18O; Individuals; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 251; North Atlantic Climate 1; Oridorsalis tener, δ13C; Oridorsalis tener, δ18O; Sample code/label; δ13C, adjusted/corrected; δ13C, standard deviation; δ18O, adjusted/corrected; δ18O, standard deviation  (1)
  • 311016224; Bavaria; CaCO3 analysis, Scheibler, DIN 19684; Calcium carbonate; Calculated; Calculated from total carbon minus CaCO3-carbon; Carbon, organic, total; Charcoal; Cobra percussion corer; CPERC; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Direct push applications in wetland (geo)archaeology; Driving cores; Elevation of event; Event label; floodplain; Holocene; Laboratory code/label; Late Neolithic; Latitude of event; Longitude of event; Loosbach valley, Pestenacker, Germany; PA_UL_GEO; PA_UL_GEO_RK10; PA_UL_GEO_RK12; PA_UL_GEO_RK15; PA_UL_GEO_RK16; PA_UL_GEO_RK8; Pestenacker; RK10; RK12; RK15; RK16; RK8; Siliciclastics; South Germany; TC; TOC; UNESCO world Heritage; wetlands; Wood remains  (1)
  • 551  (1)
Keywords
Language
  • 1
    Keywords: Carbon cycle (Biogeochemistry) ; Marine organisms ; Chemical oceanography ; Dissertation ; Hochschulschrift ; Meer ; Partikulärer organischer Stoff ; Meereschemie ; Biogeochemie ; Meer ; Kohlenstoffhaushalt ; Stickstoffhaushalt ; Redfield-Verhältnis ; Meer ; Partikulärer organischer Stoff ; Meereschemie ; Biogeochemie ; Meer ; Kohlenstoffhaushalt ; Stickstoffhaushalt ; Redfield-Verhältnis ; Meer ; Kohlenstoffhaushalt ; Partikulärer organischer Stoff ; Kohlenstoff ; Stickstoff
    Type of Medium: Book
    Pages: VI, 98 S. , Ill., graph. Darst., Kt.
    Series Statement: Berichte zur Polar- und Meeresforschung 437
    DDC: 577/.144
    RVK:
    Language: English
    Note: Zsfassung in dt. Spr , Zugl.: Bremen, Univ., Diss., 2002
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  • 2
    Keywords: Forschungsbericht ; Pleistozän ; Paläoklima ; Modell ; Simulation ; Meer ; Kohlenstoffkreislauf
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (17 Seiten, 234,62 KB)
    Language: German
    Note: Paralleltitel dem englischen Berichtsblatt entnommen , Förderkennzeichen BMBF 01LP1505A-G , Verbundnummer 01161825 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Sprache der Zusammenfassung: Deutsch, Englisch
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  • 3
    Publication Date: 2023-07-09
    Keywords: 303-U1307A; 303-U1307B; Cassidulina teretis, δ13C; Cassidulina teretis, δ18O; Comment; Corrected; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Exp303; Gyroidinoides sp., δ13C; Gyroidinoides sp., δ18O; Individuals; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mass spectrometer Finnigan MAT 251; North Atlantic Climate 1; Oridorsalis tener, δ13C; Oridorsalis tener, δ18O; Sample code/label; δ13C, adjusted/corrected; δ13C, standard deviation; δ18O, adjusted/corrected; δ18O, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 194 data points
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  • 4
    Publication Date: 2024-04-20
    Description: In 2018 and 2019, driving cores 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. The recovered cores were documented and sampled in a 5-10 cm resolution for subsequent laboratory analysis. Bulk samples from RK8, RK10, RK12, RK15 and RK16 cores were used for subsequent geochemical analysis. All samples were air dried, sieved (2 mm sieve) and weighed. Macroscopic charcoal and wood remains were removed and weighed. For calculating the total organic matter (TOC), we measured the content of total carbon (TC) by using a CNS analyser vario EL cube (Elementar) and determined the content of inorganic carbon (TIC) by calcimeter measurements (Scheibler method, Eijkelkamp). Resulting values of organic carbon (TOC) were multiplied by 1.72 in order to obtain contents of organic matter (OM). The siliciclastic content was calculated from the sum of carbonates and organic matter and subtracted this from 100 %. The content of charcoal and wood remains [%] is in relation to the total dry weight of the fine soil. The stratigraphical and geochemical findings were classified into sedimentological units. The detailed descriptions of the stratigraphical data are given in the document “Detailed lithological descriptions of recovered cores from the Loosbach valley at Pestenacker”.
    Keywords: 311016224; Bavaria; CaCO3 analysis, Scheibler, DIN 19684; Calcium carbonate; Calculated; Calculated from total carbon minus CaCO3-carbon; Carbon, organic, total; Charcoal; Cobra percussion corer; CPERC; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Direct push applications in wetland (geo)archaeology; Driving cores; Elevation of event; Event label; floodplain; Holocene; Laboratory code/label; Late Neolithic; Latitude of event; Longitude of event; Loosbach valley, Pestenacker, Germany; PA_UL_GEO; PA_UL_GEO_RK10; PA_UL_GEO_RK12; PA_UL_GEO_RK15; PA_UL_GEO_RK16; PA_UL_GEO_RK8; Pestenacker; RK10; RK12; RK15; RK16; RK8; Siliciclastics; South Germany; TC; TOC; UNESCO world Heritage; wetlands; Wood remains
    Type: Dataset
    Format: text/tab-separated-values, 1509 data points
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  • 5
    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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