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  • AGE; Astrochronology; borehole logging data; Calculated, according to Kaboth-Bahr et al. (2024); Carbon, organic, total; DEPTH, sediment/rock; FB2001; Geochemical proxies; Hydraulic rotary drilling; Messel, Germany; middle Eocene; Sulfur/Carbon Analyzer, LECO Corporation, SC-144DR  (1)
  • Araliaceoipollenites spp.; Arecipites sp.; Baculatisporites sp.; Basopollis orthobasalis; Bombacacidites sp.; Botryococcus; Brevaxones undifferentiated; Brosipollis salebrosus; Camarozonosporites sp.; Caryapollenites triangulus; Celtipollenites spp.; Cicatricosisporites sp.; Compositoipollenites rhizophorus; Dicolpopollis kockeli; Dinoflagellate cyst; Droseridites sp.; Emmapollis pseudoemmaensis; Ericipites spp.; Helmstedt; Ilexpollenites spp.; Inaperturopollenites sp.; Intratriporopollenites maxoides; Labraferoidaepollenites menatensis; Labrapollis labraferus; Laevigatosporites sp.; Leiotriletes sp.; Lithology/composition/facies; Lower Saxony, Northern Germany; Milfordia minima; Momipites punctatus; Momipites quietus; Monocolpopollenites tranquillus; Nepenthes-type; Nudopollis terminalis; Nyssapollenites kruschi; ORDINAL NUMBER; OUTCROP; Outcrop sample; Ovoidites sp.; Pentapollenites pentangulus; Pityosporites labdacus; Planctonites stellarius; Platycaryapollenites spp.; Plicapollis pseudoexcelsus; Plicatopollis plicatus; Pollen, tricolporate undifferentiated; pollen analytical standard techniques (Faegri & Iversen, 1989, Textbook Pollen); Polypodiaceoisporites sp.; Polyporopollenites spp.; Pompeckjoidaepollenites subhercynicus; Porocolpopollenites rarobaculatus; Porocolpopollenites sp.; Prasinophytes; Psilodiporites iszkaszentgyoergyi; Pterocaryapollenites stellatus; Punctilongisulcites microechinatus; Reticulataepollis intergranulatus; Sparganiaceaepollenites sp.; Spinaepollis spinosus; Spinizonocolpites spp.; Spores, trilete undifferentiated; Stereisporites sp.; Subtriporopollenites anulatus; Subtriporopollenites constans; sum spores; Tegumentisporis sp.; Tetracolporopollenites spp.; Thomsonipollis magnificus; Triatriopollenites bituitus; Triatriopollenites excelsus; Triatriopollenites rurensis; Tricolpopollenites asper; Tricolpopollenites liblarensis; Tricolpopollenites microhenrici; Tricolpopollenites quisqualis; Tricolpopollenites retiformis; Tricolpopollenites vegetus; Tricolporopollenites cingulum; Tricolporopollenites crassiexinus; Tricolporopollenites edmundii; Tricolporopollenites eofagoides; Tricolporopollenites mansfeldensis; Tricolporopollenites marcodurensis; Tricolporopollenites megaexactus; Tricolporopollenites messelensis; Tricolporopollenites microporitus; Tricolporopollenites microreticulatus; Tricolporopollenites parmularius; Tricolporopollenites pseudocingulum; Tricolporopollenites satzveyensis; Tricolporopollenites sole de portai; Tricolporopollenites sp.; Tricolporopollenites vancampoae; Triporopollenites coryloides; Triporopollenites rhenanus; Triporopollenites robustus; Varia; Verrucatosporites favus; Zonocostites ramonae  (1)
  • Average chain length; Fichtelite; Identification; Lithologic unit/sequence; Lithology/composition/facies; Lower Saxony, Germany; n-Alkane, C23/C31 ratio; OUTCROP; Outcrop sample; Ratio; Schoningen  (1)
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  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Riegel, Walter; Lenz, Olaf K; Wilde, Volker (2015): From open estuary to meandering river in a greenhouse world: an ecological case study from the middle Eocene of Helmstedt, Northern Germany. Palaios, 30(4), 304-326, https://doi.org/10.2110/palo.2014.005
    Publication Date: 2023-07-10
    Description: Tropical climates reached their northernmost expansion during the early Paleogene greenhouse phase, supporting a paratropical biota as far north as the southern shore of the ancient North Sea. There, relative sea-level fluctuations led to the formation of transgressive-regressive sequences, exposed in open-cast lignite mines in the area of Helmstedt (Lower Saxony, Germany), which record environmental changes at the marine-terrestrial interface. We studied an example from the middle Eocene of the Helmstedt Mine from which we reconstruct ecological successions from open estuary to meandering river environments, which represent vegetation at the Paleogene climatic optimum. In the absence of vertebrate and shelly fossils, environmental interpretations are made exclusively on plant matter in the sediment. Vegetational reconstructions are based mainly on quantitative palynological analyses, supported by paleobotanical and organic-petrographical evidence and confirmed by Principal Component Analysis. Diverse dinocyst assemblages in conjunction with Ophiomorpha-type bioturbation indicate open estuarine conditions. These are succeeded by mangrove, represented by pollen of Rhizophora, Avicennia, Nypa and the form species Psilodiporites iszkaszentgoergyi, and marsh environments, indicated by pollen of Restionaceae, Sparganiaceae/Typhaceae and fern spores. Subsequent lowland mire forests are characterized by a dominance of either the Tricolporopollenites cingulum group (Fagaceae) or triporate pollen of the Triporopollenites robustus/rhenanus complex (Myricaceae/Betulaceae). Within this landscape coexists a meandering river system, represented by channel lag and point-bar deposits of the active channel and by the clastic to lignitic sedimentary fill of an abandoned channel.
    Keywords: Araliaceoipollenites spp.; Arecipites sp.; Baculatisporites sp.; Basopollis orthobasalis; Bombacacidites sp.; Botryococcus; Brevaxones undifferentiated; Brosipollis salebrosus; Camarozonosporites sp.; Caryapollenites triangulus; Celtipollenites spp.; Cicatricosisporites sp.; Compositoipollenites rhizophorus; Dicolpopollis kockeli; Dinoflagellate cyst; Droseridites sp.; Emmapollis pseudoemmaensis; Ericipites spp.; Helmstedt; Ilexpollenites spp.; Inaperturopollenites sp.; Intratriporopollenites maxoides; Labraferoidaepollenites menatensis; Labrapollis labraferus; Laevigatosporites sp.; Leiotriletes sp.; Lithology/composition/facies; Lower Saxony, Northern Germany; Milfordia minima; Momipites punctatus; Momipites quietus; Monocolpopollenites tranquillus; Nepenthes-type; Nudopollis terminalis; Nyssapollenites kruschi; ORDINAL NUMBER; OUTCROP; Outcrop sample; Ovoidites sp.; Pentapollenites pentangulus; Pityosporites labdacus; Planctonites stellarius; Platycaryapollenites spp.; Plicapollis pseudoexcelsus; Plicatopollis plicatus; Pollen, tricolporate undifferentiated; pollen analytical standard techniques (Faegri & Iversen, 1989, Textbook Pollen); Polypodiaceoisporites sp.; Polyporopollenites spp.; Pompeckjoidaepollenites subhercynicus; Porocolpopollenites rarobaculatus; Porocolpopollenites sp.; Prasinophytes; Psilodiporites iszkaszentgyoergyi; Pterocaryapollenites stellatus; Punctilongisulcites microechinatus; Reticulataepollis intergranulatus; Sparganiaceaepollenites sp.; Spinaepollis spinosus; Spinizonocolpites spp.; Spores, trilete undifferentiated; Stereisporites sp.; Subtriporopollenites anulatus; Subtriporopollenites constans; sum spores; Tegumentisporis sp.; Tetracolporopollenites spp.; Thomsonipollis magnificus; Triatriopollenites bituitus; Triatriopollenites excelsus; Triatriopollenites rurensis; Tricolpopollenites asper; Tricolpopollenites liblarensis; Tricolpopollenites microhenrici; Tricolpopollenites quisqualis; Tricolpopollenites retiformis; Tricolpopollenites vegetus; Tricolporopollenites cingulum; Tricolporopollenites crassiexinus; Tricolporopollenites edmundii; Tricolporopollenites eofagoides; Tricolporopollenites mansfeldensis; Tricolporopollenites marcodurensis; Tricolporopollenites megaexactus; Tricolporopollenites messelensis; Tricolporopollenites microporitus; Tricolporopollenites microreticulatus; Tricolporopollenites parmularius; Tricolporopollenites pseudocingulum; Tricolporopollenites satzveyensis; Tricolporopollenites sole de portai; Tricolporopollenites sp.; Tricolporopollenites vancampoae; Triporopollenites coryloides; Triporopollenites rhenanus; Triporopollenites robustus; Varia; Verrucatosporites favus; Zonocostites ramonae
    Type: Dataset
    Format: text/tab-separated-values, 2820 data points
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  • 2
    Publication Date: 2023-11-28
    Keywords: Average chain length; Fichtelite; Identification; Lithologic unit/sequence; Lithology/composition/facies; Lower Saxony, Germany; n-Alkane, C23/C31 ratio; OUTCROP; Outcrop sample; Ratio; Schoningen
    Type: Dataset
    Format: text/tab-separated-values, 272 data points
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  • 3
    Publication Date: 2024-04-25
    Description: We analyzed 10 samples from the FB2001 depth interval 10-9 m for their Total Organic Carbon (TOC) content. This new data set is supplementary to the existing TOC record of Bauersachs et al. (2014) for the depth interval 145-1 m of the same core. The new samples were measured due to low spatial resolution of the existing TOC data set (~two samples per meter; Bauersachs et al., 2014; doi:10.1016/j.palaeo.2014.06.015) relative to the gamma-ray data (~10 data points per meter), and thus allow for a same-resolution assessment of the gamma-ray/TOC relationship. For the TOC measurements we followed the protocol of Bauersachs et al. (2014). In short, the dried and powdered sediment samples (ca. 30 mg) were pretreated with excess 2M hydrochloric acid (HCl) to remove carbonates, neutralized with distilled water, and again dried at 50 °C for 24 h. Subsequently, samples were measured in duplicates using a CS-Analyser 144DR (Leco Coopeation) at the Institute of Earth Sciences at Heidelberg University with a sample reproducibility of 〈 0.5%.
    Keywords: AGE; Astrochronology; borehole logging data; Calculated, according to Kaboth-Bahr et al. (2024); Carbon, organic, total; DEPTH, sediment/rock; FB2001; Geochemical proxies; Hydraulic rotary drilling; Messel, Germany; middle Eocene; Sulfur/Carbon Analyzer, LECO Corporation, SC-144DR
    Type: Dataset
    Format: text/tab-separated-values, 172 data points
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