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  • 1
    Publication Date: 2024-06-17
    Description: Yedoma is a permafrost deposit widely distributed across the Arctic and found exclusively within the unglaciated regions in northern Siberia, Alaska, and the Yukon, which are the core regions of Beringia. Yedoma deposits accumulated during the late Pleistocene Stage and are characterized by their predominantly fine-grained texture and association with syngenetic perma-frost formation. The very high ground ice content is most commonly present as pore ice and wedge ice that formed contemporaneously with sediment deposition. In the last decade, research has transitioned from debates about the origin of the Yedoma deposits towards increasing attention on the large carbon and nitrogen pools in Yedoma, their vulnerability to thaw, and increasing mobilization as the climate has warmed across the Arctic. In addition to classical cryolithological and sedimentological research, new methods such as stable isotope paleoclimate reconstruction and ancient sedimentary DNA studies have been more widely applied to better understand the characteristics of Yedoma deposits and helped emphasize their value as archives of Quaternary climate and paleoecological conditions during Ice Age Beringia.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
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  • 2
    Publication Date: 2024-06-17
    Description: As global temperatures continue to rise, a key uncertainty of terrestrial carbon (C)–climate feedback is the rate of C loss upon abrupt permafrost thaw. This type of thawing—termed thermokarst—may in turn accelerate or dampen the response of microbial degradation of soil organic matter and carbon dioxide (CO2) release to climate warming. However, such impacts have not yet been explored in experimental studies. Here, by experimentally warming three thermo-erosion gullies in an upland thermokarst site combined with incubating soils from five additional thermokarst-impacted sites on the Tibetan Plateau, we investigate how warming responses of soil CO2 release would change upon upland thermokarst formation. Our results show that warming-induced increase in soil CO2 release is ~5.5 times higher in thermokarst features than the adjacent non-thermokarst landforms. This larger warming response is associated with the lower substrate quality and higher abundance of microbial functional genes for recalcitrant C degradation in thermokarst-affected soils. Taken together, our study provides experimental evidence that warming-associated soil CO2 loss becomes stronger upon abrupt permafrost thaw, which could exacerbate the positive soil C–climate feedback in permafrost-affected regions.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
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    Elsevier
    In:  EPIC3Earth and Planetary Science Letters, Elsevier, 640, pp. 118801-118801, ISSN: 0012-821X
    Publication Date: 2024-06-17
    Description: Carbon cycle models used to calculate the marine reservoir age of the non-polar surface ocean (called Marine20) out of IntCal20, the compilation of atmospheric C, have so far neglected a key aspect of the millennial-scale variability connected with the thermal bipolar seesaw: changes in the strength of the Atlantic meridional overturning circulation (AMOC) related to Dansgaard/Oeschger and Heinrich events. Here we implement such AMOC changes in the carbon cycle box model BICYCLE-SE to investigate how model performance over the last 55 kyr is affected, in particular with respect to available 14C and CO2 data. Constraints from deep ocean 14C data suggest that the AMOC in the model during Heinrich stadial 1 needs to be highly reduced or even completely shutdown. Ocean circulation and sea ice coverage combined are the processes that almost completely explain the simulated changes in deep ocean 14C age, and these are also responsible for a glacial drawdown of ∼60 ppm of atmospheric CO2. We find that the implementation of abrupt reductions in AMOC during Greenland stadials in the model setup that was previously used for the calculation of Marine20 leads to differences of less than ±100 14C yrs. The representation of AMOC changes therefore appears to be of minor importance for deriving non-polar mean ocean radiocarbon calibration products such as Marine20, where atmospheric carbon cycle variables are forced by reconstructions. However, simulated atmospheric CO2 exhibits minima during AMOC reductions in Heinrich stadials, in disagreement with ice core data. This mismatch supports previous suggestions that millennial-scale changes in CO2 were probably not driven directly by the AMOC, but rather by biological and physical processes in the Southern Ocean and by contributions from variable land carbon storage.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
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    Naturalis Biodiversity Center
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 65 no. 1, pp. 75-82
    Publication Date: 2024-06-17
    Description: In Peninsular Malaysia, Rafflesia is represented by seven species of which R. kerrii (and R. su-meiae) stands out distinctly from the other five. The other five species, R. azlanii, R. cantleyi, R. parvimaculata, R. sharifahhapsahiae and R. tuanku-halimii, are collectively close enough to each other to be referred to as the R. cantleyi complex after its first-described species, R. cantleyi. Pulau Tioman has a population of R. cantleyi, which, because of its island location, is isolated from the mainland complex. This study was conducted to determine morphological variation in a selected location in Pulau Tioman. Twelve flowers were studied with respect to characteristics such as wart (blotch) pattern on perianth lobes, warts (dots) on upper surface of the diaphragm, shape of the aperture, shape of processes and types of ramenta. These are the characters that have been used to define species in the R. cantleyi complex. The variation in the local Tioman population was compared with the variation in the R. cantleyi complex on the mainland, which is about the same magnitude. This supports the idea that R. cantleyi is a single highly polymorphic species and that the species that have been described in the R. cantleyi complex should be reduced to varieties.
    Keywords: Plant Science ; Ecology ; Evolution ; Behavior and Systematics ; morphology ; Pulau Tioman ; Rafflesia cantleyi complex ; variability
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 5
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    Naturalis Biodiversity Center
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 65 no. 2, pp. i-ix
    Publication Date: 2024-06-17
    Keywords: Plant Science ; Ecology ; Evolution ; Behavior and Systematics
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 6
    Publication Date: 2024-06-17
    Description: Die biosfratigraphische Aussagekraft organischwandiger Dinoflagella- tenzysten in Rupel-Sedimenten (Unter-Oligozän) des Mainzer Beckens wird anhand von Material aus fünf Kernbohrungen aus verschiedenen Ablagerungsräumen untersucht. Die Abfolge vom oberen Foraminiferenmergel bis in den unteren Schleichsand lässt sich durch das Aussetzen von Wetzeliella gochtii, Rhombodinium draco, Phtanoperidinium amomum, P. comatum, W. symmetrica und Enneadocysta pectiniformis in vier Abschnitte gliedern. Ein Vergleich mit Dinoflagellatenzysten-Zonierungen für den nordwesteuro- päischen Raum ergibt die größten Übereinstimmungen mit der Zonierung von Köthe (1990). Dies weist auf eine enge paläozeanographische Verbindung zwischen dem Main- zer Becken und dem nordwestdeutschen Tertiärbecken zur Zeit des Rupels hin.
    Description: Abstract: The biostratigraphic significance of organic-walled dinoflagellate cysts from Rupelian (Lower Oligocene) sediments of the Mainz Basin (Southwest Germany) is investigated. The study material is derived from five boreholes drilled in different depo- sitional environments. The investigated succession can be subdivided into four intervals based on the last appearance data of W etzeliella gochtii, Rhombodinium draco, Phtanope- ridinium amomum, P. comatum, W. symmetrica, and Enneadocysta pectiniformis. A comparison of dinoflagellate cyst ranges in the Mainz Basin with zonations from the Northwest European Tertiary Basin yields highest agreement with the zonation of Köthe (1990) which has been established for northern Germany. This indicates a close palae- oceanographic connection between the Mainz Basin and the Northwest European Ter- tiary Basin during Rupelian times.
    Description: research
    Keywords: ddc:560.47 ; Mainzer Becken ; Biostratigraphie ; Dinoflagellaten ; Oligozän
    Language: German
    Type: doc-type:article , publishedVersion
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  • 7
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-06-17
    Description: research
    Keywords: Naturschutz ; Land- und Wasserwirtschaft ; Tragfähige Kooperationsmodelle ; Hochwasserrückhaltebecken Salzderhelden
    Language: German
    Type: doc-type:book
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  • 8
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-06-17
    Description: research
    Keywords: Naturschutzzielen ; Historischer Heidebauernwirtschaft ; Landwirtschaft ; Sandböden
    Language: German
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  • 9
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-06-17
    Description: research
    Keywords: Biomasse ; Mikroorganismen ; Böden ; ökologisch ; Ackerflächen Nicaraguas
    Language: German
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  • 10
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-06-17
    Description: research
    Keywords: Methoden der Standorterkundung ; DGPS-gestützten Ackerbaus
    Language: German
    Type: doc-type:book
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