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GEOMAR Library Ocean Research Information Access

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  • 1
    Publication Date: 2024-04-19
    Description: The late Quaternary history of Sumatra has experienced relatively little attention compared to that of the other large islands in the Indonesian archipelago. The first reports of fossils from the island date to the 1880s; they were discovered largely through the efforts of Dubois in the caves of the Padang Highlands. Following these efforts, focus shifted in the 1920s and 1930s to the archaeological records of the midden deposits of northern Sumatra and the Hoabinhian cultures preserved therein. There was little new fieldwork between 1940 and 1970, but by the mid-1970s several new campaigns seemed to herald a renewed interest in the history and prehistory of the island. This enthusiasm does not appear to have been sustained, however, and work was intermittent again in the 1980s and 1990s. Beginning in the mid-1990s and extending into the first two decades of the twenty-first century, more work at existing sites and new investigations have both taken place, extending our knowledge of both the deep-time and more recent history of the island. The application of new techniques on existing sites and the exploration and excavation of new sites are making an increasingly significant contribution to understanding the role of Sumatra in human biological and cultural evolution.
    Keywords: Hoabinhian ; Dubois ; van Stein Callenfels ; caves ; fossils ; history of archaeology ; sumatralith
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/other
    Format: application/pdf
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  • 2
    Publication Date: 2024-05-22
    Description: Carbon dioxide removal (CDR) is discussed for offsetting residual greenhouse gas emissions or even reversing climate change. All emissions scenarios of the Intergovernmental Panel on Climate Change that meet the ‘well below 2 °C’ warming target of the Paris Agreement include CDR. Ocean alkalinity enhancement (OAE) may be one possible CDR where the carbon uptake of the ocean is increased by artificial alkalinity addition. Here, we investigate the effect of OAE on modelled carbon reservoirs and fluxes in two observationally-constrained large perturbed parameter ensembles. OAE is assumed to be technically successful and deployed as an additional CDR in the SSP5-3.4 temperature overshoot scenario. Tradeoffs involving feedbacks with atmospheric CO 2 result in a low efficiency of an alkalinity-driven atmospheric CO 2 reduction of −0.35 [−0.37 to −0.33] mol C per mol alkalinity addition (skill-weighted mean and 68% c.i.). The realized atmospheric CO 2 reduction, and correspondingly the efficiency, is more than two times smaller than the direct alkalinity-driven enhancement of ocean uptake. The alkalinity-driven ocean carbon uptake is partly offset by the release of carbon from the land biosphere and a reduced ocean carbon sink in response to lowered atmospheric CO 2 under OAE. In a second step we use the Bern3D-LPX model in CO 2 peak-decline simulations to address hysteresis and temporal lags of surface air temperature change (ΔSAT) in an idealized scenario where ΔSAT increases to ~2 °C and then declines to ~1.5 °C as result of CDR. ΔSAT lags the decline in CO 2 -forcing by 18 [14–22] years, depending close to linearly on the equilibrium climate sensitivity of the respective ensemble member. These tradeoffs and lags are an inherent feature of the Earth system response to changes in atmospheric CO 2 and will therefore be equally important for other CDR methods.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
    Format: text
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  • 3
    Publication Date: 2024-05-29
    Description: The spreading of crushed olivine-rich rocks in coastal seas to accelerate weathering reactions sequesters atmospheric CO2 and reduces atmospheric CO2 concentrations. Their weathering rates depend on different factors, including temperature and the reaction surface area. Therefore, this study investigates the variations in olivine-based enhanced weathering rates across 13 regional coasts worldwide. In addition, it assesses the CO2 sequestration within 100 years and evaluates the maximum net-sequestration potential based on varying environmental conditions. Simulations were conducted using the geochemical thermodynamic equilibrium modeling software PHREEQC. A sensitivity analysis was performed, exploring various combinations of influencing parameters, including grain size, seawater temperature, and chemistry. The findings reveal significant variation in CO2 sequestration, ranging from 0.13 to 0.94 metric tons (t) of CO2 per ton of distributed olivine-rich rocks over 100 years. Warmer coastal regions exhibit higher CO2 sequestration capacities than temperate regions, with a difference of 0.4 t CO2/t olivine distributed. Sensitivity analysis shows that smaller grain sizes (10 µm) exhibit higher net CO2 sequestration rates (0.87 t/t) in olivine-based enhanced weathering across all conditions, attributed to their larger reactive surface area. However, in warmer seawater temperatures, olivine with slightly larger grain sizes (50 and 100 µm) displays still larger net CO2 sequestration rates (0.97 and 0.92 t/t), optimizing the efficiency of CO2 sequestration while reducing grinding energy requirements. While relying on a simplified sensitivity analysis that does not capture the full complexity of real-world environmental dynamics, this study contributes to understanding the variability and optimization of enhanced weathering for CO2 sequestration, supporting its potential as a sustainable CO2 removal strategy.
    Type: Article , PeerReviewed
    Format: text
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