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  • 2010-2014  (653,230)
  • 1950-1954  (4)
  • 2012  (653,230)
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Bouimetarhan, Ilham; Prange, Matthias; Schefuß, Enno; Dupont, Lydie M; Lippold, Jörg; Mulitza, Stefan; Zonneveld, Karin A F (2012): Sahel megadrought during Heinrich Stadial 1: evidence for a three-phase evolution of the low- and mid-level West African wind system. Quaternary Science Reviews, 58, 66-76, https://doi.org/10.1016/j.quascirev.2012.10.015
    Publication Date: 2024-05-27
    Description: Millennial-scale dry events in the Northern Hemisphere monsoon regions during the last Glacial period are commonly attributed to southward shifts of the Intertropical Convergence Zone (ITCZ) associated with an intensification of the northeasterly (NE) trade wind system during intervals of reduced Atlantic meridional overturning circulation (AMOC). Through the use of high-resolution last deglaciation pollen records from the continental slope off Senegal, our data show that one of the longest and most extreme droughts in the western Sahel history, which occurred during the North Atlantic Heinrich Stadial 1 (HS1), displayed a succession of three major phases. These phases progressed from an interval of maximum pollen representation of Saharan elements between ~19 and 17.4 kyr BP indicating the onset of aridity and intensified NE trade winds, followed by a millennial interlude of reduced input of Saharan pollen and increased input of Sahelian pollen, to a final phase between ~16.2 and 15 kyr BP that was characterized by a second maximum of Saharan pollen abundances. This change in the pollen assemblage indicates a mid-HS1 interlude of NE trade wind relaxation, occurring between two distinct trade wind maxima, along with an intensified mid-tropospheric African Easterly Jet (AEJ) indicating a substantial change in West African atmospheric processes. The pollen data thus suggest that although the NE trades have weakened, the Sahel drought remained severe during this time interval. Therefore, a simple strengthening of trade winds and a southward shift of the West African monsoon trough alone cannot fully explain millennial-scale Sahel droughts during periods of AMOC weakening. Instead, we suggest that an intensification of the AEJ is needed to explain the persistence of the drought during HS1. Simulations with the Community Climate System Model indicate that an intensified AEJ during periods of reduced AMOC affected the North African climate by enhancing moisture divergence over the West African realm, thereby extending the Sahel drought for about 4000 years.
    Keywords: 293; Center for Marine Environmental Sciences; GeoB9508-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 2
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    PANGAEA
    In:  Supplement to: Daniau, Anne-Laure; Bartlein, Patrick J; Harrison, S P; Prentice, Iain Colin; Brewer, Simon; Friedlingstein, Pierre; Harrison-Prentice, T I; Inoue, J; Izumi, K; Marlon, Jennifer R; Mooney, Scott D; Power, Mitchell J; Stevenson, J; Tinner, Willy; Andric, M; Atanassova, J; Behling, Hermann; Black, M; Blarquez, O; Brown, K J; Carcaillet, C; Colhoun, Eric A; Colombaroli, Daniele; Davis, Basil A S; D'Costa, D; Dodson, John; Dupont, Lydie M; Eshetu, Z; Gavin, D G; Genries, A; Haberle, Simon G; Hallett, D J; Hope, Geoffrey; Horn, S P; Kassa, T G; Katamura, F; Kennedy, L M; Kershaw, A Peter; Krivonogov, S; Long, C; Magri, Donatella; Marinova, E; McKenzie, G Merna; Moreno, P I; Moss, Patrick T; Neumann, F H; Norstrom, E; Paitre, C; Rius, D; Roberts, Neil; Robinson, G S; Sasaki, N; Scott, Louis; Takahara, H; Terwilliger, V; Thevenon, Florian; Turner, R; Valsecchi, V G; Vannière, Boris; Walsh, M; Williams, N; Zhang, Yancheng (2012): Predictability of biomass burning in response to climate changes. Global Biogeochemical Cycles, 26(4), https://doi.org/10.1029/2011GB004249
    Publication Date: 2024-05-27
    Description: We analyze sedimentary charcoal records to show that the changes in fire regime over the past 21,000 yrs are predictable from changes in regional climates. Analyses of paleo- fire data show that fire increases monotonically with changes in temperature and peaks at intermediate moisture levels, and that temperature is quantitatively the most important driver of changes in biomass burning over the past 21,000 yrs. Given that a similar relationship between climate drivers and fire emerges from analyses of the interannual variability in biomass burning shown by remote-sensing observations of month-by-month burnt area between 1996 and 2008, our results signal a serious cause for concern in the face of continuing global warming.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2024-05-27
    Keywords: 293; Acacia; AGE; Alchornea; Amaranthaceae; Annonaceae; Artemisia; Asteroideae; Balanites; Borreria; Boscia-type; Butyrospermum; Caryophyllaceae; Cassia-type; Celtis; Center for Marine Environmental Sciences; Clematis; Combretaceae; Counting, palynology; Cuviera; Cyperaceae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Ephedra distachya-type; Ephedra fragilis-type; Euphorbia-type; Fraxinus; Galium; GeoB9508-5; Gramineae; Gravity corer (Kiel type); Indigofera; Lamnea; M65/1; MARUM; Meteor (1986); Mimosa-type; Mitracarpus; Olea; Phoenix-type; Piliostigma; Pinus; Pollen, total; Psydrax-type subcordatum; Pterocarpus-type; Rhamnaceae; Rhizophora; Rubiaceae; Sedimentation rate; SL; Stereospermum-type; Tamarindus-type indica; Typha; Uapaca; Vernonia-type; Ziziphus
    Type: Dataset
    Format: text/tab-separated-values, 1776 data points
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  • 4
    Publication Date: 2024-05-27
    Keywords: 293; Acacia; AGE; Algae; Amaranthaceae/Chenopodiaceae; Artemisia; Asteroideae; Balanites; Borreria; Boscia-type; Calculated, see reference(s); Caryophyllaceae; Celtis; Center for Marine Environmental Sciences; Clematis; Counting, palynology; Cuticles; Cyperaceae; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Ephedra distachya-type; Ephedra fragilis-type; Euphorbia-type; Fraxinus; Galium; GeoB9508-5; Gramineae; Gravity corer (Kiel type); Lycopodium; M65/1; MARUM; Mass; Meteor (1986); Mimosa-type; Mitracarpus; Olea; Pinus; Pollen, total; Pollen and spores; Psydrax-type subcordata; Rhamnaceae; Rhizophora; Rubiaceae; Sedimentation rate; SL; Spores; Sporomorphes, total; Typha; Uapaca; Vernonia-type; Volume; Ziziphus
    Type: Dataset
    Format: text/tab-separated-values, 1352 data points
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  • 5
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    PANGAEA
    Publication Date: 2024-05-27
    Keywords: 175-1078C; Age model; Age model calibration; Benguela Current, South Atlantic Ocean; Center for Marine Environmental Sciences; Charcoal; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg175; MARUM; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 213 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Li, Wei; Gao, Kunshan; Beardall, John (2012): Interactive Effects of Ocean Acidification and Nitrogen-Limitation on the Diatom Phaeodactylum tricornutum. PLoS ONE, 7(12), e51590, https://doi.org/10.1371/journal.pone.0051590
    Publication Date: 2024-05-27
    Description: Climate change is expected to bring about alterations in the marine physical and chemical environment that will induce changes in the concentration of dissolved CO2 and in nutrient availability. These in turn are expected to affect the physiological performance of phytoplankton. In order to learn how phytoplankton respond to the predicted scenario of increased CO2 and decreased nitrogen in the surface mixed layer, we investigated the diatom Phaeodactylum tricornutum as a model organism. The cells were cultured in both low CO2 (390 µatm) and high CO2 (1000 µatm) conditions at limiting (10 µmol/L) or enriched (110 µmol/L) nitrate concentrations. Our study shows that nitrogen limitation resulted in significant decreases in cell size, pigmentation, growth rate and effective quantum yield of Phaeodactylum tricornutum, but these parameters were not affected by enhanced dissolved CO2 and lowered pH. However, increased CO2 concentration induced higher rETRmax and higher dark respiration rates and decreased the CO2 or dissolved inorganic carbon (DIC) affinity for electron transfer (shown by higher values for K1/2 DIC or K1/2 CO2). Furthermore, the elemental stoichiometry (carbon to nitrogen ratio) was raised under high CO2 conditions in both nitrogen limited and nitrogen replete conditions, with the ratio in the high CO2 and low nitrate grown cells being higher by 45% compared to that in the low CO2 and nitrate replete grown ones. Our results suggest that while nitrogen limitation had a greater effect than ocean acidification, the combined effects of both factors could act synergistically to affect marine diatoms and related biogeochemical cycles in future oceans.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Bicarbonate ion; Bicarbonate ion, standard deviation; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, reciprocal of photosynthetic affinity value; Carbon, inorganic, dissolved, reciprocal of photosynthetic affinity value, standard deviation; Carbon, inorganic, dissolved, standard deviation; Carbon, organic, particulate, per cell; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, reciprocal of photosynthetic affinity value; Carbon dioxide, reciprocal of photosynthetic affinity value, standard deviation; Carbon dioxide, standard deviation; Carotenoids, standard deviation; Carotenoids per cell; Cell biovolume; Cell biovolume, standard deviation; Cell counts, percent of total; Cell counts, standard deviation; Cell size; Cell size, standard deviation; Chlorophyll a, standard deviation; Chlorophyll a per cell; Chlorophyll c, standard deviation; Chlorophyll c per cell; Chromista; Coulometric titration; Effective quantum yield; Effective quantum yield, standard deviation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Identification; Laboratory experiment; Laboratory strains; Macro-nutrients; Maximal electron transport rate, relative; Maximal electron transport rate, relative, standard deviation; Maximum photochemical quantum yield of photosystem II; Maximum photochemical quantum yield of photosystem II, standard deviation; Nitrogen, organic, particulate, per cell; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Ochrophyta; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate organic carbon content per cell, standard deviation; Particulate organic nitrogen per cell, standard deviation; pH; pH, standard deviation; Phaeodactylum tricornutum; Photochemical efficiency; Photochemical efficiency, standard deviation; Phytoplankton; Potentiometric; Primary production/Photosynthesis; Respiration; Respiration rate, oxygen, per cell; Respiration rate, oxygen, per chlorophyll a; Respiration rate, oxygen, standard deviation; Salinity; Single species; Species; Spectrophotometric; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 29292 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Müller, Marius N; Beaufort, Luc; Bernard, O; Pedrotti, Maria Luiza; Talec, A; Sciandra, Antoine (2012): Influence of CO2 and nitrogen limitation on the coccolith volume of Emiliania huxleyi (Haptophyta). Biogeosciences, 9(10), 4155-4167, https://doi.org/10.5194/bg-9-4155-2012
    Publication Date: 2024-05-27
    Description: Coccolithophores, a key phytoplankton group, are one of the most studied organisms regarding their physiological response to ocean acidification/carbonation. The biogenic production of calcareous coccoliths has made coccolithophores a promising group for paleoceanographic research aiming to reconstruct past environmental conditions. Recently, geochemical and morphological analyses of fossil coccoliths have gained increased interest in regard to changes in seawater carbonate chemistry. The cosmopolitan coccolithophore Emiliania huxleyi (Lohm.) Hay and Mohler was cultured over a range of pCO2 levels in controlled laboratory experiments under nutrient replete and nitrogen limited conditions. Measurements of photosynthesis and calcification revealed, as previously published, an increase in particulate organic carbon production and a moderate decrease in calcification from ambient to elevated pCO2. The enhancement in particulate organic carbon production was accompanied by an increase in cell diameter. Changes in coccolith volume were best correlated with the coccosphere/cell diameter and no significant correlation was found between the coccolith volume and the particulate inorganic carbon production. The conducted experiments revealed that the coccolith volume of E. huxleyi is variable with aquatic CO2 concentration but its sensitivity is rather small in comparison with its sensitivity to nitrogen limitation. Comparing coccolith morphological and geometrical parameters like volume, mass and size to physiological parameters under controlled laboratory conditions is an important step to understand variations in fossil coccolith geometry.
    Keywords: -; Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Bicarbonate ion; Bicarbonate ion, standard deviation; BIOACID; Biological Impacts of Ocean Acidification; Bottles or small containers/Aquaria (〈20 L); Calcification/Dissolution; Calcite saturation state; Calcite saturation state, standard deviation; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, particulate, production per cell; Carbon, organic, particulate, production per cell; Carbon, organic, particulate/Nitrogen, particulate ratio; Carbon, organic, particulate/Phosphorus, organic, particulate ratio; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, partial pressure; Carbon dioxide, partial pressure, standard deviation; Carbon dioxide, standard deviation; Cell biovolume; Cell density; Cell density, standard deviation; Cell size; Cell size, standard deviation; Chromista; Coccoliths, other, diameter; Code; Description; Emiliania huxleyi; Experiment; Experimental treatment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gene expression (incl. proteomics); Growth/Morphology; Growth rate; Growth rate, standard deviation; Haptophyta; Laboratory experiment; Laboratory strains; Macro-nutrients; Nitrogen, total, particulate/Phosphorus, organic, particulate, ratio; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Particulate inorganic carbon, production, standard deviation; Particulate inorganic carbon/particulate organic carbon ratio; Particulate inorganic carbon/particulate organic carbon ratio, standard deviation; Particulate organic carbon, production, standard deviation; Pelagos; pH; pH, standard deviation; Phosphorus, organic, particulate, production per cell; Phytoplankton; Primary production/Photosynthesis; Salinity; Single species; Species; Standard deviation; Temperature, standard deviation; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 397 data points
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  • 8
    Publication Date: 2024-05-27
    Keywords: 293; AGE; Center for Marine Environmental Sciences; Depth, reference; DEPTH, sediment/rock; GeoB9508-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); see reference(s); SL; Thorium-230 excess; Thorium-230 excess, standard deviation; Vertical rain rate
    Type: Dataset
    Format: text/tab-separated-values, 77 data points
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  • 9
    Publication Date: 2024-05-27
    Keywords: 175-1078C; Acacia; Adenia; Afzelia; AGE; Alchornea; Alisma plantago-aquatica; Amaranthaceae/Chenopodiaceae; Anemia; Annonaceae; Anthoceros; Anthospermum; Avicennia; Balanites; Basella; Benguela Current, South Atlantic Ocean; Blighia-type; Botryococcus; Brachystegia; Bridelia; Burkea; Buxus-type madagascaria; Canthium spp.; Canthium subcordatum; Caryophyllaceae; Cassia-type; Celastraceae/Hippocrateaceae; Celtis; Cnestis-type; Coccinia; Colophospermum mopane; Combretaceae/Melastomataceae; Corymbium-type; Cotula-type; Counting, palynology; Crudia-type; Cussonia; Cyperaceae; Daisy-type; Daniellia-type; Dialium-type; Diospyros; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Erica (Africa); Erythrina; Euphorbia; Fabaceae; Funtumia; Gazania-type; Geraniaceae; Geranium; Glomus; Hermannia; Hygrophila-type; Hymenocardia; Hypoestes type; Hyptis; Ilex cf.. mitis; Indigofera-type; Ipomoea-type; Isoberlinia-type; Joides Resolution; Justicia/Monechma; Kohautia; Lannea; Leg175; Liguliflorea-type; Liverwort; Maerua-type; Mallotus; Marker, added; Marker, found; Meliaceae; Monolete spore(s); Myrica; Myrsine africana; Nitraria; Ocean Drilling Program; ODP; Olea; Pelargonium; Pentzia-type; Pericopsis; Pheoceros; Phyllanthus; Poaceae; Podocarpus; Pollen, total; Pollen indeterminata; Polygonum senegalense-type; Protea; Pteris; Pyrite; Rhizophora; Rhus-type; Rothmannia; Sample code/label; Sapotaceae; Securinega; Sedimentation rate; Sherbournea; Spermacoce; Spindel; Spores, trilete; Stipularia africana; Stoebe-type; Tarchonanthus/Artemisia-type; Tephrosia; Tetrorchidium; Thymelaeaceae; Tribulus; Tubuliflorae-type; Typha spp.; Uapaca; Urticaceae; Varia; Vernonia-type; Zanthoxylum
    Type: Dataset
    Format: text/tab-separated-values, 12995 data points
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  • 10
    Publication Date: 2024-05-27
    Keywords: 293; AGE; Calculated; Center for Marine Environmental Sciences; GeoB9508-5; Gravity corer (Kiel type); M65/1; MARUM; Meteor (1986); SL; Thorium-230 excess; Thorium-230 excess, standard deviation; Vertical rain rate
    Type: Dataset
    Format: text/tab-separated-values, 72 data points
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