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  • 2015-2019  (54)
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  • 11
    Publication Date: 2017-05-07
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
    Location Call Number Limitation Availability
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  • 12
    Publication Date: 2017-06-18
    Description: We investigate the redistribution of terrigenous materials in the northeastern (NE) South American continental margin during slowdown events of the Atlantic Meridional Overturning Circulation (AMOC). The compilation of stratigraphic data from 108 marine sediment cores collected across the western tropical Atlantic shows an extreme rise in sedimentation rates off the Parnaíba River mouth (about 2◦S) during Heinrich Stadial 1 (HS1, 18–15 ka). Sediment core GeoB16206-1, raised offshore the Parnaíba River mouth, documents relatively constant 143 Nd/144 Nd values (expressed as εNd(0) ) throughout the last 30 ka. Whereas the homogeneous εNd(0) data support the input of fluvial sediments by the Parnaíba River from the same source area directly onshore, the increases in Fe/Ca, Al/Si and Rb/Sr during HS1 indicate a marked intensification of fluvial erosion in the Parnaíba River drainage basin. In contrast, the εNd(0) values from sediment core GeoB16224-1 collected off French Guiana (about 7◦N) suggest Amazon-sourced materials within the last 30 ka. We attribute the extremely high volume of terrigenous sediments deposited offshore the Parnaíba River mouth during HS1 to (i) an enhanced precipitation in the catchment region and (ii) a reduced North Brazil Current, which are both associated with a weakened AMOC.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 13
    Publication Date: 2022-05-26
    Description: © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Nature Communications 9 (2018): 121, doi:10.1038/s41467-017-02504-1.
    Description: Sediments in deep ocean trenches may contain crucial information on past earthquake history and constitute important sites of carbon burial. Here we present 14C data on bulk organic carbon (OC) and its thermal decomposition fractions produced by ramped pyrolysis/oxidation for a core retrieved from the 〉7.5 km-deep Japan Trench. High-resolution 14C measurements, coupled with distinctive thermogram characteristics of OC, reveal hemipelagic sedimentation interrupted by episodic deposition of pre-aged OC in the trench. Low δ13C values and diverse 14C ages of thermal fractions imply that the latter material originates from the adjacent margin, and the co-occurrence of pre-aged OC with intervals corresponding to known earthquake events implies tectonically triggered, gravity-flow-driven supply. We show that 14C ages of thermal fractions can yield valuable chronological constraints on sedimentary sequences. Our findings shed new light on links between tectonically driven sedimentological processes and marine carbon cycling, with implications for carbon dynamics in hadal environments.
    Description: This study is supported by Doc.Mobility Fellowship (P1EZP2_159064) (R.B.) from the Swiss National Science Foundation (SNSF). This work is also supported by SNF “CAPS-LOCK” project 200021_140850 (T.I.E.), by SNSF grant (133481) (M.S.), and Austrian Science Foundation (P 29678-N28) (M.S.).
    Keywords: Carbon cycle ; Sedimentology
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 14
    Publication Date: 2022-05-26
    Description: Nordic Seas sedimentation data file, v. 2
    Description: Records from ten Aanderaa current meters deployed along with 5 current meter/sediment trap mooring arrays in the Fram Strait and Greenland Basin, each deployed for approximately one year between 1983 and 1986, are presented in this data file. Data included are current vectors, temperatures, frequency spectra, and two- and three-dimensional vector diagrams.
    Description: Funding was provided by the Office of Naval Research under Grant Number N00014-85-C-0001.
    Keywords: Ocean currents
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: application/pdf
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  • 15
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    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2023-03-16
    Keywords: ANT-IV/2; Calculated; Course; CT; DATE/TIME; LATITUDE; LONGITUDE; Polarstern; PS08; PS08/2-track; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 7124 data points
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  • 16
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    PANGAEA
    In:  Supplement to: Zhao, X; Dupont, Lydie M; Schefuß, Enno; Meadows, Michael E; Hahn, A; Wefer, Gerold (2016): Holocene vegetation and climate variability in the winter and summer rainfall zones of South Africa. The Holocene, 26(6), 843-857, https://doi.org/10.1177/0959683615622544
    Publication Date: 2023-03-03
    Description: To better understand Holocene vegetation and hydrological changes in South Africa, we analyzed pollen and microcharcoal records of two marine sites GeoB8331 and GeoB8323 from the Namaqualand mudbelt offshore the west coast of South Africa covering the last 9900 and 2200 years, respectively. Our data corroborate findings from literature that climate developments apparently contrast between the summer rainfall zone (SRZ) and winter rainfall zone (WRZ) over the last 9900 years, especially during the early and middle Holocene. During the early Holocene (9900-7800 cal.yr BP), a minimum of grass pollen suggests low summer rainfall in the SRZ, and the initial presence of Renosterveld vegetation indicates relatively wet conditions in the WRZ. Towards the middle Holocene (7800-2400 cal. yr BP), a rather moist savanna/grassland rich in grasses suggests higher summer rainfall in the SRZ resulting from increased austral summer insolation and a decline of fynbos vegetation accompanied by an increasing Succulent Karoo vegetation in the WRZ possibly suggests a southward shift of the Southern Hemisphere westerlies. During the last 2200 years, a trend towards higher aridity was observed for the SRZ, while the climate in the WRZ remained relatively stable. The Little Ice Age (ca. 700-200 cal. yr BP) was rather cool in both rainfall zones and drier in the SRZ while wetter in the WRZ.
    Keywords: Center for Marine Environmental Sciences; MARUM; RAiN; Regional Archives for Integrated iNvestigations
    Type: Dataset
    Format: application/zip, 8 datasets
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  • 17
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    PANGAEA
    In:  Supplement to: Grimmer, Friederike; Dupont, Lydie M; Lamy, Frank; Jung, Gerlinde; González, Catalina; Wefer, Gerold (2018): Early Pliocene vegetation and hydrology changes in western equatorial South America. Climate of the Past, 14(11), 1739-1754, https://doi.org/10.5194/cp-14-1739-2018
    Publication Date: 2023-03-03
    Description: Vegetation and climate change in nortwestern South America were studied using pollen analysis in combination with XRF scanning on marine sediments of ODP Site 1239 from the East Equatorial Pacific comprising the interval between 4.7 and 4.2 Ma. The study site is sensitive to latitudinal shifts of the Intertropical Convergence Zone (ITCZ) shifts insofar as a southward (northward) shift would result in increased (decreased) precipitation over Ecuador. The presented pollen record (46 samples) comprises representatives from five ecological groups: lowland rainforest, lower montane forest, upper montane forest, páramo, and broad range taxa. A broad tropical rainforest coverage persisted in the study area throughout the early Pliocene, without significant open vegetation below the forest line. Between 4.7 and 4.42 Ma, humidity increases, reaching its peak around 4.42 Ma, and slightly decreasing again afterwards. The stable, permanently humid conditions are rather in agreement with paleoceanographic data indicating a southward shift of the ITCZ, possibly in response to closure of the Central American Seaway. The presence of páramo vegetation indicates that the Western Cordillera of the northern Andes had already reached considerable elevation by the early Pliocene. The trend in iron/potassium-ratios (Fe/K) is similar to the pattern of humidity inferred from the pollen spectrum, showing the highest values around 4.46 Ma, thus supporting the hydrological interpretation of the pollen record.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 18
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    PANGAEA
    In:  Supplement to: Zhang, Yancheng; Chiessi, Cristiano Mazur; Mulitza, Stefan; Zabel, Matthias; Trindade, Ricardo F; Hollanda, Maria Helena B M; Dantas, Elton L; Govin, Aline; Tiedemann, Ralf; Wefer, Gerold (2015): Origin of increased terrigenous supply to the NE South American continental margin during Heinrich Stadial 1 and the Younger Dryas. Earth and Planetary Science Letters, 432, 493-500, https://doi.org/10.1016/j.epsl.2015.09.054
    Publication Date: 2023-06-15
    Description: We investigate the redistribution of terrigenous materials in the northeastern (NE) South American continental margin during slowdown events of the Atlantic Meridional Overturning Circulation (AMOC). The compilation of stratigraphic data from 108 marine sediment cores collected across the western tropical Atlantic shows an extreme rise in sedimentation rates off the Parnaíba River mouth (about 2°S) during Heinrich Stadial 1 (HS1, 18-15 ka). Sediment core GeoB16206-1, raised offshore the Parnaíba River mouth, documents relatively constant 143Nd/144Nd values (expressed as epsilonNd(0)) throughout the last 30 ka. Whereas the homogeneous epsilonNd(0) data support the input of fluvial sediments by the Parnaíba River from the same source area directly onshore, the increases in Fe/Ca, Al/Si and Rb/Sr during HS1 indicate a marked intensification of fluvial erosion in the Parnaíba River drainage basin. In contrast, the epsilonNd(0) values from sediment core GeoB16224-1 collected off French Guiana (about 7°N) suggest Amazon-sourced materials within the last 30 ka. We attribute the extremely high volume of terrigenous sediments deposited offshore the Parnaíba River mouth during HS1 to (i) an enhanced precipitation in the catchment region and (ii) a reduced North Brazil Current, which are both associated with a weakened AMOC.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Limitation Availability
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  • 19
    Publication Date: 2023-06-15
    Keywords: BP-102; BP-103; BP-104A; BP-105; BP-106; BP-107; BP-109A2; BP-135; BP-136; BP-137; BP-138; BP-141; BP-142; BP-149; BP-150; BP-160; BP-163; BP-168; BP-170; BP-171; BP-172; BP-175; BP-176; BP-177; BP-179; BP-182; BP-184; BP-64; BP-65; BP-67; BP-68; BP-74; BP-75A; BP-75B; BP-80; BP-81A; BP-82E; BP-82F; BP-82G; BP-82I; BP-84A; BP-84B; BP-88; BP-89; BP-91; BP-92; BP-97; BP-98; BP-99; Calculated; Center for Marine Environmental Sciences; DEPTH, sediment/rock; Event label; MARUM; Parnaiba River; Reference/source; Stratigraphy; ε-Neodymium (0)
    Type: Dataset
    Format: text/tab-separated-values, 147 data points
    Location Call Number Limitation Availability
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  • 20
    Publication Date: 2023-06-15
    Keywords: Aluminium; Amazon; Amazonas_AM-08-05; Beni_AM-07-04; Beni_AM-07-09; Calcium; Center for Marine Environmental Sciences; Event label; Iron; Latitude of event; Longitude of event; Madeira_AM-05-15; Madeira_AM-06-35; Madeira_AM-06-38; Madeira_AM-06-43; Madeira_MAO_22b; Madeira_MAO_25c; Madeira_MAO_28c; Madeira_MAO_38; Madeira_MAO_42; Madeira_MAO_45; Madre_de_Dios_AM-07-14; Maranon_AM-08-24; Maranon_AM-08-33; MARUM; Negro; Negro_MAO_01; Negro_MAO_02f; Negro_MAO_03c; Negro_MAO_81; Negro_MAO_83; Negro_MAO_93; Number; Potassium; Reference/source; River; Silicon; Solimoes_AM-06-09; Solimoes_MAO_05d; Solimoes_MAO_10d; Solimoes_MAO_13d; Solimoes_MAO_72; Solimoes_MAO_77; Solimoes_MAO_80; Tapajos_STM_11; Tapajos_STM_13; Tapajos_STM_19; Tapajos_STM_24; Tapajos_STM_33; Tapajos_STM_37; Tapajos_STM_39; Titanium; Xingu_XA_01; Xingu_XA_19; Xingu_XA_23; Xingu_XA_26; Xingu_XA_28; Xingu_XA_39; Xingu_XA_49; Xingu_XA_53; Xingu_XA_73
    Type: Dataset
    Format: text/tab-separated-values, 414 data points
    Location Call Number Limitation Availability
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