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  • PANGAEA  (345)
  • American Physical Society (APS)  (2)
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  • 1
    Publication Date: 2016-12-28
    Description: Author(s): Benedikt Scharf, Tobias Frank, Martin Gmitra, Jaroslav Fabian, Igor Žutić, and Vasili Perebeinos We theoretically investigate excitons in MoS 2 monolayers in an applied in-plane electric field. Tight-binding and Bethe-Salpeter equation calculations predict a quadratic Stark shift, of the order of a few meV for fields of 10 V/ μ m , in the linear absorption spectra. The spectral weight of the main e… [Phys. Rev. B 94, 245434] Published Tue Dec 27, 2016
    Keywords: Surface physics, nanoscale physics, low-dimensional systems
    Print ISSN: 1098-0121
    Electronic ISSN: 1095-3795
    Topics: Physics
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  • 2
    Publication Date: 2016-04-23
    Description: Author(s): Tobias Frank, Martin Gmitra, and Jaroslav Fabian We study orbital and spin-orbit proximity effects in graphene adsorbed to the Cu(111) surface by means of density functional theory (DFT). The proximity effects are caused mainly by the hybridization of graphene π and copper d orbitals. Our electronic structure calculations agree well with the exper… [Phys. Rev. B 93, 155142] Published Fri Apr 22, 2016
    Keywords: Electronic structure and strongly correlated systems
    Print ISSN: 1098-0121
    Electronic ISSN: 1095-3795
    Topics: Physics
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  • 3
    Publication Date: 2023-03-10
    Keywords: ANT-XXIII/1; ANT-XXIII/3; Bay of Biscay; Canarias Sea; CTD; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; GOFLO; Go-Flo bottles; Hafnium, dissolved; Latitude of event; Longitude of event; MC-ICP-MS, isotope dilution; Multi-collector inductively coupled plasma mass spectrometer (MC-ICP-MS); Neodymium, dissolved; Nitrate; Phosphate; Polarstern; PS69; PS69/003-1; PS69/006-1; PS69/011-1; PS69/018-1; PS69/021-1; PS69/026-1; PS69/140-2; PS69/224-1; Salinity; Silicate; South Atlantic Ocean; Temperature, water, potential; ε-Hafnium; ε-Hafnium, standard deviation; ε-Neodymium
    Type: Dataset
    Format: text/tab-separated-values, 310 data points
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  • 4
    Publication Date: 2023-03-10
    Keywords: BATS15m; Cerium, dissolved; CTD/Rosette; CTD-RO; DEPTH, water; Dysprosium, dissolved; Erbium, dissolved; Europium, dissolved; Gadolinium, dissolved; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; Holmium, dissolved; Lanthanum, dissolved; Lutetium, dissolved; Neodymium, dissolved; Praseodymium, dissolved; Samarium, dissolved; South Atlantic Ocean; Terbium, dissolved; Thulium, dissolved; Ytterbium, dissolved; Yttrium, dissolved
    Type: Dataset
    Format: text/tab-separated-values, 225 data points
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  • 5
    Publication Date: 2023-03-10
    Keywords: BATS2000m; Cerium, dissolved; CTD/Rosette; CTD-RO; DEPTH, water; Dysprosium, dissolved; Erbium, dissolved; Europium, dissolved; Gadolinium, dissolved; GEOTRACES; Global marine biogeochemical cycles of trace elements and their isotopes; Holmium, dissolved; Lanthanum, dissolved; Lutetium, dissolved; Neodymium, dissolved; Praseodymium, dissolved; Samarium, dissolved; South Atlantic Ocean; Terbium, dissolved; Thulium, dissolved; Ytterbium, dissolved; Yttrium, dissolved
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Rickli, Jörg Dominik; Frank, Martin; Halliday, Alex N (2009): The hafnium-neodymium isotopic composition of Atlantic seawater. Earth and Planetary Science Letters, 280(1-4), 118-127, https://doi.org/10.1016/j.epsl.2009.01.026
    Publication Date: 2023-03-10
    Description: The first full water column hafnium isotopic compositions of Atlantic seawater have been obtained at seven locations from the Labrador Sea to the Drake Passage. Despite subpicomolar concentrations in seawater, a precision of the Hf isotopic measurements of 〈0.7 epsilon-Hf units was achieved. An overall epsilon-Hf range between -3.1 in the Labrador Sea and +4.4 in Antarctic bottom water was determined, the distribution of which broadly reflects continental weathering inputs. Within particular water column profiles, significant differences of up to 4 epsilon-Hf units occur. Combined with Nd isotope data of the same samples, it is evident that the Hf isotopic composition of seawater is too radiogenic for a given Nd isotopic composition and that the largest difference between expected and measured Hf isotopic compositions in seawater occurs near the oldest continental crust in the Labrador Sea. This corroborates the previous proposition, which was mainly based on ferromanganese crust data, that the Hf isotopic composition of seawater is controlled by incongruent weathering of continental crust and possibly, to some extent, by hydrothermal contributions. Hafnium concentrations in the ocean do not increase along the deep ocean conveyer indicating an oceanic residence time of only a few hundred years, which is significantly shorter than previously assumed. The Hf isotopic composition of past seawater can therefore serve as a proxy for short distance, basin scale mixing processes and the regime and intensity of nearby continental weathering processes.
    Keywords: ANT-XXIII/1; ANT-XXIII/3; Bay of Biscay; Canarias Sea; CTD/Rosette; CTD-RO; GOFLO; Go-Flo bottles; Polarstern; PS69; PS69/003-1; PS69/006-1; PS69/011-1; PS69/018-1; PS69/021-1; PS69/026-1; PS69/140-2; PS69/224-1; South Atlantic Ocean; Tha15; Thalassa; WNA05; WNA05_15
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    Publication Date: 2023-03-02
    Keywords: 302-CompSite; Age, comment; Age model; Age model, composite; Arctic Coring Expedition, ACEX; Calculated, see reference(s); CCGS Captain Molly Kool (Vidar Viking); COMPCORE; Composite Core; DEPTH, sediment/rock; Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; Interval comments; IODP; Sample comment; Sedimentation rate
    Type: Dataset
    Format: text/tab-separated-values, 38 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Dausmann, Veit; Frank, Martin; Zieringer, Moritz (2020): Water mass mixing versus local weathering inputs along the Bay of Biscay: Evidence from dissolved hafnium and neodymium isotopes. Marine Chemistry, 224, 103844, https://doi.org/10.1016/j.marchem.2020.103844
    Publication Date: 2023-03-10
    Description: We present dissolved neodymium and hafnium concentrations and radiogenic isotope compositions of surface and deep-water masses from the Bay of Biscay. Neodymium isotope signatures in surface waters of the Bay of Biscay are dominated by local weathering inputs from the surrounding continental margin. Subsurface Eastern North Atlantic Central Water (ENACW) shows a distinct Nd isotope signature (εNd≅‑12.0) at the southwestern-most station and is significantly diluted by mixing with more radiogenic waters on its way north along the European margin. Furthermore, the Nd isotope data clearly show a declining fraction of Mediterranean Outflow Water (MOW) at intermediate depths on its way north indicating that only 40% to 60% of MOW still present in the mixture at the Galician margin arrive at the stations further north in the Bay of Biscay. A potentially seasonal variability of the flow path of MOW is identified when comparing the results of the Nd isotope compositions and salinity data of this study with those of earlier studies from the area. In agreement with Nd isotope and concentration analyses Hf isotope composition of MOW is affected by large-scale inputs of terrigenous material into the Mediterranean as can be deduced from elevated Hf concentrations at the Galician margin. Hf isotope signatures of all water masses of the Bay of Biscay, moreover, are overprinted by local weathering inputs and do not reflect water mass mixing. However, combined dissolved Nd and Hf isotopes serve as a useful indicator of local weathering influences on signatures expected from long distance admixture.
    Keywords: Area/locality; Bay of Biscay; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; Hafnium, dissolved; Hafnium-176/Hafnium-177; Hafnium-176/Hafnium-177, standard deviation; Latitude of event; Longitude of event; M84/5; M84/5_559; M84/5_560; M84/5_576; M84/5_577; M84/5_589; M84/5_611; M84/5_612; M84/5_615; M84/5_624; M84/5_625; M84/5_635; M84/5_638; M84/5_639; M84/5_666; M84/5_SW01; M84/5_SW02; M84/5_SW03; M84/5_SW04; M84/5_SW05; M84/5_SW06; Membrane pump; Meteor (1986); MP; Neodymium, dissolved; Salinity; South Atlantic Ocean; Temperature, water; Volume; ε-Hafnium; ε-Hafnium, standard deviation; ε-Neodymium; ε-Neodymium, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 452 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Frank, Martin; Eckhardt, Joerg-Detlef; Eisenhauer, Anton; Kubik, Peter W; Dittrich-Hannen, Beate; Segl, Monika; Mangini, Augusto (1994): Beryllium 10, thorium 230, and protactinium 231 in Galapagos microplate sediments: Implications of hydrothermal activity and paleoproductivity changes during the last 100,000 years. Paleoceanography, 9(4), 559-578, https://doi.org/10.1029/94PA01132
    Publication Date: 2023-05-12
    Description: Biogenic particle fluxes from highly productive surface waters, boundary scavenging, and hydrothermal activity are the main factors influencing the deposition of radionuclides in the area of the Galapagos microplate, eastern Equatorial Pacific. In order to evaluate the importance of these three processes throughout the last 100 kyr, concentrations of the radionuclides 10Be, 230Th, and 231Pa, and of Mn and Fe were measured at high resolution in sediment samples from two gravity cores KLH 068 and KLH 093. High biological productivity in the surface waters overlying the investigated area has led to 10Be and 231Pa fluxes exceeding production during at least the last 30 kyr and probably the last 100 kyr. However, during periods of high productivity at the up welling centers off Peru and extension of the equatorial high-productivity zone, a relative loss of 10Be and 231Pa may have occurred in these sediment cores because of boundary scavenging. The effects of hydrothermal activity were investigated by comparing the 230Thex concentrations to the Mn/Fe ratios and by comparing the fluxes of 230Th and 10Be which exceed production. The results suggest an enhanced hydrothermal influence during isotope stages 4 and 5 and to a lesser extent during isotope stage 1 in core KLH 093. During isotope stages 2 and 3, the hydrothermal supply of Mn was deposited elsewhere, probably because of changes in current regime or deep water oxygenation. A strong increase of the Mn/Fe ratio at the beginning of climatic stage 1 which is not accompanied by an increase of the 230Thex concentration is interpreted to be an effect of Mn remobilization and reprecipitation in the sediment.
    Keywords: Equatorial East Pacific; HYMAS II; KAL; Kasten corer; KLH068; KLH093; SO60; SO60_68; SO60_93; Sonne
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 10
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    PANGAEA
    In:  Supplement to: Rühlemann, Carsten; Diekmann, Bernhard; Mulitza, Stefan; Frank, Martin (2001): Late Quaternary changes of western equatorial Atlantic surface circulation and Amazon lowland climate recorded in Ceara Rise deep-sea sediments. Paleoceanography, 16(3), 293-305, https://doi.org/10.1029/1999PA000474
    Publication Date: 2023-05-12
    Description: Today the western tropical Atlantic is the most important passage for cross-equatorial transfer of heat in the form of warm surface water flowing from the South into the North Atlantic. Circulation changes north of South America may thus have influenced the global thermohaline circulation system and high northern latitude climate. Here we reconstruct late Quaternary variations of western equatorial Atlantic surface circulation and Amazon lowland climate obtained from a multiproxy sediment record from Ceará Rise. Variations in the illite/smectite ratio suggest drier climatic conditions in the Amazon Basin during glacials relative to interglacials. The 230Thex-normalized fluxes and the 13C/12C record of organic carbon indicate that sea level fluctuations, shelf topography, and changes of the surface circulation pattern controlled variations and amplitude of terrigenous sediment supply to the Ceará Rise. We attribute variations in thermocline depth, reconstructed from vertical planktic foraminiferal oxygen isotope gradients and abundances of the phytoplankton species Florisphaera profunda, to changes in southeast trade wind intensity. Strong trade winds during ice volume maxima are associated with a deep western tropical Atlantic thermocline, strengthening of the North Brazil Current retroflection, and more vigorous eastward flow of surface waters.
    Keywords: GeoB; Geosciences, University of Bremen; SFB261; South Atlantic in Late Quaternary: Reconstruction of Budget and Currents
    Type: Dataset
    Format: application/zip, 4 datasets
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