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  • 1
    Electronic Resource
    Electronic Resource
    Oxford UK : Blackwell Science Ltd
    Freshwater biology 46 (2001), S. 0 
    ISSN: 1365-2427
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: 1. Food sources and trophic structure of the macroinvertebrate community along a longitudinal gradient were examined in a glacier stream of the Swiss Alps (Val Roseg). Analysis of multiple stable isotopes (δ13C and δ15N) and measurement of C : N ratios were used to differentiate between allochthonous and autochthonous organic matter.2. Although isotopic signatures of algae varied widely among sites and dates, it was possible to discriminate between allochthonous and autochthonous food sources using a site-specific approach.3. Dominant food sources of herbivorous invertebrates in all main channel sites were epilithic diatoms and the filamentous gold alga Hydrurus foetidus. Allochthonous organic matter was of some importance only in a groundwater-fed stream close to the floodplain margin.4. Seasonal changes in the δ13C signature of the macroinvertebrates corresponded with seasonal changes in δ13C of the gold alga H. foetidus. This indicated that the energy base remains autochthonous throughout the year.5. Because of limited food sources, feeding plasticity of the invertebrate community was high. Both grazers and shredders fed predominantly on algae, whereas gatherer-collectors seemed to be omnivorous.6. The overall enrichment of δ15N was 2.25‰ (r2=0.99) per trophic level. On a gradient from the glacier site to a downstream forested site trophic enrichment was constant but variation in δ15N within trophic levels decreased.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 428 (2004), S. 130-132 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In 1997–98, extreme El Niño climatic conditions in the tropical Pacific had severe consequences in Indonesia. A prolonged period of dry weather resulted in drought, and favoured the ensuing forest and peat fires (Fig. 1) that were among the largest of the past century. Massive ...
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1432-1157
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The oxidation and reduction that occur during early diagenesis of sediments has been studied in the interstitial waters of a rapidly accumulating sedimentary sequence from the Mediterranean margin of Spain. A series of reactions that are mediated by progressively lower free energy derived from oxidation of organic matter is evident in the sedimentary sequence. Iron and manganese are rapidly reduced. Phosphate and alkalinity maxima at a subbottom depth of 15 m indicate maximal organic matter degradation. Methane first appears at ∼20 m subbottom after sulfate is depleted, and its concentrations quickly climb.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2023-02-24
    Keywords: 339-U1390; AGE; Bottom water temperature; COMPCORE; Composite Core; Exp339; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Joides Resolution; Mediterranean Outflow; Salinity; Salinity, standard error; Temperature, water, standard error; Uvigerina mediterranea, δ18O; δ18O, ice volume effect; δ18O, seawater, reconstructed; δ18O, standard error; δ18O anomaly
    Type: Dataset
    Format: text/tab-separated-values, 455 data points
    Location Call Number Limitation Availability
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  • 5
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    Unknown
    PANGAEA
    In:  Supplement to: Fiskal, Annika; Deng, Longhui; Michel, Anja; Eickenbusch, Philip; Han, Xingguo; Lagostina, Lorenzo; Zhu, Rong; Sander, Michael; Schroth, Martin H; Bernasconi, Stefano M; Dubois, Nathalie; Lever, Mark A (2019): Effects of eutrophication on sedimentary organic carbon cycling in five temperate lakes. Biogeosciences, 16(19), 3725-3746, https://doi.org/10.5194/bg-16-3725-2019
    Publication Date: 2023-01-13
    Description: We sampled sediments from three water depths in five lakes in central Switzerland: Lake Lucerne, Lake Zurich, Lake Zug, Lake Baldegg, and Lake Greifen. All took place in June and July of 2016. Three sublittoral stations differing in water depth and bottom water O2 concentrations were sampled. Per each lake station, one 60-mm diameter and 3–4 150-mm diameter gravity cores (UWITEC, AT) were taken from boats or motorized platforms. The thin cores were used for analyses of radionuclides, X-ray fluorescence, grain size, and archiving (one-half). Wide cores were used as follows: the core with the least disturbed sediment surface was used for microsensor measurements (O2, pH). Sediment porewater samples were obtained by rhizons (0.2 μm pore size, Rhizosphere) from a designated core with pre-drilled holes that were taped during coring for analyses of dissolved anions and cations including redox sensitive elements. Sediment samples for cell counts, methane concentration analyses, and physical property determinations (porosity, bulk density, dry density, water content) were taken from a third core using sterile cut-off syringes. Samples for solid-phase carbon analyses (TOC, total inorganic carbon (TIC)) were also taken from this core.
    Type: Dataset
    Format: application/zip, 30 datasets
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  • 6
    Publication Date: 2023-01-30
    Keywords: climate; Clumped isotopes; Continental; Eocene; LATITUDE; Oxygen isotopes; Paleocene; siderite; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Vapour saturation pressure; Vapour saturation pressure, maximum; Vapour saturation pressure, minimum
    Type: Dataset
    Format: text/tab-separated-values, 60 data points
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  • 7
    Publication Date: 2023-01-30
    Keywords: Area/locality; Average temperature; climate; Clumped isotopes; Confidence value; Continental; DATE/TIME; Eocene; Isotopic fractionation factor; LATITUDE; Number; Offset; Oxygen isotopes; Paleocene; siderite; Time zone; Uncertainty; Δ47; Δ47, standard deviation; Δ47, uncertainty; Δ48 offset; Δ49; δ13C, siderite; δ18O, precipitation; δ18O, siderite
    Type: Dataset
    Format: text/tab-separated-values, 1975 data points
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  • 8
    Publication Date: 2023-01-30
    Keywords: Calcium carbonate; climate; Clumped isotopes; Continental; Eocene; Iron carbonate, siderite; Location; Magnesium carbonate, magnesite; Manganese carbonate; Microprobe; Oxygen isotopes; Paleocene; Sample ID; siderite
    Type: Dataset
    Format: text/tab-separated-values, 216 data points
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  • 9
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    Unknown
    PANGAEA
    In:  Supplement to: van Dijk, Joep; Ziegler, Martin; de Nooijer, Lennart Jan; Reichart, Gert-Jan; Xuan, Chuang; Ducassou, Emmanuelle; Bernasconi, Stefano M; Lourens, Lucas Joost (2018): A Saltier Glacial Mediterranean Outflow. Paleoceanography and Paleoclimatology, 33(2), 179-197, https://doi.org/10.1002/2017PA003228
    Publication Date: 2023-02-24
    Description: The state of Atlantic Meridional Overturning Circulation (AMOC) is influenced by both the strength and the location of the Mediterranean Outflow (MOW) plume in the Gulf of Cadiz. To evaluate the influence of MOW on AMOC over deglaciations, precise and accurate salinity and temperature reconstructions are needed. For this purpose, we measured Mg/Ca and clumped isotopes of several benthic foraminiferal species at IODP Site U1390 in the Gulf of Cadiz. The clumped isotope results of Cibicidoides pachyderma, Uvigerina mediterranea and Pyrgo spp. are consistent between species and record no significant difference in Glacial to Holocene DWT. Over the deglaciation, the Mg/Ca-based temperatures derived from U. mediterranea indicate three periods of MOW absence at site U1390. Mg/Ca-based temperatures of Hoeglundina elegans and C. pachyderma are on average 6 °C too cold when compared to the present core-top temperature, which we explain by a carbonate ion effect on these epibenthic species related to the high alkalinity of the MOW. Combining DWT estimates with the benthic oxygen isotope data and considering different relationships between seawater oxygen isotopes and salinity, we infer a salinity decrease of MOWby 3 to 8 units over the deglaciation, and 4 units during S1, accounting for the global d18O depletion due to the decrease in ice volume. Our findings confirm that the Mediterranean Sea accumulates excess salt during a glacial low stand, and suggest that this salt surged into the Atlantic over the deglaciation, presumably during HS1.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 9 datasets
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  • 10
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    Unknown
    PANGAEA
    In:  Eidgenössische Technische Hochschule Zürich | Supplement to: Ausín, Blanca; Haghipour, Negar; Wacker, Lukas; Voelker, Antje H L; Hodell, David A; Magill, Clayton; Looser, Nathan; Bernasconi, Stefano M; Eglinton, Timothy Ian (2019): Radiocarbon Age Offsets Between Two Surface Dwelling Planktonic Foraminifera Species During Abrupt Climate Events in the SW Iberian Margin. Paleoceanography and Paleoclimatology, 34(1), 63-78, https://doi.org/10.1029/2018PA003490
    Publication Date: 2023-02-12
    Description: Oxygen and Carbon isotope data from Globigerinoides ruber from sediment core SHAK06-5K. Between 6 and 12 specimens of G. ruber were measured with a Gas Bench II connected to a Delta V Plus isotope ratio mass spectrometer at the Stable Isotope Laboratory of Climate Geology, ETH Zurich. Calibration to the Vienna Pee Dee Belemnite (VPDB) scale was accomplished using two in‐house standards previously calibrated against the NBS‐18 and NBS‐19 international standards. The associated long‐term standard deviation is 〈0.07‰. This isotopic record was concluded to be affected by the coupled effect of bioturbation with changes in the abundance of G. ruber. We refer potential users to the published article.
    Keywords: DEPTH, sediment/rock; GC; Globigerinoides ruber, δ13C; Globigerinoides ruber, δ18O; Gravity corer; Mass spectrometer Delta V plus; planktonic foraminifera; G. ruber; Portuguese Margin; oxygen isotopes; carbon isotopes; Shackleton Sites; SHAK06-5K
    Type: Dataset
    Format: text/tab-separated-values, 280 data points
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