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  • 11
    Publikationsdatum: 2024-04-20
    Beschreibung: A thick lacustrine sediment succession in Lake Towuti, located on the island of Sulawesi, Indonesia, offers a unique opportunity to study the relationships between tropical environmental conditions, Fe-rich sediment transport and deposition, and biological and sediment diagenetic processes under variable redox conditions through time. Lake Towuti is located in the East Sulawesi Ophiolite, the third largest ophiolite in the world; several rivers drain into Lake Towuti and supply the lake with high abundances of Fe and other metals from the catchment. The Towuti Drilling Project (TDP) was conducted in 2015 to collect deeper drill-cores from the lake bottom. Over 1000 m of sediment core were recovered, the deepest reaching bedrock at 162.8 m below the lake floor. Major characteristics include basal sediments dominated by silts and sands, overlain by a 2.5 m thick woody peat layer at 100 m depth, reported here as meters composite depth (mcd), and an upper 100 m of alternating thinly bedded red and green clay-sized sediment with localized turbidites, tephras, and diatomaceous oozes. Here we present chemical and spectral data from a 100 m long drill core into lacustrine sediments from a mafic basin. We include the ICP-determined oxide abundances in weight percent of sediment samples and the reflectance spectra of the sediment samples from wavelengths 0.35-28 micrometers.
    Schlagwort(e): Binary Object; Binary Object (File Size); Binary Object (Media Type); COMPCORE; Composite Core; ICDP; International Continental Scientific Drilling Program; Lake Towuti, Sulawesi, Indonesia; sediment; spectra; TDP-TOW15-1; tropical lake
    Materialart: Dataset
    Format: text/tab-separated-values, 2 data points
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  • 12
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © The Author(s), 2018. This is the author's version of the work. It is posted here under a nonexclusive, irrevocable, paid-up, worldwide license granted to WHOI. It is made available for personal use, not for redistribution. The definitive version was published in Organic Geochemistry 125 (2018): 70-81, doi: 10.1016/j.orggeochem.2018.08.008.
    Beschreibung: Reconstructions of climate using leaf wax D/H ratios (δDwax) require accounting for the apparent isotopic fractionation (εapp) between plant source water and waxes. There have been conflicting publications on whether plants in the Arctic growing under 24-hour continuous light, fractionate less than temperate and tropical plants. In this study, we examine the effect of diurnal light (DL) versus 24-hour continuous light (CL) on the isotopic composition of leaf n-alkanes and n-acids in greenhouse experiments using two common Arctic plants (Eriophorum vaginatum, or tussock cottongrass and Betula nana, or dwarf birch). For E. vaginatum, the δDwax values of various wax homologues were 5–11‰ more positive for CL plants relative to their DL counterparts, whereas for B. nana, CL waxes were 3–24‰ more negative, suggesting that daylight length is not a unifying control on leaf wax D/H ratios of Arctic plants. The δ13Cwax of B. nana was more negative for plants grown in continuous light compared to diurnal light, reflecting lower water-use efficiency, associated with prolonged stomatal opening in the CL treatment. We modeled the impact of increasing stomatal conductance and effective flow path lengths (mimicking variable leaf morphologies) on the isotopic composition of leaf waters (δDlw) and find that variations in leaf-water enrichment may explain the variable δDwax responses seen between E. vaginatum and B. nana. We suggest that between-species differences in the δDlw response to light, and differences in the utilization of stored carbohydrates, were important for governing δDwax. Our greenhouse results suggest that Arctic plant leaf waxes do not consistently display reduced εapp values as a result of 24-hour day light, providing additional support for field observations.
    Beschreibung: We thank Fred Jackson and Chris Claussen of the Brown University Plant Environmental Center for assistance with growth chambers, Chelsea Parker for assistance in plant care, and Rafael Tarozo for laboratory assistance. We want to thank Trevor Porter and three anonymous reviewers for constructive comments to improve the manuscript. This work was funded by NSF Arctic Natural Sciences grant 1503846 to Yongsong Huang and James Russell and NSF-OPP grant 1603214 to Anne Giblin. We also acknowledge graduate support for Will Daniels from the Brown-MBL joint graduate program and the Institute at Brown for Environment and Society.
    Schlagwort(e): Leaf waxes ; Hydrogen isotopes ; Carbon isotopes ; Growth experiment ; Arctic ; Continuous light
    Repository-Name: Woods Hole Open Access Server
    Materialart: Preprint
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  • 13
    Publikationsdatum: 2022-05-25
    Beschreibung: Author Posting. © American Geophysical Union, 2010. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Paleoceanography 25 (2010): PA1102, doi:10.1029/2009PA001871.
    Beschreibung: Instrumental data suggest that major shifts in tropical Pacific atmospheric dynamics and hydrology have occurred within the past century, potentially in response to anthropogenic warming. To better understand these trends, we use the hydrogen isotopic ratios of terrestrial higher plant leaf waxes (δDwax) in marine sediments from southwest Sulawesi, Indonesia, to compile a detailed reconstruction of central Indo-Pacific Warm Pool (IPWP) hydrologic variability spanning most of the last two millennia. Our paleodata are highly correlated with a monsoon reconstruction from Southeast Asia, indicating that intervals of strong East Asian summer monsoon (EASM) activity are associated with a weaker Indonesian monsoon (IM). Furthermore, the centennial-scale oscillations in our data follow known changes in Northern Hemisphere climate (e.g., the Little Ice Age and Medieval Warm Period) implying a dynamic link between Northern Hemisphere temperatures and IPWP hydrology. The inverse relationship between the EASM and IM suggests that migrations of the Intertropical Convergence Zone and associated changes in monsoon strength caused synoptic hydrologic shifts in the IPWP throughout most of the past two millennia.
    Beschreibung: This research was supported by the U.S. NSF, the Ocean and Climate Change Institute at WHOI, and a National Defense Science and Engineering Graduate Fellowship to J. Tierney.
    Schlagwort(e): Tropical Pacific climate ; Compound-specific hydrogen isotopes
    Repository-Name: Woods Hole Open Access Server
    Materialart: Article
    Format: application/postscript
    Format: application/pdf
    Format: text/plain
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  • 14
    facet.materialart.
    Unbekannt
    American Association for the Advancement of Science
    In:  EPIC3Science, American Association for the Advancement of Science, 371(6531), pp. 811-818
    Publikationsdatum: 2022-10-01
    Beschreibung: Geological archives record multiple reversals of Earth's magnetic poles, but the global impacts of these events, if any, remain unclear. Uncertain radiocarbon calibration has limited investigation of the potential effects of the last major magnetic inversion, known as the Laschamps Excursion 41 to 42 thousand years ago (ka). We use ancient New Zealand kauri trees (Agathis australis) to develop a detailed record of atmospheric radiocarbon levels across the Laschamps Excursion. We precisely characterize the geomagnetic reversal and perform global chemistry-climate modeling and detailed radiocarbon dating of paleoenvironmental records to investigate impacts. We find that geomagnetic field minima ~42 ka, in combination with Grand Solar Minima, caused substantial changes in atmospheric ozone concentration and circulation, driving synchronous global climate shifts that caused major environmental changes, extinction events, and transformations in the archaeological record.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
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  • 15
    ISSN: 1476-4687
    Quelle: Nature Archives 1869 - 2009
    Thema: Biologie , Chemie und Pharmazie , Medizin , Allgemeine Naturwissenschaft , Physik
    Notizen: [Auszug] Severe stratospheric ozone depletion is the result of perturbations of chlorine chemistry owing to the presence of polar stratospheric clouds (PSCs) during periods of limited exchange of air between the polar vortex and midlatitudes and partial exposure of the vortex to sunlight. These ...
    Materialart: Digitale Medien
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  • 16
    Digitale Medien
    Digitale Medien
    Springer
    Solar physics 165 (1996), S. 23-39 
    ISSN: 1573-093X
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Physik
    Notizen: Abstract Data from the Halogen Occultation Experiment (HALOE) provide the first opportunity to examine solar center-to-limb relative intensity measured exoatmospherically at wavelengths from 2.4 to 10 μm. The data were obtained from limb-to-limb scans across the solar equator on days of very low activity in May 1994. Coefficients for a function describing limb darkening are obtained at eight infrared wavelengths using a nonlinear least-squares fitting technique. Relative intensities produced by the limb-darkening functions are precise to 0.1% (2σ). From the limb-darkening coefficients, it is possible to calculate temperature information about the photosphere. At each of the eight HALOE wavelengths, the brightness temperature from the flux, T b disk(λ), and the temperature as a function of monochromatic optical depth, T(τλ), are determined and normalized using Kondratyev et al. (1965) and calibrated Pierce (1954) central intensity measurements. The two temperature quantities are compared with the predictions of Vernazza, Avrett, and Loeser's (1976) model M, and in general there is good agreement. The largest differences occur between 2.4 and 3 μm and suggest that the central intensities used in this spectral region are low.
    Materialart: Digitale Medien
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  • 17
    Publikationsdatum: 2024-02-07
    Beschreibung: Geological archives record multiple reversals of Earth’s magnetic poles, but the global impacts of these events, if any, remain unclear. Uncertain radiocarbon calibration has limited investigation of the potential effects of the last major magnetic inversion, known as the Laschamps Excursion [41 to 42 thousand years ago (ka)]. We use ancient New Zealand kauri trees (Agathis australis) to develop a detailed record of atmospheric radiocarbon levels across the Laschamps Excursion. We precisely characterize the geomagnetic reversal and perform global chemistry-climate modeling and detailed radiocarbon dating of paleoenvironmental records to investigate impacts. We find that geomagnetic field minima ~42 ka, in combination with Grand Solar Minima, caused substantial changes in atmospheric ozone concentration and circulation, driving synchronous global climate shifts that caused major environmental changes, extinction events, and transformations in the archaeological record.
    Materialart: Article , PeerReviewed
    Format: text
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