Search results for "Surface Processes"

showing 4 items of 1294 documents

Late Jurassic (Kimmeridgian–Tithonian) stable isotopes (δ18O, δ13C) and Mg/Ca ratios: New palaeoclimate data from Helmsdale, northeast Scotland

2010

Abstract The data presented here provide the first detailed stable isotope ( δ 18 O, δ 13 C) and geochemical (Mg/Ca) investigation of Kimmeridgian–Tithonian belemnites from the Helmsdale Coast, Scotland, UK. Oxygen and carbon stable isotope values from well preserved specimens range from − 2.8 to + 0.3‰ and from − 2.3 to + 2.8‰ respectively. The oxygen isotope data are consistent with palaeotemperatures of up to 24 °C in the Early Kimmeridgian cymodoce Zone and down to 11 °C in the Mid Tithonian rotunda–fittoni Zones. These estimates are strongly supported by the Mg/Ca data, which also indicate a cooling episode (and very similar palaeotemperatures, 11–22 °C) at this time. The cooling event…

δ13Cbiologyδ18OStable isotope ratioPaleontologyOceanographybiology.organism_classificationIsotopes of oxygenPaleontologyIsotopes of carbonChemostratigraphyPaleoclimatologyBelemnitesEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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A 2600-year record of past polycyclic aromatic hydrocarbons (PAHs) deposition at Holzmaar (Eifel, Germany)

2014

Polycyclic aromatic hydrocarbons (PAHs) are a proxy for climate- and human-related historical fire activity which has rarely been used beyond 1800 AD. We explored the concentration and composition patterns of PAHs together with other proxies (charcoal, C, N, S, δ13C, δ15N, and δ34S) in a sediment core of Holzmaar as indicators of variations in climate and anthropogenic activity over the past 2600 years. The concentrations of pyrogenic PAHs remained low (< 500 ng g− 1) from the pre-Roman Iron Age (600 BC) until the first significant increases to ca. 1000–1800 ng g− 1 between 1700 and 1750 AD related to regional iron production. The highest increases in pyrogenic PAH concentrations occurred w…

δ13Cbusiness.industryPaleontologyδ15NOceanographyδ34SIron AgeEnvironmental chemistryvisual_artvisual_art.visual_art_mediumSedimentary organic matterCoalPolycyclic HydrocarbonsbusinessCharcoalEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Unraveling environmental histories from skeletal diaries — Advances in sclerochronology

2013

High-resolution proxy archives from aquatic settings are essential to better understand processes and mechanisms of global change. During the last decade, it has become increasingly evident that calcified tissues of bivalve mollusks and cold-water corals, in particular, can significantly increase our knowledge of seasonal to multi-decadal paleoclimate and paleoenvironmental variability in the extratropical oceans and coastal marine settings. Daily, tidal, fortnightly and annual growth patterns of periodically formed skeletal hard parts provide a means to place the proxy record in a precise temporal context. Their extreme longevity coupled with the running similarity between growth increment…

δ13Cδ18OPaleontologyGlobal changeOceanographyProxy (climate)Waves and shallow waterOceanographySclerochronologyPaleoclimatologyResource useEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Variation in Sr uptake in the shell of the freshwater gastropod Bithynia tentaculata from Lake Arreo (northern Spain) and culture experiments

2010

The Sr uptake features in Bithynia tentaculata aragonite shells from monthly collections in Lake Arreo (northern Spain) over a two-year period are compared with those from the same species grown in culture experiments with similar waters under controlled temperature. The shell aragonite of B. tentaculata from Lake Arreo formed in isotopic equilibrium with the lake water. A comparison of the stable oxygen isotope values (δ18O) from the shells and waters allowed the selection of suitable shells for Sr uptake studies. The Sr/Ca molar ratio in B. tentaculata shells (Sr/Cashell) from the lake and from the culture experiments positively correlate with some chemical parameters like conductivity an…

δ18Ochemistry.chemical_elementMineralogyengineering.materialOceanographyIsotopes of oxygenBithynia tentaculataMollusk shellEcology Evolution Behavior and SystematicsEarth-Surface ProcessesStrontiumbiologyStable isotope ratioAragoniteTrace elementPaleontologyTentaculatabiology.organism_classificationOxygen isotopeAragonitechemistryStrontiumEnvironmental chemistryengineeringTrace elementGeology
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