Search results for "Carbon isotope excursion"

showing 3 items of 3 documents

Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum.

2021

Description

MultidisciplinaryEarth Environmental Ecological and Space Sciences010504 meteorology & atmospheric sciencesIsotopes of lithiumGeochemistrychemistry.chemical_elementSciAdv r-articlesGeology15. Life on land010502 geochemistry & geophysics01 natural sciencesGeochemistrychemistry13. Climate actionCarbon isotope excursionErosionEnhanced weatheringPeriod (geology)Environmental scienceWater cycleCarbon0105 earth and related environmental sciencesResearch ArticleScience advances
researchProduct

Correlation between extinction pattern and δ13C fluctuations across the Triassic Jurassic boundary in shallow water settings: a proxy for the present…

2018

With the aim to assess the possible influence of the carbon variations on the benthic communities across the Triassic Jurassic boundary we have carried out sedimentological, biostratigraphic and stable isotope studies on an about 220 m thick peritidal section cropping out in Northwestern Sicily. The subtidal facies of the lower and middle part of this succession show the common occurrence of large and thick megalodontids and a benthic foraminiferal assemblage with Triasina hantkeni and Aulotuortids that supports a Rhaetian age. In the lower part of the succession, a significative biotic perturbation is evidenced by a sudden reduction of the size, shell thickness and abundance of the large m…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaTriassic-Jurassic boundary extinction events carbon isotope excursion carbonate platform acidification Sicily
researchProduct

Acidification processes in a peritidal carbonate succession across the Triassic/Jurassic boundary (Sicily)

2017

For the first time, a correlation between biostratigraphic events and δ13C curve was attempted along an UpperTriassic-Lower Jurassic peritidal limestone succession cropping out in westernmost Sicily. The peritidal carbonates are organized in shallowing upward cycles characterized by subtidal skeletal mudstone to grainstone, intertidal microbial mats and supratidal paleosoils. About 300 meters of this succession covering the Triassic-Jurassic interval were studied in details. On the base of the macro- and microfossil assemblages from the subtidal facies, four informal units have been recognized along the studied section. Unit R1 (at the base, 111 m thick) is dominated by large megalodonts, r…

Triassic-Jurassic boundary biotic crises carbon isotope excursion carbonate platform SicilySettore GEO/02 - Geologia Stratigrafica E Sedimentologica
researchProduct