The global Hangenberg Crisis (Devonian–Carboniferous transition): review of a first-order mass extinction
Abstract The global Hangenberg Crisis near the Devonian–Carboniferous boundary (DCB)
represents a mass extinction that is of the same scale as the so-called 'Big Five'first-order …
represents a mass extinction that is of the same scale as the so-called 'Big Five'first-order …
Carbon-isotope stratigraphy across the Permian–Triassic boundary: a review
C Korte, HW Kozur - Journal of Asian Earth Sciences, 2010 - Elsevier
The Palaeozoic–Mesozoic transition is marked by distinct perturbations in the global carbon
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
[HTML][HTML] 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater
A total of 2128 calcitic and phosphatic shells, mainly brachiopods with some conodonts and
belemnites, were measured for their δ 18O, δ 13C and 87Sr/86Sr values. The dataset covers …
belemnites, were measured for their δ 18O, δ 13C and 87Sr/86Sr values. The dataset covers …
Strontium isotope stratigraphy: LOWESS version 3: best fit to the marine Sr-isotope curve for 0–509 Ma and accompanying look-up table for deriving numerical age
JM McArthur, RJ Howarth… - The Journal of …, 2001 - journals.uchicago.edu
An improved and updated version of the statistical LOWESS fit to the marine 87Sr/86Sr
record and a revised look-up table (V3: 10/99; available from j. mcarthur@ ucl. ac. uk) based …
record and a revised look-up table (V3: 10/99; available from j. mcarthur@ ucl. ac. uk) based …
Strontium isotope stratigraphy
JM McArthur - 2010 - pubs.geoscienceworld.org
Strontium Isotope Stratigraphy | Application of Modern Stratigraphic TechniquesTheory and
Case Histories | GeoScienceWorld Books | GeoScienceWorld Skip to Main Content …
Case Histories | GeoScienceWorld Books | GeoScienceWorld Skip to Main Content …
Chemostratigraphy of the Jurassic System: applications, limitations and implications for palaeoceanography
Current chemostratigraphical studies of the Jurassic System primarily involve the use of one
sedimentary component (marine organic carbon), one divalent transition metal substituted in …
sedimentary component (marine organic carbon), one divalent transition metal substituted in …
Strontium isotope evolution of Late Permian and Triassic seawater
The 87Sr/86Sr values based on brachiopods and conodonts define a nearly continuous
record for the Late Permian and Triassic intervals. Minor gaps in measurements exist only …
record for the Late Permian and Triassic intervals. Minor gaps in measurements exist only …
Dating the 840–544 Ma Neoproterozoic interval by isotopes of strontium, carbon, and sulfur in seawater, and some interpretative models
MR Walter, JJ Veevers, CR Calver, P Gorjan… - Precambrian …, 2000 - Elsevier
We construct a time scale for the 840–544Ma Neoproterozoic interval from isotopic variation
of δ13Ccarbonate and δ13Corganic, 87Sr/86Sr, and δ34Ssulfate in seawater measured …
of δ13Ccarbonate and δ13Corganic, 87Sr/86Sr, and δ34Ssulfate in seawater measured …
Strontium isotopes and prehistoric human migration: the Bell Beaker period in central Europe
TD Price, C Knipper, G Grupe… - European journal of …, 2004 - cambridge.org
Human skeletal remains from Bell Beaker graves in southern Germany, Austria, the Czech
Republic, and Hungary were analyzed for information on human migration. Strontium …
Republic, and Hungary were analyzed for information on human migration. Strontium …
Application of multiple isotopic and geochemical tracers for investigation of recharge, salinization, and residence time of water in the Souss–Massa aquifer, southwest …
L Bouchaou, JL Michelot, A Vengosh, Y Hsissou… - Journal of …, 2008 - Elsevier
Groundwater and surface water in Souss–Massa basin in the west-southern part of Morocco
is characterized by a large variation in salinity, up to levels of 37gL− 1. The high salinity …
is characterized by a large variation in salinity, up to levels of 37gL− 1. The high salinity …