Results 61 to 70 of about 2,191 (193)

End-Triassic calcification crisis and blooms of organic-walled 'disaster species' [PDF]

open access: yes, 2007
The Triassic–Jurassic (T–J) mass-extinction event is marked by isotope anomalies in organic (δ13Corg) and carbonate carbon (δ13Ccarb) reservoirs. These have been attributed to a (rapid) 4-fold rise in pCO2 as a result of massive flood basalt volcanism ...
Bailey, T. R.   +8 more
core   +2 more sources

The effect of precipitation rate on Mg/Ca and Sr/Ca ratios in biogenic calcite as observed in a belemnite rostrum [PDF]

open access: yes, 2017
This is the author's manuscript - under review for journal Biogeosciences and available online from the publisher via the DOI in this record.Isotopic ratios and concentrations of the alkaline earth metals Mg and Sr in biogenic calcite are of great ...
Ullmann, CV
core   +1 more source

The effect of shell secretion rate on Mg / Ca and Sr / Ca ratios in biogenic calcite as observed in a belemnite rostrum [PDF]

open access: yes, 2017
ArticleThis is the final version of the article. Available from European Geosciences Union via the DOI in this record.Isotopic ratios and concentrations of the alkaline earth metals Mg and Sr in biogenic calcite are of great importance as proxies for ...
Pogge von Strandmann, PAE, Ullmann, CV
core   +2 more sources

MASS EXTINCTIONS AND CLADE EXTINCTIONS IN THE HISTORY OF BRACHIOPODS: BRIEF REVIEW AND A POST-PALEOZOIC CASE STUDY

open access: yesRivista Italiana di Paleontologia e Stratigrafia, 2019
Brachiopods are a key group in Phanerozoic marine diversity analyses for their excellent fossil record and distinctive evolutionary history. A genus-level survey of raw diversity trajectories allows the identification of the Brachiopod Big Five, episodes
ATTILA VÖRÖS   +2 more
doaj   +1 more source

Sr-Isotope Stratigraphy: Assigning Time in the Campanian, Pliensbachian, Toarcian, and Valanginian [PDF]

open access: yes, 2016
The trend of marine 87Sr/86Sr against stratigraphic level through sections, whether linear or not, can identify hiatuses and changing rates of sedimentation through those sections and so be a valuable constraint on attempts to assign numerical ages to ...
Landman, NH   +3 more
core   +2 more sources

Palaeoenvironmental significance of Toarcian black shales and event deposits from southern Beaujolais, France [PDF]

open access: yes, 2017
New sedimentological, biostratigraphical and geochemical data recording the Toarcian Oceanic Anoxic Event (T-OAE) are reported from a marginal marine succession in southern Beaujolais, France.
FÖLLMI, KARL B.   +10 more
core  

A calcareous nannofossil and organic geochemical study of marine palaeoenvironmental changes across the Sinemurian/Pliensbachian (early Jurassic, ~191Ma) in Portugal [PDF]

open access: yes, 2016
The Sinemurian/Pliensbachian boundary (~ 191 Ma) is acknowledged as one of the most important steps in the radiation of planktonic organisms, especially primary producers such as dinoflagellates and coccolithophores.
Baudin, F.   +6 more
core   +4 more sources

Analysis of global diversity patterns and dynamics of selected Mesozoic marine invertebrate groups [PDF]

open access: yes, 2015
Megjegyzés az értekezés megjelenítéséről: a szerző kérésére a disszertáció 2017-08-31-től lehet nyilvános; a tézisek ...
Kocsis, Tibor Ádám
core   +1 more source

Tectonic forcing of Early to Middle Jurassic seawater Sr/Ca [PDF]

open access: yes, 2015
types: ArticleThis is the author formatted version of Ullman et al. (2013) Geology 41(12), 1211-1214. doi:10.1130/G34817.1 http://geology.gsapubs.org/content/41/12/1211.full Uploaded under the terms of Green Open Access in GSA's Open Access PolicyThe ...
Hesselbo, Stephen P.   +2 more
core   +1 more source

Barium Isotopes Indicate Spatiotemporal Heterogeneity of Marine Primary Productivity During the Toarcian Oceanic Anoxic Event

open access: yesGeophysical Research Letters, Volume 53, Issue 10, 28 May 2026.
Abstract The Toarcian Oceanic Anoxic Event (T‐OAE, ∼183 Ma) was characterized by globally enhanced organic‐carbon burial and a negative carbon‐isotope excursion (N‐CIE). However, the role of marine productivity at this time, and its spatiotemporal variability, is unclear.
Wenhan Chen   +11 more
wiley   +1 more source

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