We present new carbon and oxygen isotope curves from sections in the Bakony Mts. (Hungary), constrained by biostratigraphy and magnetostratigraphy in order to evaluate whether carbon isotopes can provide a tool to help establish and correlate the last system boundary remaining undefined in the Phanerozoic as well provide data to better understand the carbon cycle history and environmental drivers during the Jurassic-Cretaceous interval. We observe a gentle decrease in carbon isotope values through the Late Jurassic. A pronounced shift to more positive carbon isotope values does not occur until the Valanginian, corresponding to the Weissert event. In order to place the newly obtained stable to relatively stable δ 13 C values, compounded by a slope which is too slight. There is no clear isotopic marker event for the system boundary. The long-term gradual change towards more negative carbon isotope values through the Jurassic-Cretaceous transition has previously been explained by increasingly oligotrophic condition and lessened primary production. However, this contradicts the reported increase in 87 Sr/ 86 Sr ratios suggesting intensification of weathering (and a decreasing contribution of non-radiogenic hydrothermal Sr) and presumably a concomitant rise in nutrient input into the oceans.The concomitant rise of modern phytoplankton groups (dinoflagellates and coccolithophores) would have also led to increased primary productivity, making the negative carbon isotope trend even more notable. We suggest that gradual oceanographic changes, more effective connections and mixing between the Tethys, Atlantic and Pacific Oceans, would have promoted a shift towards enhanced burial of isotopically heavy carbonate carbon and effective recycling of isotopically light organic matter.These processes account for the observed long-term trend, interrupted only by the Weissert event in the Valanginian.
The present paper reports dental remains from Jurassic marine sediments of Hungary, referred to as Asteracanthus dunaii sp. nov. and Asteracanthus ornatissimus. Teeth of the new species Asteracanthus dunaii sp. nov. differ from all other Jurassic species of Asteracanthus
by the unique occlusal ornamentation, by the presence of a mesiodistally running, low and wide transversal ridge (causing a hat-like, asymmetrical outline in cross-section view), and by the arched shape of the mesially domed second lateral teeth. The tooth material of the new species is assumed
to belong to the same individual. The present study also highlights the importance of the revision of previously collected and/or not inventoried fossil materials housed in private and museum collections, and also that of untended sections of palaeontological collections worldwide. A revision
of the Jurassic species of Asteracanthus, and a short summary of what we know about the feeding strategy and body size of Asteracanthus is also reported.
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