ArticleGoogle Scholar Lang, W.D. and Spath, L.F., The Black Marl of Black Ven and Stonebarrow, in the Lias of the Dorset coast, 1926, vol. 82, pp. 144–187. Lukeneder, P. and Lukeneder, A., Sinemurian biostratigraphy of the Tannscharten section near Reichraming (Lower Jurassic,...
The input of terrigenous clastic mineral matter and OM was high according to the proximity to the coast. The initiation of the black shale deposition probably was moderated by changes in sea level, with a sea level drop causing basin restriction initiated in the Late Pliensbachian, followed by...
Due to the size of the subcontinent, many inland regions were far from the coast and had vast deserts. The only places on the continent with adequate moisture for vegetation were on the fringes. The earliest dinosaurs appeared at this time and were widespread. RIVERSIDE. The Herrerasaurus, ...
A. Shifts in shell mineralogy and metabolism of Concholepas concholepas juveniles along the Chilean coast. Mar. Freshw. Res. 66, 1147–1157 (2015). Article Google Scholar Ries, J. Review: geological and experimental evidence for secular variation in seawater Mg/Ca (calcite–aragonite seas) ...
Hence a single hotspot may have formed successive sets of SDRs during the southward propagation of the Central Atlantic, from 200–190 Ma along the east coast of North America to 180–170 Ma in Demerara, at the southernmost tip of the Central Atlantic. However, the duration of hotspot ...
Palaeomagnetism of the Mesozoic coast-parallel dolerite dikes of West Greenland Can. J. Earth Sci., 12 (1975), pp. 1244-1248 CrossrefGoogle Scholar Fisher, 1953 R.A. Fisher Dispersion on a sphere. Proc. R. Soc. London Series A, 217 (1953), pp. 295-305 CrossrefView in ScopusGoogle...
Marine reptiles from the Upper Lias (Lower Toarcian, Lower Jurassic) of the Yorkshire coast Proceedings of the Yorkshire Geological Society, 44 (1984), pp. 399-429 CrossrefView in ScopusGoogle Scholar Boomer et al., 2021 I. Boomer, P. Copestake, K.P. Page, J. Huxtable, T. Loy, P.R...
The Samarka terrane, a fragment of the Jurassic accretionary prism13,15,31,32,33, forms a 30–70 km-wide strip extending north-northeastward for nearly 900 km from the southern coast of Primorye to the Amur River basin (Fig. 2). The terrane is bounded in the east by the Central Sikho...
represented by an incomplete wing ofDobbertinia reticulataHandlirsch 1920 (Ansorge2001). The scarcity of both Coniopterygidae and Sialidae in these lower Toarcian marine sediments can be explained by the assumption that their habitats could be located far from the coast, and they did not fly...
For the successful realization and productivity prediction of new hydrothermal projects in the South German Molasse Basin, the hydraulic matrix properties of the Upper Jurassic Malm reservoir have to be determined as accurately as possible. To obtain specific information on the distribution of the petrop...