Results 51 to 60 of about 1,144 (173)
Terra Nova, Volume 38, Issue 2, Page 130-140, April 2026.ABSTRACT We present novel 3D subsidence data enabling vertical movements' quantification during the early formation of the Pyrenean retro‐wedge. From Cenomanian to Turonian times, subsidence is relatively low (~26 ± 10 m/Myr), corresponding to a brief 10 Myr thermal re‐equilibration of the European lithosphere following the hyperextended rift episode ...
Benoit Issautier +5 more
wiley +1 more source
New Zealand Geological Timescale 2025
New Zealand Journal of Geology and Geophysics, Volume 69, Issue 1, March 2026.New Zealand Geological Timescale 2025 (NZGT 2025) is the first comprehensive update and revision of the New Zealand Geological Timescale in a decade. The criteria used to establish age ranges of New Zealand Stages within the NZGT have been reviewed, calibrated, and revised where required against the 2023/04 International Chronostratigraphic Chart and ...
Christopher D. Clowes +13 more
wiley +1 more source
Papers in Palaeontology, Volume 12, Issue 2, March/April 2026.Abstract The fossil record of coelacanths (Actinistia) is diminished by several nominal gaps that obscure vital information pertaining to the clade's evolutionary history. Latimeriidae, the family that includes the extant coelacanth Latimeria, in addition to the Cenozoic, has an outstanding missing gap of 50 myr during the Mesozoic, with no records of ...
Jack L. Norton +4 more
wiley +1 more source
Chukhonastovka – the reference section of the Turonian-Lower Santonian from the Volga-Ilovlya interfluve (the Volga right bank area near Volgograd). Paper 2. Characteristics of the Oryctocomplexes [PDF]
Известия Саратовского университета. Новая серия: Серия Науки о ЗемлеA representative complex of the Turonian-Santonian carbonate-producing invertebrates has been revealed. It comprised benthic foraminifers, diverse echinoderms, brachiopods, calcareous and siliceous sponges.
Pervushov, Evgeniy Mikhaylovich +4 more
doaj +1 more source
Geochemistry, Geophysics, Geosystems, Volume 27, Issue 2, February 2026.Abstract Widespread organic‐rich shales are associated with perturbations in productivity or preservation conditions; however, the major controlling factors, especially the phosphorus (P) and iron (Fe) interactions and their impacts on organic carbon burial in the paleolake ecosystem remain poorly understood.
Bo Wang +7 more
wiley +1 more source
Dinosaur footprints in the Upper Turonian-Coniacian limestone in the Krnica Bay (NE Istria, Croatia)
Geologija, 2003 Three isolated footprints and one trackway that can be attributed to bipedal dinosaur, from a limestone bed in vicinity of Požara promontory, Krnica Bay, are described. According to the stratigraphic position the footprints are late Turonian to Coniacian
Alenka Mauko, Borut Florjančič
doaj
Turonian ammonites from Breznik area (Southwestern Bulgaria)
Geologica Balcanica, 1994 Six Turonian ammonite species from the region between the towns of Breznik and Trăn are determinated: Lewesiceras peramplum (Mantell), Collignoniceras woollgari (Mantell), C. carolinum (d’Orbigny), C. bravaisianum (d’Orbigny), Subprionocyclus neptuni (Geinitz) and Scaphites genitzii (d’Orbigny).
openaire +1 more source
The Cenomanian-Turonian transition on the Peruvian margin
Cretaceous Research, 1993 Abstract In Peru, various deposittonal sequences can be recognized during the late middle Cenomanian to early Coniacian timespan, most of which seem to have an eustatic origin. For instance, the early late Cenomanian, late early Turonian and early Coniacian maximum floodings identified in Peru coincide with well-known global eustatic events.
/Jaillard, Etienne, Arnaud-Vanneau, A.
openaire +2 more sources
Revista Mexicana de Ciencias Geológicas, 2018 A biostratigraphic zonation of the Cenomanian–Coniacian rocks of the Guerrero–Morelos basin (southern Mexico) is proposed. The stratigraphic distribution of 70 species of calcareous algae and benthic and planktonic foraminifers is used to characterize ...
Noemí Aguilera-Franco
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THE HETERODONT BIVALVE APHRODINA DUTRUGEI (COCQUAND, 1862) FROM THE CENOMANIAN OF JORDAN
Rivista Italiana di Paleontologia e Stratigrafia, 2005 The almost equivalved, strongly inequilateral Aphrodina dutrugei (Coquand, 1862) from the Shuayb Formation of the Zarqa area, Jordan, is described.
FAYEZ AHMAD
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