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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Tommotiida
TANNUOLINA AND MICRINA (TANNUOLINIDAE) FROM THE LOWER CAMBRIAN OF EASTERN YUNNAN, SOUTH CHINA, AND THEIR SCLERITOME RECONSTRUCTION Available to Purchase
Occurrence of Tannuolina in the early Cambrian siltstones of the Hazara Basin, North Pakistan, and its biostratigraphical significance Available to Purchase
Discussion Open Access
The scleritome of Eccentrotheca from the Lower Cambrian of South Australia: Lophophorate affinities and implications for tommotiid phylogeny Available to Purchase
Discovery of Lower Cambrian Small Shelly Fossils and Brachiopods from the Lower Vindhyan of Son Valley, Central India Available to Purchase
Small shelly fossils of late Precambrian and early Cambrian age: a review of recent work Available to Purchase
New biostratigraphical constraints on the Lower and lower Middle Cambrian of the Kharaulakh Mountains ( northeastern Siberian Platform, Chekurovka anticline ) Available to Purchase
The oldest Cambrian skeletal fossils of Spain (Cadenas Ibéricas, Aragón) Available to Purchase
New early Cambrian sclerites of Lapworthella schodakensis from NE Greenland: advancements in knowledge of lapworthellid taxonomy, sclerite growth and scleritome organization Available to Purchase
Cambrian Age 3 small shelly fossils from the Terrades inlier, southern Pyrenees, Spain: Biostratigraphic and paleobiogeographic implications Available to Purchase
Faunas and Cambrian Volcanism on the Avalonian Marginal Platform, Southern New Brunswick Available to Purchase
Chronology of early Cambrian biomineralization Available to Purchase
The Precambrian–Phanerozoic and Ediacaran–Cambrian boundaries: a historical approach to a dilemma Available to Purchase
Abstract The Cambrian was originally defined as a rock interval with a trilobite-dominated fauna that overlay a presumed biologically barren Precambrian epoch. Work to formally define the Cambrian base arose after the discovery of Precambrian macrofossils in South Australia. The Working Group on the Precambrian–Cambrian Boundary (set up in 1972) promoted an emphasis on an extended pre-trilobitic interval with mineralized skeletal elements (small shelly fossils or early skeletal fossils). The study of early skeletal fossils made the Ulakhan-Sulugur (Siberia) and Meishucun (South China) sections candidates for the basal Cambrian Global Stratotype Section and Point (GSSP), but difficulties in correlation and the taxonomy of early skeletal fossils did not allow the selection of a reliably correlative horizon. Bilaterian ichnofaunas below the first diverse early skeletal fossils suggested the definition of a Cambrian base GSSP below the early skeletal fossils. Work on the thick, stratigraphically continuous and fairly unifacial sections in the Burin Peninsula, southeastern Newfoundland led in 1992 to an ichnofossil-defined GSSP at Fortune Head. Despite arguments for a revision and redefinition of the lower boundary of the Cambrian System, the best definition of the basal Cambrian GSSP is at Fortune Head and does not rely on the Treptichnus/Trichophycus pedum (abbreviated below as T. pedum) first appearance datum, but rather on the base of the T. pedum Assemblage Zone at the highest occurrence of Ediacaran taxa and in the lower range of T. pedum .