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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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Morocco
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Asia
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China
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North America
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Invertebrata
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upper Precambrian
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Primary terms
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absolute age (1)
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Africa
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North Africa
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Atlas Mountains
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Moroccan Atlas Mountains
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High Atlas (1)
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Morocco
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Moroccan Atlas Mountains
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High Atlas (1)
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Nubian Shield (1)
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Arctic region
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Asia
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Australasia
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Australia
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biogeography (8)
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Canada
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carbon
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Ossa-Morena Zone (1)
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Spain
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Spanish Pyrenees (1)
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Western Europe
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France
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Scandinavia
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Inarticulata (2)
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isotopes
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GeoRef Categories
Era and Period
Epoch and Age
Date
Availability
Hyolithes
Cambrian Age 3 small shelly fossils from the Terrades inlier, southern Pyrenees, Spain: Biostratigraphic and paleobiogeographic implications
New Middle Ordovician hyoliths from the Ossa Morena Zone, southwestern Spain
Exceptionally preserved hyolithids from the middle Cambrian of North China
An outer shelf shelly fauna from Cambrian Series 2 (Stage 4) of North Greenland (Laurentia)
The oldest hyolithids (Cambrian Series 2, Montezuman Stage) from the Iapetan margin of Laurentia
COPROLITES IN THE RAVENS THROAT RIVER LAGERSTÄTTE OF NORTHWESTERN CANADA: IMPLICATIONS FOR THE MIDDLE CAMBRIAN FOOD WEB
Small shelly fossils from the Montezuman–Delamaran of the Great Basin in Nevada and California
Soft-bodied biota from the middle Cambrian (Drumian) Rockslide Formation, Mackenzie Mountains, northwestern Canada
Cambrian stratigraphy of Jordan
A Complete Reconstruction of the Hyolithid Skeleton
New Hyolitha from the Devonian of Bolivia
SIGNS OF BORING PREDATION ON MIDDLE DEVONIAN HYOLITHIDS FROM THE MICHIGAN BASIN
DEVONIAN (GIVETIAN) HYOLITHA FROM THE KERSADIOU FORMATION, MASSIF AMORICAIN, FRANCE
FIRST OCCURRENCE OF ORTHOTHECA NOVÁK, 1886 (HYOLITHA, EARLY DEVONIAN) IN NORTH AMERICA
Permian Hyolithida from Australia: The Last of the Hyoliths?
Paleontological data from the Early Cambrian of Germany and paleobiogeographical implications for the configuration of central Perigondwana
Fossiliferous Early Cambrian strata from central Europe are known from two fragmentary preserved units situated in eastern Germany: the Görlitz syncline and the Torgau-Doberlug syncline. The fossil assemblages from both regions and their geological framework are presented. The taxonomic content, the internal structure, and the biostratigraphic positions of the containing assemblages are quite different. Trilobites and other shelly fossils (from Görlitz syncline) and archaeocyathans (from Torgau-Doberlug syncline) show strong relationships to equivalent faunas in Morocco, Spain, and France. Further, there are some indications for relationships to the Far East. The German faunas indicate very active faunal exchange within the peri-Gondwanan realm and probably over longer distances along the Gondwana margin, too. Together with the nearly shelf-wide consistent sedimentary facies patterns, consequently, they contradict the model of local and isolated basins for the areas of deposition. The current patchy geographical distribution of Cambrian sediments in central and southern Europe is interpreted as a phenomenon of (1) regionally different sedimentation rates on the Gondwanan shelf (probably by local origination of open intra-shelf basins caused by a general rifting process), and of (2) Late Cambrian to Early Ordovician different-scaled uplift and denudation of parts of the shelf. The content, the coinciding evolutionary patterns, and the paleogeographical relationships of the Cambrian faunas suggest that separation and evolution of terranes in central Perigondwana had not started before the end of the Cambrian or the beginning of the Early Ordovician. For Early and Middle Cambrian times at least, a slightly differentiated shelf-configuration of Perigondwana without isolated areas (terranes) fits best with the paleontological and sedimentological data.