Results 41 to 50 of about 340 (144)
Ediacaran metazoan reefs from the Nama Group, Namibia [PDF]
Reef-building inmetazoans represents an important ecological innovationwhereby individuals collectively enhance feeding efficiency and gain protection from competitors and predation.
Hoffman, K. H. +7 more
core +1 more source
Multiple branching and attachment structures in cloudinomorphs, Nama Group, Namibia [PDF]
The Ediacaran-Cambrian cloudinomorphs, which include Cloudina, are the first putative skeletal metazoans. They have a benthic ecology and tubular, organic, or biomineralized stacked funnel morphologies but an unresolved phylogenetic affinity.
Curtis, A. +7 more
core +1 more source
Carbonate sedimentology: An evolved discipline
Abstract Although admired and examined since antiquity, carbonate sediment and rock research really began with Charles Darwin who, during a discovery phase, studied, documented and interpreted their nature in the mid‐19th century. The modern discipline, however, really began after World War II and evolved in two distinct phases.
Noel P. James, Peir K. Pufahl
wiley +1 more source
Se compara la lito- bio- y quimioestratigrafía de sucesiones sedimentarias del Neoproterozoico del Cratón del Río de la Plata, a saber: Grupo Arroyo del Soldado (GAS), Uruguay y Grupo Sierras Bayas - Formación Cerro Negro (GSB-FmCN) de Tandilia ...
Claudio Gaucher +3 more
doaj +2 more sources
An updated stratigraphic subdivision of the Ediacaran and Terreneuvian in the Alcudia valley and the Toledo Mountains, Central Iberian Zone, is documented here.
J. J. Álvaro +4 more
doaj +1 more source
Palaeoecology of Ediacaran metazoan reefs [PDF]
Terminal Ediacaran metazoan reefs (~548-541 Million years ago (Ma)) can be locally substantial and the skeletal metazoans Cloudina riemkeae, C. hartmannae, Namacalathus and Namapoikia produced diverse reef types with complex ecologies in association with
Wood, Rachel
core +1 more source
ABSTRACT The lower Nama Group in southern Namibia contains trace fossils and soft‐bodied and biomineralized macro‐organisms from the terminal Ediacaran Period (ca 550 to 539 Ma), offering insights into early metazoan evolution. Interpretation of the fossilized Nama Group organisms as being preserved in, or very close to, the environments in which they ...
Brennan O'Connell +7 more
wiley +1 more source
How to engineer a habitable planet: the rise of marine ecosystem engineers through the Phanerozoic
Abstract Ecosystem engineers are organisms that modify their physical habitats in a way that alters resource availability and the structure of the communities they live in. The evolution of ecosystem engineers over the course of Earth history has thus been suggested to have been a driver of macroevolutionary and macroecological changes that are ...
Alison T. Cribb, Simon A. F. Darroch
wiley +1 more source
ABSTRACT The end‐Neoproterozoic transition marked a gradual but permanent shift between distinct configurations of Earth's biosphere. This interval witnessed the demise of the enigmatic Ediacaran Biota, ushering in the structured trophic webs and disparate animal body plans of Phanerozoic ecosystems.
Giovanni Mussini, Frances S. Dunn
wiley +1 more source
New Cloudina-like morphotype from the Ediacaran Tamengo Formation (Neoproterozoic, Corumbá Group), Southwest Brazil [PDF]
The late Ediacaran index fossil Cloudina Germs is known for its funnel-in-funnel tubular calcareous shell. The Brazilian species Cloudina lucianoi (Beurlen and Sommer) occurs in limestones of the Tamengo Formation, near the top of the Corumbá Group, in ...
Meira, F. +5 more
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