Results 151 to 160 of about 16,111 (210)
The Rise of Algae promoted eukaryote predation in the Neoproterozoic benthos. [PDF]
Mills DB +4 more
europepmc +1 more source
Litho-structural mapping using remote sensing, petrographic characterization, and SEM/EDX mineralization analysis: insights from the Arabian-Nubian Shield. [PDF]
El-Awny H +7 more
europepmc +1 more source
The chitin raft hypothesis for the colonization of the open ocean by cyanobacteria. [PDF]
Braakman R.
europepmc +1 more source
Benthic diel oxygen variability and stress as potential drivers for animal diversification in the Neoproterozoic-Palaeozoic. [PDF]
Hammarlund EU +12 more
europepmc +1 more source
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2023
ABSTRACT Neoproterozoic to Cambrian isolation of Laurentia during the breakup of Rodinia was associated with multiple large igneous provinces, protracted multiphase rifting, and variable subsidence histories along different margin segments. In this contribution, we develop a paleogeographic model for the Neoproterozoic tectonic evolution
Francis A. Macdonald +3 more
openaire +1 more source
ABSTRACT Neoproterozoic to Cambrian isolation of Laurentia during the breakup of Rodinia was associated with multiple large igneous provinces, protracted multiphase rifting, and variable subsidence histories along different margin segments. In this contribution, we develop a paleogeographic model for the Neoproterozoic tectonic evolution
Francis A. Macdonald +3 more
openaire +1 more source
Annual Review of Earth and Planetary Sciences, 2011
The Neoproterozoic is a time of transition between the ancient microbial world and the Phanerozoic, marked by a resumption of extreme carbon isotope fluctuations and glaciation after a billion-year absence. The carbon cycle disruptions are probably accompanied by changes in the stock of oxidants and connect to glaciations via changes in the ...
Pierrehumbert, R. +3 more
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The Neoproterozoic is a time of transition between the ancient microbial world and the Phanerozoic, marked by a resumption of extreme carbon isotope fluctuations and glaciation after a billion-year absence. The carbon cycle disruptions are probably accompanied by changes in the stock of oxidants and connect to glaciations via changes in the ...
Pierrehumbert, R. +3 more
openaire +2 more sources
A Neoproterozoic Snowball Earth
Science, 1998Negative carbon isotope anomalies in carbonate rocks bracketing Neoproterozoic glacial deposits in Namibia, combined with estimates of thermal subsidence history, suggest that biological productivity in the surface ocean collapsed for millions of years.
, Hoffman +3 more
openaire +2 more sources
Precambrian Research, 2019
Carbonate successions are principal geochemical archives of the extraordinary environmental changes that occurred during the Neoproterozoic Era. In this study, we present a stratigraphic record of carbonate rare earth element (REE) compositions from Neoproterozoic and Cambrian strata in central and southern Australia.
Jack Ward, Ai Duc Nguyen
exaly +5 more sources
Carbonate successions are principal geochemical archives of the extraordinary environmental changes that occurred during the Neoproterozoic Era. In this study, we present a stratigraphic record of carbonate rare earth element (REE) compositions from Neoproterozoic and Cambrian strata in central and southern Australia.
Jack Ward, Ai Duc Nguyen
exaly +5 more sources
Learning to tell Neoproterozoic time
Precambrian Research, 2000In 1989, the International Commission on Stratigraphy established a Working Group on the Terminal Proterozoic Period. Nine years of intensive, multidisciplinary research by scientists from some two dozen countries have markedly improved the framework for the correlation and calibration of latest Proterozoic events.
openaire +2 more sources
Neoproterozoic magmatism in eastern Himalayan terrane
Science Bulletin, 2017Geochronological investigation on gneisses of granitic to leucogranitic compositions in Cuona, south Tibet, reveal that their protoliths formed at 808.8±7.9-816.4±3.4Ma and 855.8±7.0Ma, respectively. Zircon rims from the granitic gneiss record a metamorphic age of 739.4±4.3Ma.
Yuhua, Wang +7 more
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