Results 91 to 100 of about 12,978 (245)
The Ediacaran Period witnessed major environmental change and an expansion of eukaryotic life following the Marinoan glaciation. The Doushantuo Formation of south China has furnished much of our understanding of Earth System and biosphere evolution ...
Shujun Han +5 more
semanticscholar +1 more source
On the coevolution of Ediacaran oceans and animals [PDF]
Fe speciation and S-isotope of pyrite data from the terminal Proterozoic Sheepbed Formation in Canada and Doushantuo Formation in China reveal that ocean deep waters were anoxic after the global glaciations (snowball Earth) ending 635 million years ago, but that marine sulfate concentrations and inferentially atmospheric oxygen levels were higher than ...
Yanan, Shen +2 more
openaire +2 more sources
A putative triradial macrofossil from the Ediacaran Jiangchuan Biota
Summary: The late Ediacaran Jiangchuan biota, from the Dengying Formation in eastern Yunnan, is well-known for its diverse macroalgal fossils, opening a window onto eukaryotic-dominated ecosystems from the late Neoproterozoic of South China.
Mingsheng Zhao +6 more
doaj +1 more source
The Ediacaran–Cambrian period witnessed episodic extinctions, oxygenation of seawaters, Cambrian explosions, and tectonic events. However, compared with the various high-resolution geochemical records of the early–middle Ediacaran and Cambrian, the ...
Xiaojun Zhang +16 more
doaj +1 more source
The Ediacaran-Lower Ordovician successions exposed in the Eastern Pyrenees are updated and revised based on recent U-Pb zircon radiometric ages, intertonguing relationships of carbonate-dominated strata, and onlapping patterns marking the top of volcano ...
M. Padel +3 more
doaj +3 more sources
Ediacaran survivors in the Cambrian: suspicions, denials and a smoking gun
The relative timing of extinctions and originations is a foundation for reconstructing evolutionary causes. However, there has been a tendency to dismiss reported Ediacaran holdovers in favour of effective extinction around the Cambrian boundary.
Jennifer F. Hoyal Cuthill
semanticscholar +1 more source
A movable beast: glaciation in the Ediacaran
<p>Ediacaran time (635–543 million years ago [Ma]) represents the dawn of macroscopic life following two Neoproterozoic Snowball Earth episodes [<span></span><a>1</a>], where a runaway ice-albedo effect caused the entire planet to become engulfed in ice [<span></span><a>2</a>,<span>< ...
openaire +2 more sources
Ediacaran reorganization of the marine phosphorus cycle
Significance The evolution of macroscopic animals in the latest Proterozoic Eon is associated with many changes in the geochemical environment, but the sequence of cause and effect remains a topic of intense research and debate. In this study, we use two
T. Laakso +3 more
semanticscholar +1 more source
Abstract Precambrian supercontinent reconstructions largely rely on robust geological constraints. Among these, the basin affinities recorded by Precambrian sedimentary fragments preserved in orogenic belts provide critical evidence for resolving the paleogeographic configurations of microcontinents and continental blocks.
Yongcheng Li +14 more
wiley +1 more source
: It has been an intense debate on the exact boundary between Ediacaran and Cambrian in the southwest Yangtze Block. The calibration of this critical boundary has a remarkable influence on the further investigation of the break-up of the Rodinia ...
Jun-ping Liu +10 more
doaj +1 more source

