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 …

The evolutionary rise of powerful new ecosystem engineering impacts is thought to have
played an important role in driving waves of biospheric change across the Ediacaran …

The Precambrian covers 80% of the history the Earth. In this timespan, the Earth developed
from an anaerobic planet to the oxygenic planet dominated by Wilson-style plate tectonics …

Since the 1980s, the existence of one or more extinction events in the late Ediacaran has
been the subject of debate. Discussion surrounding these events has intensified in the last …

Fossil material assigned to Nenoxites from the late Ediacaran Khatyspyt Formation of Arctic
Siberia (550–544 Ma) has been presented as evidence for bioturbation prior to the basal …

Himatiichnus mangano igen. et isp. nov., a new trace fossil from the late Ediacaran Huns
Member of the Urusis Formation, southern Namibia, comprises intertwining tubes exhibiting …

Abstract The Anti-Atlas Mountains of Morocco preserve one of the most complete latest
Neoproterozoic to Cambrian stratigraphic successions worldwide, with high-resolution …

A single phosphatised specimen from the middle Cambrian Henson Gletscher Formation
(Miaolingian Series, Wuliuan Stage) of North Greenland is interpreted as the hatching larva …

Abstract The Tagatiya Guazú (PY) and Tamengo (BR) formations are South-American
Ediacaran-Cambrian carbonate units that share striking similarities between their …

The rise of morphological complexity and taxonomic diversity of trace fossils during the
Cambrian Period has been a prominent focus to track the evolution and diversification of …