Neoproterozoic tectonic geography was dominated by the formation of the supercontinent
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …

The Central Asian Orogenic Belt (c. 1000–250 Ma) formed by accretion of island arcs,
ophiolites, oceanic islands, seamounts, accretionary wedges, oceanic plateaux and …

The long-awaited revision of the industry standard on phylogenetics Since the publication of
the first edition of this landmark volume more than twenty-five years ago, phylogenetic …

Supercontinents play an important role in Earth's history. The exact definition of what
constitutes a supercontinent is difficult to establish. Here the argument is made, using …

The assembly of the Gondwana supercontinent during the waning stages of the Proterozoic
provides a tectonic backdrop for the myriad biological, climatological, tectonic and …

Peninsular India forms a keystone in Gondwana, linking the East African and Malagasy
orogens with Ediacaran–Cambrian orogenic belts in Sri Lanka and the Lützow Holm Bay …

The Ediacaran Period was a critical time in the history of life and Earth. Understanding the
complex interactions between geological and biological events during this interval requires …

The Precambrian geologic history of Peninsular India covers nearly 3.0 billion years of time.
India is presently attached to the Eurasian continent although it remains (for now) a separate …

Abstract Distinctive uppermost Ediacaran–Ordovician rocks (Avalonian overstep sequence)
were key in definition of Avalonia, which comprises large areas of the NE Appalachians and …

The old terrane of Siberia occupied a very substantial area in the centre of today's political
Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China …