Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's
oceans through time have been documented through stratigraphic study of marine …

Abstract The McArthur Basin is part of a Proterozoic basin system on the North Australian
Craton that represents a world-class Zn-Pb province. Ore bodies are typically stratiform and …

Deep-sea benthic foraminifera live in the largest habitat on Earth, constitute an important
part of its benthic biomass, and form diverse assemblages with common cosmopolitan …

Abstract The Early Middle Pleistocene Transition (EMPT) is the term used to describe the
prolongation and intensification of glacial–interglacial climate cycles that initiated after …

In this paper we present geological evidence from the Larsemann Hills (Lambert Glacier–
Amery Ice Shelf region, East Antarctica) of marine sediments at an altitude of c. 8ma. sl, as …

The distribution of forest cover alters Earth surface mass and energy exchange and is
controlled by physiology, which determines plant environmental limits. Ancient plant …

Retreat of glacier ice from Nares Strait and other straits in the Canadian Arctic Archipelago
after the end of the last Ice Age initiated an important connection between the Arctic and the …

The feeding behavior of marine predators varies with the level of competition to which they
are exposed. Populations living in the same or overlapping geographic regions (sympatric) …

Abstract The late Miocene‐early Pliocene was a time of global cooling and the development
of modern meridional thermal gradients. Equatorial Pacific sea surface conditions potentially …

Despite decades of research, the cause of deglaciations is not fully understood, leaving a
critical gap in our understanding of Earth's climate system. During the most recent …