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The Anthropocene: From Global Change to Planetary Stewardship
The Anthropocene is a reminder that the Holocene, during which complex human societies have developed, has been a stable, accommodating environment and is the only state of the Earth System that the authors know for sure can support contemporary society.
The Anthropocene is functionally and stratigraphically distinct from the Holocene
C climatic, biological, and geochemical signatures of human activity in sediments and ice cores, Combined with deposits of new materials and radionuclides, as well as human-caused modification of sedimentary processes, the Anthropocene stands alone stratigraphically as a new epoch beginning sometime in the mid–20th century.
The new world of the Anthropocene.
The Anthropocene, following the lost world of the Holocene, holds challenges for both science and society.
The Anthropocene: a new epoch of geological time?
Questions of the scale, magnitude and significance of this environmental change, particularly in the context of the Earth’s geological history, provide the basis for this Theme Issue.
Graptolites in British stratigraphy
Abstract 697 taxa of planktonic graptolites are recorded, and their stratigraphical ranges are given, through 60 biozones and subzones in the Ordovician and Silurian strata of England, Wales and
Climate and environment of a Pliocene warm world
The Pliocene Epoch, 5.33–2.58 million years ago (Ma), was a generally warmer and wetter interval with atmospheric CO2-concentrations at or slightly above modern levels. This paper provides an
Are we now living in the Anthropocene
The term Anthropocene, proposed and increasingly employed to denote the current interval of anthropogenic global environmental change, may be discussed on stratigraphic grounds. A case can be made
Stratigraphy of the Anthropocene
The Anthropocene, an informal term used to signal the impact of collective human activity on biological, physical and chemical processes on the Earth system, is assessed using stratigraphic criteria and includes geologically novel aspects and geologically will have permanent effects.
The geological cycle of plastics and their use as a stratigraphic indicator of the Anthropocene
The rise of plastics since the mid-20th century, both as a material element of modern life and as a growing environmental pollutant, has been widely described. Their distribution in both the
When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal
Abstract We evaluate the boundary of the Anthropocene geological time interval as an epoch, since it is useful to have a consistent temporal definition for this increasingly used unit, whether the