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Sökning: WFRF:(Grinevald Jacques)

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1.
  • Steffen, Will, et al. (författare)
  • Stratigraphic and Earth System approaches to defining the Anthropocene
  • 2016
  • Ingår i: Earth's Future. - 2328-4277. ; 4:8, s. 324-345
  • Forskningsöversikt (refereegranskat)abstract
    • Stratigraphy provides insights into the evolution and dynamics of the Earth System over its long history. With recent developments in Earth System science, changes in Earth System dynamics can now be observed directly and projected into the near future. An integration of the two approaches provides powerful insights into the nature and significance of contemporary changes to Earth. From both perspectives, the Earth has been pushed out of the Holocene Epoch by human activities, with the mid-20th century a strong candidate for the start date of the Anthropocene, the proposed new epoch in Earth history. Here we explore two contrasting scenarios for the future of the Anthropocene, recognizing that the Earth System has already undergone a substantial transition away from the Holocene state. A rapid shift of societies toward the UN Sustainable Development Goals could stabilize the Earth System in a state with more intense interglacial conditions than in the late Quaternary climate regime and with little further biospheric change. In contrast, a continuation of the present Anthropocene trajectory of growing human pressures will likely lead to biotic impoverishment and a much warmer climate with a significant loss of polar ice.
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2.
  • Steffen, Will, et al. (författare)
  • The Anthropocene : conceptual and historical perspectives
  • 2011
  • Ingår i: Philosophical Transactions. Series A. - : The Royal Society. - 1364-503X .- 1471-2962. ; 369:1938, s. 842-867
  • Tidskriftsartikel (refereegranskat)abstract
    • The human imprint on the global environment has now become so large and active that it rivals some of the great forces of Nature in its impact on the functioning of the Earth system. Although global-scale human influence on the environment has been recognized since the 1800s, the term Anthropocene, introduced about a decade ago, has only recently become widely, but informally, used in the global change research community. However, the term has yet to be accepted formally as a new geological epoch or era in Earth history. In this paper, we put forward the case for formally recognizing the Anthropocene as a new epoch in Earth history, arguing that the advent of the Industrial Revolution around 1800 provides a logical start date for the new epoch. We then explore recent trends in the evolution of the Anthropocene as humanity proceeds into the twenty-first century, focusing on the profound changes to our relationship with the rest of the living world and on early attempts and proposals for managing our relationship with the large geophysical cycles that drive the Earth’s climate system.
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3.
  • Zalasiewicz, Jan, et al. (författare)
  • Introduction: : Buffon and the History of the Earth
  • 2018. - 1
  • Ingår i: The Epochs of Nature. - Chicago, IL and London : University of Chicago Press. - 9780226395432 - 9780226395579 ; , s. xiii-xxxiv
  • Bokkapitel (refereegranskat)
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