Changes in physical, biological, and chemical processes in soils and waters have resulted from human activities that include urban development, industrialization, agriculture and mining,

and construction and removal of dams and levees. Human activity has also been linked to our warming climate over the past several decades, which in turn induces further alterations in Earth processes and systems. Human-induced changes to Earth’s surface, oceans, Bortezomib cryosphere, ecosystems, and climate are now so great and rapid that the concept of a new geological epoch defined by human activity, the Anthropocene, is widely debated (Crutzen and Stoermer, 2000). A formal proposal to name this new epoch within the Geological Time Scale is in development for consideration by the International Commission on Stratigraphy (Zalasiewicz et al., 2011). A strong need exists to accelerate scientific research to understand, predict, and respond to rapidly changing processes on Earth.

Human impact on the environment has been studied beginning at least a century and a half ago (Marsh, 1864), increasingly since Thomas’ publication (Thomas, 1956), Man’s Role in changing selleck kinase inhibitor the Face of the Earth in 1956. Textbooks and case studies have documented variations in the human impacts and responses on Earth; many journals have similarly approached the topic from both natural and social scientific perspectives. Yet, Anthropocene responds to new and emerging challenges and opportunities of our time. It provides a venue for addressing a Grand Challenge identified recently by the U.S. National Research Council (2010) – How Will Earth’s Surface Evolve in the “Anthropocene”? Meeting this challenge calls for broad interdisciplinary collaborations to account explicitly for human interactions with Earth systems, involving development and application of new conceptual frameworks

and integrating methods. Anthropocene aims to stimulate and integrate research across many scientific fields and over multiple spatial and temporal scales. Understanding from and predicting how Earth will continue to evolve under increasing human interactions is critical to maintaining a sustainable Earth for future generations. This overarching goal will thus constitute a main focus of the Journal. Anthropocene openly seeks research that addresses the scale and extent of human interactions with the atmosphere, cryosphere, ecosystems, oceans, and landscapes. We especially encourage interdisciplinary studies that reveal insight on linkages and feedbacks among subsystems of Earth, including social institutions and the economy. We are concerned with phenomena ranging over time from geologic eras to single isolated events, and with spatial scales varying from grain scale to local, regional, and global scales.