Book contents
- Frontmatter
- Contents
- Preface
- Editors’Acknowledgement
- 1 Introduction: Towards a Historical View of Humanity and the Biosphere
- 2 Introductory Overview: the Expanding Anthroposphere
- 3 The Holocene: Global Change and Local Response
- 4 Environment and the Great Transition: Agrarianization
- 5 Exploring the Past: on Methods and Concepts
- 6 Increasing Social Complexity
- 7 Empire: the Romans in the Mediterranean
- 8 Understanding: Fragments of a Unifying Perspective
- 9 Population and Environment in Asia since 1600 AD
- 10 The Past 250 Years: Industrialization and Globalization
- 11 Back to Nature? The Punctuated History of a Natural Monument
- 12 Conclusions: Retrospect and Prospects
- Notes
- Bibliography
- About the Authors
- Index of Subjects
- Index of Names
- Index of Geographic Names
3 - The Holocene: Global Change and Local Response
Published online by Cambridge University Press: 25 January 2021
- Frontmatter
- Contents
- Preface
- Editors’Acknowledgement
- 1 Introduction: Towards a Historical View of Humanity and the Biosphere
- 2 Introductory Overview: the Expanding Anthroposphere
- 3 The Holocene: Global Change and Local Response
- 4 Environment and the Great Transition: Agrarianization
- 5 Exploring the Past: on Methods and Concepts
- 6 Increasing Social Complexity
- 7 Empire: the Romans in the Mediterranean
- 8 Understanding: Fragments of a Unifying Perspective
- 9 Population and Environment in Asia since 1600 AD
- 10 The Past 250 Years: Industrialization and Globalization
- 11 Back to Nature? The Punctuated History of a Natural Monument
- 12 Conclusions: Retrospect and Prospects
- Notes
- Bibliography
- About the Authors
- Index of Subjects
- Index of Names
- Index of Geographic Names
Summary
Climatic and environmental catastrophes are only catastrophes because human beings and activities are involved. For nature alone, climate changes, floods, earthquakes, volcanic eruptions, etc. are a self-evident part of its dynamic processes.
Messerli, 2000: 477Introduction
Nature is change. Geological forces of change are a mixture of slow, constant processes and sudden pulsed events such as earthquakes; such forces have been in operation ever since planet Earth came into being. Their domain, the lithosphere, interacts with the hydrosphere and the atmosphere, each having its own suite of processes. How these processes interact, particularly with human populations, is the focus of this chapter. Let us start at the beginning. As life evolved over the course of time, large parts of the earth's crust became covered with vegetation. The biosphere was born. Animals appeared, which in turn modified the vegetation cover. Natural landscapes developed from the interplay of geological, physico-chemical and biological processes. Then, only recently on the geological clock, the genus Homo entered the scene – another step in the unfolding complexity of the earth.With the emergence of cognition, language and culture, the notion of an environment-for-humans got its meaning. The anthroposphere had come into existence. The ‘natural’ landscape became, as an environment-for-humans, dotted with ‘human’ imprints, the material remains of which now help us to construct the puzzle of past changes. In addition to these artefacts, numerous symbolic and religious structures were built, some of which are present, others are lost but all are harder to reconstruct than material remains.
There is little doubt that the physical, biological and climatic environment has influenced human populations as civilizations emerged, rose and declined. Transformation processes, increasingly leading to completely human-dominated landscapes, can be collectively referred to as ‘environmental change’. This is the subject of recent scientific disciplines such as historical ecology, environmental history or human ecology. This chapter then is about nature and the environment as experienced, and possibly acted upon by human groups during the last 10,000 years. This length of time, forming the most recent geological period of the Holocene, follows the Last Glacial period and encompasses the development of hunter-gatherers, early agriculturists and increasingly sedentary life. These topics can be investigated from many different stances that have developed into rather specialized disciplines with their own empirical concepts, facts, hypotheses and theories.
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- Mappae MundiHumans and their Habitats in a Long-Term Socio-Ecological Perspective, pp. 47 - 70Publisher: Amsterdam University PressPrint publication year: 2002