We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
To save content items to your account,
please confirm that you agree to abide by our usage policies.
If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account.
Find out more about saving content to .
To save content items to your Kindle, first ensure no-reply@cambridge.org
is added to your Approved Personal Document E-mail List under your Personal Document Settings
on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part
of your Kindle email address below.
Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations.
‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi.
‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
The transition from the middle to late Holocene (5000–4000 BP) coincided with profound socioeconomic transformations and intensified regional and trans-regional interactions in late prehistoric China. These environmental and socioeconomic changes gave rise to diverse lifeways and settlement modes that constituted the foundation for the emergence of regional civilisations. In this Element, prehistoric China is divided roughly into the Highlands, Lowlands, and Coastal areas, each with unique environmental and ecological conditions and distinctive technological and economic traditions between 5000–4000 BP. The author gathers and reviews large amounts of environmental and archaeological data, and reconstructs brief environmental and settlement changes and lifeways. The author argues that environmental conditions and subsistence adaptations are two of the engines driving the increased socioeconomic complexity and rise of civilisations in the late prehistoric China. This title is also available as Open Access on Cambridge Core.
Learning is critical for our capacity to govern the environment and adapt proactively to complex and emerging environmental issues. Yet, underlying barriers can challenge our capacity for learning in environmental governance. As a result, we often fail to adequately understand pressing environmental problems or produce innovative and effective solutions. This Element synthesizes insights from extensive academic and applied research on learning around the world to inform both research and practice. We distill the social and structural features of governance to help researchers and practitioners better understand, diagnose, and support learning and more adaptive responses to environmental problems.
Archaeology and cultural evolution theory both predict that environmental variation and population size drive the likelihood of inventions (via individual learning) and their conversion to population-wide innovations (via social uptake). We use the case study of the adoption of the bow and arrow in the Great Basin to infer how patterns of cultural variation, invention, and innovation affect investment in new technologies over time and the conditions under which we could predict cultural innovation to occur. Using an agent-based simulation to investigate the conditions that manifest in the innovation of technology, we find the following: (1) increasing ecological variation results in a greater reliance on individual learning, even when this decreases average fitness due to the costs of learning; (2) decreasing population size increases variability in the types of learning strategies that individuals use; among smaller populations drift-like processes may contribute to randomization in interpopulation cultural diffusion; (3) increasing the mutation rate affects the variability in learning patterns at different rates of environmental variation; and (4) increasing selection pressure increases the reliance on social learning. We provide an open-source R script for the model and encourage others to use it to test additional hypotheses.
Antarctica (Figure 3.1) is at the forefront of the climate change crisis. We know that it is an important player in global circulations of the atmosphere and the ocean, and that the gain/loss of ice on the continent exerts a major control on sea level. We are also aware that Antarctica has been pivotal in modulating past climate change and sea levels. This appreciation has only been achieved through scientific research over the past fifty years – a remarkable evolution in understanding, considering it was a remote and unknown continent in the early 1900s. Indeed, the first expeditions in which targeted scientific discovery was the sole focus date only to the late 1950s. Considering the rapid evolution in our understanding of Antarctica’s ice sheet, and the continent on which it flows, it is worth taking time to review briefly how we arrived at this point.
Greenland has been peopled from the west by several different groups and only once – in the late tenth century ad – from the east, this time by Norse farmers from northern Europe. Unlike the mobile Arctic hunters, the Norse settlers were sedentary, and the society they established in southwest Greenland was based on the natural vegetation, hunting, and trade with their homelands. For almost 500 years the Norse population in Greenland thrived, and then it vanished for reasons not yet fully understood. Several explanations have been put forward: that the small Norse society failed because of inflexible social and economic strategies,1 or fell victim to a combination of unfortunate circumstances,2 or (as recently argued) suffered from organized and systematic violence by invading Inuit.
Antarctic soils provide an excellent setting to test biogeographical patterns across spatial and environmental scales given their relatively simple communities and the dominance of physical factors that create strong environmental gradients. Additional urgency is given by the fact that their unique terrestrial communities are the subject of conservation efforts in a rapidly changing environment. We investigated relationships of soil community assembly and alpha and beta diversity with climatic and environmental parameters across regional and local scales in Maritime Antarctica. We sampled from a regional gradient of sites that differ in habitat severity, ranging from relatively favourable to harsher physicochemical conditions. At the regional scale, bacterial community characteristics and microarthropod abundance varied along this severity gradient, but most measures of fungal communities did not. Microarthropod and microbial communities differed in which soil and climate parameters were most influential, and the specific parameters that influenced each taxon differed across broad and fine spatial scales. This suggests that conservation efforts will need to focus on a large variety of habitat characteristics to successfully encompass diversity across taxa. Because beta diversity was the result of species turnover, conservation efforts also cannot focus on only the most biodiverse sites to effectively preserve all aspects of biodiversity.
Possession Island was one of the first landing places in the Antarctic region, now more than 180 years ago, yet there is little scientific knowledge of this island archipelago in the western Ross Sea. Although the islands are often passed and have been landed on for a few brief hours a number of times, the area is a challenging environment to visit or work in, as weather, sea and ice conditions can be unpredictable.
This paper documents the discovery of the islands, and their history of exploration, the broad range of fleetingly conducted science endeavours, weather and climate and since the 1990s, eco-tourism visits. The islands deserve to be better known, and their rich history provides a foundation for future research and eco-tourism.
Tree-ring series offer considerable potential for the development of environment-sensitive proxy records. However, with traditional increment cores, only small amounts of wood are often available from annual tree-ring sequences. For this reason, it is important to understand the reliability (and reproducibility) of radiocarbon measurements obtained from small-sized samples. Here we report the F14C results from the Chronos 14Carbon-Cycle Facility of modern tropical Australian tree samples over a range of four graphite target sizes from the same rings. Our study shows that similar precision can be obtained from full-sized, half-sized, as well as small-sized graphite targets using standard pretreatment and analysis procedures. However, with a decline in sample size, there was an increase seen in the associated variance of the ages and the smallest target weights started showing a systematic bias. Wiggle-matching accuracy tests, comparing the Southern Hemisphere post-bomb atmospheric calibration curve to the different sample weight sequences, were all significant except for the 200 μgC graphite targets. Our results indicate that samples smaller than 350 μgC have limited accuracy and precision. Overall, reliable measurements of F14C sequences from tree-ring records across a range of sample sizes, with best results found using graphitized samples >350 μgC.
The ninth to the fifth centuries BCE saw a series of significant historical transformations across Cyprus, especially in the growth of towns and in developments in the countryside. In this book, Catherine Kearns argues that changing patterns of urban and rural sedentism drove social changes as diverse communities cultivated new landscape practices. Climatic changes fostered uneven relationships between people, resources like land, copper, and wood, and increasingly important places like rural sanctuaries and cemeteries. Bringing together a range of archaeological, textual, and scientific evidence, the book examines landscapes, environmental history, and rural practices to argue for their collective instrumentality in the processes driving Iron Age political formations. It suggests how rural households managed the countryside, interacted with the remains of earlier generations, and created gathering spaces alongside the development of urban authorities. Offering new insights into landscape archaeologies, Dr Kearns contributes to current debates about society's relationships with changing environments.
Many of the most contentious questions that concern the ecology of helminths could be resolved with data on helminth abundance over the past few decades or centuries, but unfortunately these data are rare. A new sub-discipline – the historical ecology of parasitism – is resurrecting long-term data on the abundance of parasites, an advancement facilitated by the use of biological natural history collections. Because the world's museums hold billions of suitable specimens collected over more than a century, these potential parasitological datasets are broad in scope and finely resolved in taxonomic, temporal and spatial dimensions. Here, we set out best practices for the extraction of parasitological information from natural history collections, including how to conceive of a project, how to select specimens, how to engage curators and receive permission for proposed projects, standard operating protocols for dissections and how to manage data. Our hope is that other helminthologists will use this paper as a reference to expand their own research programmes along the dimension of time.
This chapter provides a review of archaeologies of landscape and outlines where environmental studies reside within these discussions, particularly in the recent rise of climatic and environmental histories of the ancient Mediterranean. Through a review of the challenges of environmental determinism and the interpretive problems of studies of the historical forcing of climatic events in human history, Kearns argues for integrated methodologies that look critically at varied scales of evidence and interpretation. In advocating the study of weathered materials and their instrumentality within ancient landscape studies, the chapter engages with recent archaeological scholarship on materialism that analyzes how things act and effect historical change. Kearns contends that differentiated entanglements of communities and their physical, changing surroundings contributed to transformations in social and political evaluations of land, place, and status.
Earth's geological history is punctuated by episodes of unusually protracted and large-scale volcanic activity, during which huge volumes of igneous rock are added to Earth's surface and crust. Humans have not witnessed this type of large-scale volcanic activity, known as large igneous province volcanism, but it is often temporally associated with profound environmental and climatic changes, such as mass extinction events. In order to understand what triggers these global changes, we need to consider the fluxes of particles and gas emitted by large igneous province-scale volcanic activity and match our projections with the signals left in the geological record. This is a challenging endeavour and this chapter discusses how evidence from today's active volcanoes can teach us not just about the present-day impact of volcanism, but also about these much larger volcanic eruptions that happened tens to hundreds of millions of years ago. The author argues that by peering into volcanoes, we can shed new light on enigmas surrounding the evolution of Earth's environment and biology over its deep geological history.
The archipelago of Svalbard is a good example of an Arctic locale undergoing rapid changes on multiple levels. This contribution is a joint effort of three anthropologists with up-to-date ethnographic data from Svalbard (mostly Longyearbyen and Barentsburg) to frame and interpret interconnected changes. The processes impacting Svalbard are related to issues such as geopolitical interests, and increasing pressure by the Norwegian government to exercise presence and control over the territory. Our interpretations are based on a bottom-up approach, drawing on experiences living in the field. We identify three great ruptures in recent years – the avalanche of 2015, the gradual phasing out of mining enterprises and the COVID-19 pandemic – and show how they further impact, accelerate or highlight preexisting vulnerabilities in terms of socio-economic development, and environmental and climate change. We discuss the shift from coal mining to the industries of tourism, education, and research and development, and the resulting changed social and demographic structure of the settlements. Another facet is the complexity of environmental drivers of change and how they relate to the socio-economic ones. This article serves as an introductory text to the collection of articles published in Polar Record in 2021/2022 with the overarching theme “changing Svalbard”. Issues discussed range from socio-economic change and its implications for local populations including identity of place, through tourism (value creation, mediation, human–environment relations, environmental dilemmas, balancing contradictory trends), to security and risk perception, and environmental and climate change issues.
The production of hazardous pollutants is part of everyday life for most every human; the problem is that the degree of production per person today is greater than it has ever been – and only getting worse. We all participate in this process, but not equally. We are currently in a moment of geologic history where something living is now the single largest driver of planetary change: humans. In the process of creating this change we are also creating substantial and unnecessary human health hazards, what I call environmental violence. Environmental violence (EV) encompasses many activities and processes – but certainly not everything – that humans do, particularly processes of consumption and production that exceed well past meeting basic needs. In this chapter I work through the theoretical threads that underpin the concept of EV and work to situate EV in human evolutionary and geologic history. I also chart out the rest of the book, providing a roadmap of where we are going and the materials, evidence, case studies, and methods that I will employ along the journey.
Edited by
Marie Roué, Centre National de la Recherche Scientifique (CNRS), Paris,Douglas Nakashima, United Nations Educational, Scientific and Cultural Organization (UNESCO), France,Igor Krupnik, Smithsonian Institution, Washington DC
We have entered the era of the Anthropocene. Our rapid transformation of the planet poses a particular threat to socio-ecological systems and the Indigenous peoples who create and sustain them. A strengthened partnership between Indigenous knowledge holders and scientists is required based on decolonized knowledge co-production (DKC). Quite the opposite of scientific extractivism, which selectively exploits local and Indigenous knowledge to its own advantage, and more ambitious than the mere recognition and appraisal of Indigenous knowledge, DKC requires dedicated partners from knowledge systems who have learned through years of collaborative work. This introductory chapter proposes a methodology and ethic for DKC based on a problem-oriented and engaged approach built around mutual trust and benefits, and a profound equity between knowledge systems. It examines the intellectual contributions that laid bare the legacies of colonialism and the hegemony of science, opening the way for DKC: Elinor Ostrom who first coined the term co-production, Bruno Latour and Sheila Jasanoff from science and technology studies, with decisive insights from, among others, Edward Said, Vincent Deloria and Tuhuwai Smith.
This is the first book to present a comprehensive, up to date overview of archaeological and environmental data from the eastern Mediterranean world around 6000 BC. It brings together the research of an international team of scholars who have excavated at key Neolithic and Chalcolithic sites in Syria, Anatolia, Greece, and the Balkans. Collectively, their essays conceptualize and enable a deeper understanding of times of transition and changes in the archaeological record. Overcoming the terminological and chronological differences between the Near East and Europe, the volume expands from studies of individual societies into regional views and diachronic analyses. It enables researchers to compare archaeological data and analysis from across the region, and offers a new understanding of the importance of this archaeological story to broader, high-impact questions pertinent to climate and culture change.
The socio-cultural and environmental shifts that have taken place in southern Italy over the last 30 years can usefully be traced by their impact on folkloric texts which present modifications that tend to emerge progressively over time. An analysis of such modifications to a body of southern Italian folkloric texts – as used in practice over the last three decades – finds that these reflect and are driven by changes in the people's living environment denoting a cultural dilution and a growing distance between people and the natural world, particularly the land. These modifications also expose a shift of emphasis from ends (e.g. food) to means (e.g. money), indicating increased commercial dependence driven by socio-economic changes. These changes are also reflected in folkloric texts which demonstrate a decline of direct, physical experience of some aspects of the natural world while including references relating to the local environment. Understanding these processes allows us to gauge the extent to which verbal folklore connects contemporary societies to past knowledge.
Many of Earth’s large lowland rivers are heavily impacted by land change and hydraulic engineering to support a range of societal demands. Dams and river engineering for flood control have disconnected rivers from floodplains, reduced coastal sediment flux, and driven land subsidence of deltaic wetlands because of reduced sediment loads. Structural modification of lowland rivers alters hydrologic and sedimentary processes, resulting in unintended geomorphic and environmental adjustments that require decades to unfold. Such problems not only degrade associated riparian ecosystems but also increase human vulnerability to flooding. Integrated approaches to lowland river management are needed to reduce flood risk, conserve and restore riparian environments, while ensuring that lowland rivers continue to meet societal demands.