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Open AccessJournal ArticleDOI

Human responses to climate and ecosystem change in ancient Arabia.

TLDR
Data from northern Arabia suggest that Holocene populations responded to environmental challenges through high mobility, managing water sources, and transforming their economies, which illustrated diverse strategies to resilience and provide important lessons for a world in which climate predictions forecast dramatic changes in temperature and precipitation.
Abstract
Recent interdisciplinary archaeological and paleoenvironmental research in the Arabian peninsula is transforming our understanding of ancient human societies in their ecological contexts. Hypotheses about the cultural and demographic impacts of a series of droughts have primarily been developed from the environmental and archaeological records of southeastern Arabia. Here we examine these human-environment interactions by integrating ongoing research from northern Arabia. While droughts and extreme environmental variability in the Holocene had significant impacts on human societies, responses varied across space and time and included mobility at various scales, as well as diverse social, economic and cultural adaptations, such as the management of water resources, the introduction of pastoral lifeways, and the construction of diverse types of stone structures. The long-term story of human societies in Arabia is one of resilience in the face of climate change, yet future challenges include rising temperatures and flash flooding. The history of human responses to climatic and ecosystem changes in Arabia can provide important lessons for a planet facing catastrophic global warming and environmental change.

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Citations
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Defining the Anthropocene

TL;DR: The evidence suggests that of the various proposed dates two do appear to conform to the criteria to mark the beginning of the Anthropocene: 1610 and 1964.
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Large-scale features and evaluation of the PMIP4-CMIP6 midHolocene simulations

TL;DR: The PMIP4-CMIP6 ensemble for the mid-Holocene has a global mean temperature change of −0.3 ǫK, which is − 0.2 ôK cooler than the previous generation (PMIP3 -CMIP5) of simulations as mentioned in this paper.
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Mobilizing the past to shape a better Anthropocene.

TL;DR: In this paper, the authors argue that information from the past has a valuable role to play in enhancing the sustainability and resilience of our societies and highlight the ways that past data can be mobilized for a variety of efforts, from supporting conservation to increasing agricultural sustainability and food security.
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Holocene regional population dynamics and climatic trends in the Near East: A first comparison using archaeo-demographic proxies

TL;DR: In this paper, a long-term trend in human population and climate from the Late Pleistocene to the Late Holocene (14,000-2500 cal. yr. BP) was analyzed using a large corpus of archaeo-demographic data.
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Archaeology, climate, and global change in the Age of Humans

TL;DR: Contributions by archaeology—the study of the human past—to interdisciplinary research programs designed to evaluate current social and environmental challenges and contribute to solutions for the future are highlighted.
References
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Journal ArticleDOI

High-resolution mapping of global surface water and its long-term changes

TL;DR: Using three million Landsat satellite images, this globally consistent, validated data set shows that impacts of climate change and climate oscillations on surface water occurrence can be measured and that evidence can be gathered to show how surface water is altered by human activities.
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Global warming and changes in drought

TL;DR: In this article, a commonly used drought index and observational data are examined to identify the cause of these discrepancies, and the authors indicate that improvements in the quality and coverage of precipitation data and quantification of natural variability are necessary to provide a better understanding of how drought is changing.
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Global flood risk under climate change

TL;DR: This article used several climate models to estimate the global risk of flooding at the end of the century and showed that vulnerability is dependent on the degree of warming and the interannual variability in precipitation.
Journal ArticleDOI

Defining the Anthropocene

TL;DR: The authors reviewed the historical genesis of the Anthropocene Epoch idea and assessed anthropogenic signatures in the geological record against the formal requirements for the recognition of a new epoch, finding that of the various proposed dates two do appear to conform to the criteria to mark the beginning of the anthropocene: 1610 and 1964.
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What was the impact of the 536 AD climatic event on the Arabian peninsula?

The provided paper does not mention the specific impact of the 536 AD climatic event on the Arabian peninsula.