Libros: "Climatic tracers"

1

K, Swart P., ed. Climate change in continental isotopic records. Washington, DC: American Geophysical Union, 1993.

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2

1955-, Dawson Todd E. y Siegwolf Rolf T. W, eds. Stable isotopes as indicators of ecological change. Amsterdam: Elsevier Academic Press, 2007.

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3

National Climatic Data Center (U.S.) y United States. Naval Meteorology and Oceanography Command. Fleet Numerical Meteorology and Oceanography Detachment., eds. Global tropical/extratropical cyclone climatic atlas. 2^a ed. [Asheville, N.C.]: The Command, 1996.

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4

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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5

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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6

Tze-shan, Cheng. A modified persistence-climatology method to forecast tropical cyclone movement. Hong Kong: Royal Observatory, 1986.

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7

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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8

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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9

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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10

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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11

Piper, David Z. Trace-element deposition in the Cariaco Basin, Venezuela shelf, under sulfate-reducing conditions: A history of the local hydrography and global climate, 20 ka to the present. [Washington, D.C.]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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12

W, Ko M. K. y United States. National Aeronautics and Space Administration., eds. Semi-annual report on coupling processes between atmospheric chemistry and climate: NAS5-97039. [Washington, DC: National Aeronautics and Space Administration, 1997.

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13

Ajiboye, Paul. Methane sulphonic acid as a tracer for non sea salt sulphate: Implications for global climate regulation. Oxford: Oxford Brookes University, 1999.

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14

W, Ko Malcolm K. y United States. National Aeronautics and Space Administration., eds. Semi-annual report on coupling processes between atmospheric chemistry and climate: NAS5-97039. [Washington, DC: National Aeronautics and Space Administration, 1999.

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15

Whyte, Jeffrey. The Birth of Psychological War. Oxford: British Academy, 2023. http://dx.doi.org/10.5871/bacad/9780197267493.001.0001.

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Abstract In the current climate of concern over disinformation and the so-called ‘post-truth era,’ psychological warfare has returned to discussions of national and international politics. Yet questions concerning psychological warfare — when, where, and how it came about — are poorly understood. This monograph reveals the complexity of these questions by investigating the historical-geographical contexts in which psychological warfare emerged. Identifying the home front and the foreign theatre as its key contexts, this monograph traces psychological warfare’s trajectory from the Second World War, to the ‘Cold War of ideas’ in Europe, to the counterinsurgency campaigns of the Vietnam war. While psychological warfare often claims to make war more humane, this book shows that in practice it has expanded the scale and scope of military violence. Despite psychological warfare’s perennial failures to ‘win hearts and minds’ abroad, this monograph shows that its influence nevertheless continues to transform the practice and meaning of contemporary warfighting and international relations.

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16

1968-, Baker Andy, ed. Speleothem science: From process to past environments. Hoboken, N.J: Wiley, 2012.

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17

Lohmann, K. C., S. Savin, J. McKenzie y P. K. Swart. Climate Change in Continental Isotopic Records. Wiley & Sons, Limited, John, 2013.

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18

Dawson, Todd E. y Rolf Siegwolf. Stable Isotopes As Indicators of Ecological Change. Elsevier Science & Technology Books, 2011.

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19

Furuhata, Yuriko. Climatic Media. Duke University Press, 2022. http://dx.doi.org/10.1215/9781478022435.

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In Climatic Media, Yuriko Furuhata traces climate engineering from the early twentieth century to the present, emphasizing the legacies of Japan’s empire building and its Cold War alliance with the United States. Furuhata boldly expands the scope of media studies to consider technologies that chemically “condition” Earth’s atmosphere and socially “condition” the conduct of people, focusing on the attempts to monitor and modify indoor and outdoor atmospheres by Japanese scientists, technicians, architects, and artists in conjunction with their American counterparts. She charts the geopolitical contexts of what she calls climatic media by examining a range of technologies such as cloud seeding and artificial snowflakes, digital computing used for weather forecasting and weather control, cybernetics for urban planning and policing, Nakaya Fujiko’s fog sculpture, and the architectural experiments of Tange Lab and the Metabolists, who sought to design climate-controlled capsule housing and domed cities. Furuhata’s transpacific analysis offers a novel take on the elemental conditions of media and climate change.

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20

Mora, Germán y Donna Surge. Isotopic and elemental tracers of Cenozoic climate change. Geological Society of America, 2005. http://dx.doi.org/10.1130/spe395.

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21

Deutsche Bank. Deutsche Asset Management. Global climate change policy tracker: An investor's assessment. 2009.

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22

House, Booksy. Sleep Tracker: Climate Change National Park. Independently Published, 2021.

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23

Special Paper 395: Isotopic and elemental tracers of Cenozoic climate change. Geological Society of America, 2005. http://dx.doi.org/10.1130/0-8137-2395-7.

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24

Fujiko, Fujio F. y Masanori Ōnishi. Doraemon Kagaku Wārudo: Tenki to kishō no fushigi. 2014.

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25

Woodburne, Michael O., Gregg F. Gunnell y Richard K. Stucky. Land Mammal Faunas of North America Rise and Fall During the Early Eocene Climatic Optimum. Denver Museum of Nature & Science, 2009. http://dx.doi.org/10.55485/rkck3803.

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Climatic warming at the beginning of the Early Eocene Climatic Optimum (EECO) resulted in major increases in plant diversity and habitat complexity reflective of temporally unique, moist, paratropical conditions from about 53–50 Ma in the Western Interior of North America. In the early part of the EECO, mammalian faunal diversity increased at both local and continental scales in conjunction with a major increase in tropicality resulting from mean annual temperatures reaching 23 ̊C and mean annual precipitation approaching 150 cm/yr. A strong episode of taxonomic origination (high number of first appearances) in the latest Wasatchian and earliest Bridgerian Land Mammal Ages apparently was in response to these greatly diversified floral and habitat associations along with increasing temperature and precipitation. This is in contrast to a similar increase in first appearances at the beginning of the Wasatchian (Paleocene-Eocene Thermal Maximum, or PETM) that can be traced instead to climate-induced transcontinental immigration. In the later part of the EECO, from Br-1b–Br-3, climatic deterioration resulted in a major loss of faunal diversity at both continental and local levels, apparently mirroring climatic deterioration. Relative abundance shifted from diverse, evenly distributed communities to much less diverse, skewed distributions dominated by the condylarth Hyopsodus. Evolutionary innovation through the 53–50 Ma interval included a modest overall increase in body size and increased efficiency in carnivory and folivory as reflected by within-lineage patterns of evolution. Rather than being “optimum,” the EECO engendered the greatest episode of mammalian faunal turnover of the first 15 million years of the Cenozoic era, with both first and last appearances at their highest levels. Both the PETM and EECO faunas were climatically shaped.

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26

(Editor), German Mora y Donna M. Surge (Editor), eds. Isotopic And Elemental Tracers of Cenozoic Climate Change (Special Papers (Geological Society of America)). Geological Society of America, 2005.

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27

Gerrard, Michael B. United States Climate Change Law. Editado por Kevin R. Gray, Richard Tarasofsky y Cinnamon Carlarne. Oxford University Press, 2016. http://dx.doi.org/10.1093/law/9780199684601.003.0027.

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This chapter presents an overview of climate change law in the United States, given the global impact of its domestic and international climate change policies. It traces the evolution of US climate change policy under different presidents, and discusses emerging programs under the Clean Air Act (CAA). Under the CAA, the Environmental Protection Agency (EPA) issues emissions standards, and under the Energy Policy Conservation Act, the National Highway Traffic Safety Administration (NHTSA) issues Corporate Average Fuel Economy (CAFE) standards. The chapter also describes the protection of endangered species under the Endangered Species Act (ESA). The ESA directs the Fish and Wildlife Service to designate certain species as endangered or threatened; for marine species that task falls to the National Marine Fisheries Service.

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28

Dubash, Navroz K. y Lavanya Rajamani. Multilateral Diplomacy on Climate Change. Editado por David M. Malone, C. Raja Mohan y Srinath Raghavan. Oxford University Press, 2010. http://dx.doi.org/10.1093/oxfordhb/9780198743538.013.48.

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This chapter reviews India’s foreign policy on climate change, arguing that while it is marked by tactical virtuosity, it increasingly exhibits strategic vacuity. The chapter traces the evolution of India’s role in international climate negotiations, noting particularly India’s key role in highlighting equity and enshrining the concept of ‘common but differentiated responsibilities and respective capabilities’ as a cornerstone of the negotiation process. The chapter then examines the turbulent phase from 2007 onwards, when India, along with other large developing country allies, experimented with new articulations of climate policy. This discussion explores the emergent drivers of Indian climate policy, including international pressures, shifting domestic political context, the emergence of ‘co-benefits’ as a framing concept, and the role of key personalities. The chapter concludes by suggesting that an exclusive emphasis on an equitable climate deal should transition to an approach that provides equal attention to equity and effectiveness in international climate outcomes.

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29

Retro Climate Change Is Real Earth Planet Nature Conservancy Raglan Baseball - Saving Tracker. Independently Published, 2021.

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30

Retro Climate Change Is Real Earth Planet Nature Conservancy Raglan Baseball - Debt Tracker. Independently Published, 2021.

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31

Personal Expense Tracker - Retro Vintage Bumble Bee Save the Bees Keeper Climate Change. Independently Published, 2021.

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32

Simple Weight Tracker - Retro Vintage Bumble Bee Save the Bees Keeper Climate Change. Independently Published, 2021.

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33

Personal Expense Tracker - Retro Vintage Bumble Bee Save the Bees Keeper Climate Change. Independently Published, 2021.

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34

Crawford, Neta C. The Pentagon, Climate Change, and War. The MIT Press, 2022. http://dx.doi.org/10.7551/mitpress/14617.001.0001.

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How the Pentagon became the world's largest single greenhouse gas emitter and why it's not too late to break the link between national security and fossil fuel consumption. The military has for years (unlike many politicians) acknowledged that climate change is real, creating conditions so extreme that some military officials fear future climate wars. At the same time, the U.S. Department of Defense—military forces and DOD agencies—is the largest single energy consumer in the United States and the world's largest institutional greenhouse gas emitter. In this eye-opening book, Neta Crawford traces the U.S. military's growing consumption of energy and calls for a reconceptualization of foreign policy and military doctrine. Only such a rethinking, she argues, will break the link between national security and fossil fuels. The Pentagon, Climate Change, and War shows how the U.S. economy and military together have created a deep and long-term cycle of economic growth, fossil fuel use, and dependency. This cycle has shaped U.S. military doctrine and, over the past fifty years, has driven the mission to protect access to Persian Gulf oil. Crawford shows that even as the U.S. military acknowledged and adapted to human-caused climate change, it resisted reporting its own greenhouse gas emissions. Examining the idea of climate change as a “threat multiplier” in national security, she argues that the United States faces more risk from climate change than from lost access to Persian Gulf oil—or from most military conflicts. The most effective way to cut military emissions, Crawford suggests provocatively, is to rethink U.S. grand strategy, which would enable the United States to reduce the size and operations of the military.

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35

Fei, Jie. Meteorological History and Historical Climate of China. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.594.

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The Chinese meteorological records could be traced back to the oracle-bone inscriptions of the Shang Dynasty (c. 1600 bc–c. 1046 bc). For the past 3,000 years, continuous meteorological records are available in official histories, chronicles, local gazetteers, diaries, and other historical materials. Ever since the Qin Dynasty (221–207 bc), precipitation reports to the central government were officially organized; however, only those of the Qing Dynasty (1644–1912 ad) are extant, and they have been widely used to reconstruct precipitation variability.Modern meteorological knowledge began to be introduced in China during the late Ming Dynasty (1368–1644 ad). Modern meteorological observation possibly began in the 17th century, whereas continuous meteorological observation records go back to the mid-19th century.Previous researches have reconstructed the chronologies of the temperature change in China during the past 2,000 years, and the Medieval Warm Period and Little Ice Age were identified. With regard to precipitation variability, yearly charts of dryness/wetness in China for the past 500 years were produced. Several chronologies of dust storm, plum rain (Meiyu), and typhoon were also established. Large volcanic eruptions resulted in short scale abrupt cooling in China during the past 2,000 years. Climatic change was significantly related to the war occurrences and dynastic cycles in historical China.

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36

Passarelli, Richard, David Michel y William Durch. From “Inconvenient Truth” to Effective Governance. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198805373.003.0008.

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The Earth’s climate system is a global public good. Maintaining it is a collective action problem. This chapter looks at a quarter-century of efforts to understand and respond to the challenges posed by global climate change and why the collective political response, until very recently, has seemed to lag so far behind our scientific knowledge of the problem. The chapter tracks the efforts of the main global, intergovernmental process for negotiating both useful and politically acceptable responses to climate change, the UN Framework Convention on Climate Change, but also highlights efforts by scientific and environmental groups and, more recently, networks of sub-national governments—especially cities—and of businesses to redefine interests so as to meet the dangers of climate system disruption.

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37

Fay, Jennifer. Inhospitable World. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190696771.001.0001.

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Inhospitable World explores the connection between cinema and artificial weather, climates, and even planets in or on which hospitality and survival are at stake. Cinema’s dominant mode of aesthetic world-making is often at odds with the very real human world it is meant to simulate. The chapters in this book take the reader to a scene—the mise-en-scène—where human world-making is undone by the force of human activity, whether it is explicitly for the sake of making a film, or for practicing war and nuclear science, or for the purpose of addressing climate change in ways that exacerbate its already inhospitable effects. The episodes in this book emphasize our always unnatural and unwelcoming environment as a matter of production, a willed and wanted milieu, however harmful, that is inseparable from but also made perceivable through film. While no one film or set of films adds up to a totalizing explanation of climate change, cinema enables us to glimpse anthropogenic environments as both an accidental effect of human activity and a matter of design. Chapters on Buster Keaton, American atomic test films, film noir, the art of China’s Three Gorges Dam, and films of early Antarctic exploration trace parallel histories of film and location design that spell out the ambitions, sensations, and narratives of the Anthropocene, especially as it consolidates into the Great Acceleration starting in 1945.

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38

Benestad, Rasmus. Climate in the Barents Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.655.

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The Barents Sea is a region of the Arctic Ocean named after one of its first known explorers (1594–1597), Willem Barentsz from the Netherlands, although there are accounts of earlier explorations: the Norwegian seafarer Ottar rounded the northern tip of Europe and explored the Barents and White Seas between 870 and 890 ce, a journey followed by a number of Norsemen; Pomors hunted seals and walruses in the region; and Novgorodian merchants engaged in the fur trade. These seafarers were probably the first to accumulate knowledge about the nature of sea ice in the Barents region; however, scientific expeditions and the exploration of the climate of the region had to wait until the invention and employment of scientific instruments such as the thermometer and barometer. Most of the early exploration involved mapping the land and the sea ice and making geographical observations. There were also many unsuccessful attempts to use the Northeast Passage to reach the Bering Strait. The first scientific expeditions involved F. P. Litke (1821±1824), P. K. Pakhtusov (1834±1835), A. K. Tsivol’ka (1837±1839), and Henrik Mohn (1876–1878), who recorded oceanographic, ice, and meteorological conditions.The scientific study of the Barents region and its climate has been spearheaded by a number of campaigns. There were four generations of the International Polar Year (IPY): 1882–1883, 1932–1933, 1957–1958, and 2007–2008. A British polar campaign was launched in July 1945 with Antarctic operations administered by the Colonial Office, renamed as the Falkland Islands Dependencies Survey (FIDS); it included a scientific bureau by 1950. It was rebranded as the British Antarctic Survey (BAS) in 1962 (British Antarctic Survey History leaflet). While BAS had its initial emphasis on the Antarctic, it has also been involved in science projects in the Barents region. The most dedicated mission to the Arctic and the Barents region has been the Arctic Monitoring and Assessment Programme (AMAP), which has commissioned a series of reports on the Arctic climate: the Arctic Climate Impact Assessment (ACIA) report, the Snow Water Ice and Permafrost in the Arctic (SWIPA) report, and the Adaptive Actions in a Changing Arctic (AACA) report.The climate of the Barents Sea is strongly influenced by the warm waters from the Norwegian current bringing heat from the subtropical North Atlantic. The region is 10°C–15°C warmer than the average temperature on the same latitude, and a large part of the Barents Sea is open water even in winter. It is roughly bounded by the Svalbard archipelago, northern Fennoscandia, the Kanin Peninsula, Kolguyev Island, Novaya Zemlya, and Franz Josef Land, and is a shallow ocean basin which constrains physical processes such as currents and convection. To the west, the Greenland Sea forms a buffer region with some of the strongest temperature gradients on earth between Iceland and Greenland. The combination of a strong temperature gradient and westerlies influences air pressure, wind patterns, and storm tracks. The strong temperature contrast between sea ice and open water in the northern part sets the stage for polar lows, as well as heat and moisture exchange between ocean and atmosphere. Glaciers on the Arctic islands generate icebergs, which may drift in the Barents Sea subject to wind and ocean currents.The land encircling the Barents Sea includes regions with permafrost and tundra. Precipitation comes mainly from synoptic storms and weather fronts; it falls as snow in the winter and rain in the summer. The land area is snow-covered in winter, and rivers in the region drain the rainwater and meltwater into the Barents Sea. Pronounced natural variations in the seasonal weather statistics can be linked to variations in the polar jet stream and Rossby waves, which result in a clustering of storm activity, blocking high-pressure systems. The Barents region is subject to rapid climate change due to a “polar amplification,” and observations from Svalbard suggest that the past warming trend ranks among the strongest recorded on earth. The regional change is reinforced by a number of feedback effects, such as receding sea-ice cover and influx of mild moist air from the south.

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39

Chitalkar, Poorvi y David M. Malone. India and Global Governance. Editado por David M. Malone, C. Raja Mohan y Srinath Raghavan. Oxford University Press, 2010. http://dx.doi.org/10.1093/oxfordhb/9780198743538.013.42.

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India’s engagement with the institutions and norms of global governance has evolved significantly since independence in 1947. This chapter traces the evolution—beginning with early engagement with international organizations under Nehru, to the waning of its enthusiasm for multilateralism in the 1960s and 1970s, and its struggle for greater voice and recognition internationally in the twenty-first century. Through the prism of its quest for a permanent seat in the UN Security Council, its approach to climate change negotiations, global economic diplomacy, and its engagement with global norms, this chapter traces India’s rise as a vital player in the rebalancing of international relations in a multipolar world. However, despite its tremendous progress, some ongoing challenges continue to constrain India’s meaningful participation in global governance at times. The chapter concludes with an assessment of India’s contribution to global governance and its prospects as a stakeholder and shareholder on the global stage.

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40

Barr, Charles. British Cinema: A Very Short Introduction. Oxford University PressOxford, 2022. http://dx.doi.org/10.1093/actrade/9780199688333.001.0001.

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Abstract British Cinema: A Very Short Introduction discusses cinema in Britain, considering its films and film-makers as well as its studios and sponsorships. It does this against the backdrop of changing artistic, socio-political, and industrial climates up to the present day. Cinema is indeed a powerful cultural medium, both reflecting and influencing society. The role of British cinema has been particularly controversial; it is sometimes derided, but also vigorously celebrated, especially for specific films and film-makers. This VSI traces how British cinema has developed its own unique path, and has been admired for its innovative approaches and distinctive artistic language.

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41

Radner, Karen. Assyrians and Urartians. Editado por Gregory McMahon y Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0033.

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This article traces the interactions between Assyria and Urartu, military and otherwise, and their impact on the neighboring Anatolian kingdoms, especially the chain of buffer states situated between Assyria's northern and Urartu's southern border. To the Assyrian mind, Urartu was on one hand an anti-Assyria, the archenemy and eternal temptation for its vassals, and on the other a mirror image, a kind of Assyria in the mountains; inscriptions and archival materials alike attribute Assyrian concepts to Biainili, for example, by superimposing the Assyrian administrative structure onto the other country, referring to provinces and governors and using various specifically Assyrian titles for Urartian officials. This tends to promote the idea that the two kingdoms were very much alike, but the fact that climatic conditions and the economic basis of Assyria and Urartu were very different should make it clear that this assumption is implausible. The various states situated in the border region between Assyria and Urartu, too, had their own distinct identities and traditions.

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42

Woodward, Jamie, ed. The Physical Geography of the Mediterranean. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780199268030.001.0001.

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This volume explores the climates, landscapes, ecosystems and hazards that comprise the Mediterranean world. It traces the development of the Mediterranean landscape over very long timescales and examines modern processes and key environmental issues in a wide range of settings. The Mediterranean is the only region on Earth where three continents meet and this interaction has produced a very distinctive Physical Geography. This book examines the landscapes and processes at the margins of these continents and the distinctive marine environment between them. Catastrophic earthquakes, explosive volcanic eruptions and devastating storms and floods are intimately bound up within the history and mythology of the Mediterranean world. This is a key region for the study of natural hazards because it offers unrivalled access to long records of hazard occurrence and impact through documentary, archaeological and geological archives. The Mediterranean is also a biodiversity hotspot; it has been a meeting place for plants, animals and humans from three continents throughout much of its history. The Quaternary records of these interactions are more varied and better preserved than in any other part of the world. These records have provided important new insights into the tempo of climate, landscape and ecosystem change in the Mediterranean region and beyond. The region is unique because of the very early and widespread impact of humans in landscape and ecosystem change - and the richness of the archaeological and geological archives that chronicle this impact. This book examines this history and these interactions and places current environmental issues in long term context.

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43

Esler, Karen J., Anna L. Jacobsen y R. Brandon Pratt. Transformation. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198739135.003.0008.

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Extensive habitat loss and habitat conversion has occurred across all mediterranean-type climate (MTC) regions, driven by increasing human populations who have converted large tracts of land to production, transport, and residential use (land-use, land-cover change) while simultaneously introducing novel forms of disturbance to natural landscapes. Remaining habitat, often fragmented and in isolated or remote (mountainous) areas, is threatened and degraded by altered fire regimes, introduction of invasive species, nutrient enrichment, and climate change. The types and impacts of these threats vary across MTC regions, but overall these drivers of change show little signs of abatement and many have the potential to interact with MTC region natural systems in complex ways.

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44

Boelhower, William. The Influence of Atlantic Studies on American Literary Scholarship. Oxford University Press, 2016. http://dx.doi.org/10.1093/oxfordhb/9780199935338.013.35.

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This article traces the important paradigm shift from Atlantic history to Atlantic studies. It then identifies the creative tensions generated by a three-dimensional conception of cis-Atlantic, trans-Atlantic, and circum-Atlantic perspectivism. With this new hermeneutic climate in mind, it turns to a discussion of recent U.S. literary scholarship, above all in terms of a select number of exemplars that self-consciously acknowledge and depart from the pathbreaking work of Paul Gilroy, Joseph Roach, and a number of historians of slavery and the African diaspora, such as Marcus Rediker, Peter Linebaugh, David Brion Davis, and Orlando Patterson.

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45

Betts, Matthew. Zooarchaeology and the Reconstruction of Ancient Human-Animal Relationships in the Arctic. Editado por Max Friesen y Owen Mason. Oxford University Press, 2016. http://dx.doi.org/10.1093/oxfordhb/9780199766956.013.8.

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Permafrost-preserved faunal assemblages from Arctic archaeological sites provide a high-resolution record of animal exploitation, ancient ecosystems, and climate. This chapter provides a review of what more than 90 years of archaeofaunal research has revealed about human-animal relationships in the Arctic and Aleutian Subarctic. Taking an alternate approach, the overview focuses on the evidence for the procurement, butchery, storage, and consumption of specific northern vertebrate and molluscan taxa, beginning from the earliest archaeological traces and tracking exploitation strategies geographically through time and space. Additionally, related paleoecological research, methodological advancements, and studies which address the social and ideational correlates of animal exploitation and consumption are reviewed.

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46

Vincent, Warwick F. Lakes: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198766735.001.0001.

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From the mysterious depths of Lake Vostok, Antarctica, to tropical floodplain lakes, inland seas, hydro-reservoirs, and numerous waterbodies in our local environment, lakes encompass a huge diversity of shapes, sizes, depths, colours, and even salinities. Lakes are important, unique ecosystems, providing us with drinking water and food. Lakes: A Very Short Introduction introduces lake science (‘limnology’), discussing the importance of sustaining these complex ecosystems; and the impact on lake biodiversity of features such as climate, seasons, salinity, and sedimentation. It traces the origins of lake science from François Forel’s seminal work on Lake Geneva to modern approaches, such as environmental sensors, satellite observations, stable isotope analysis, and DNA-based technologies.

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47

Povinelli, Elizabeth A. Between Gaia and Ground. Duke University Press, 2021. http://dx.doi.org/10.1215/9781478021872.

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In Between Gaia and Ground Elizabeth A. Povinelli theorizes the climatic, environmental, viral, and social catastrophe present as an ancestral catastrophe through which that Indigenous and colonized peoples have been suffering for centuries. In this way, the violence and philosophies the West relies on now threaten the West itself. Engaging with the work of Glissant, Deleuze and Guattari, Césaire, and Arendt, Povinelli highlights four axioms of existence—the entanglement of existence, the unequal distribution of power, the collapse of the event as essential to political thought, and the legacies of racial and colonial histories. She traces these axioms' inspiration in anticolonial struggles against the dispossession and extraction that have ruined the lived conditions for many on the planet. By examining the dynamic and unfolding forms of late liberal violence, Povinelli attends to a vital set of questions about changing environmental conditions, the legacies of violence, and the limits of inherited Western social theory. Between Gaia and Ground also includes a glossary of the keywords and concepts that Povinelli has developed throughout her work.

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48

Attfield, Robin. Environmental Ethics: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198797166.001.0001.

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Environmental ethics studies the values and principles involved in combating environmental problems such as pollution, loss of species and habitats, and climate change. Environmental Ethics: A Very Short Introduction traces the discipline’s origins and considers how it defends the independent value of living creatures and the need to make decisions informed by the needs and interests of future generations. Exploring the diverse approaches to ethical decisions and judgements, it highlights the importance of making production and consumption sustainable, and of addressing human population levels, together with policies for preserving species, sub-species, and their habitats. It also discusses the different social and political movements involved and considers the environmental attitudes of the world’s religions.

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49

Taiz, Lincoln y Lee Taiz. Crop Domestication and Gender. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190490263.003.0003.

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“Crop Domestication and Gender” traces the rise of permanent settlements and incipient agriculture from the Pre-pottery Neolithic to the Pottery Neolithic in the Levant, together with the iconographic changes that show a shift from the predominance of zoomorphic forms to female forms concurrent with the increasing importance of agriculture. It discusses relevant geographic features, climactic periods and changes in temperature, rainfall and glaciation while exploring the important transitional cultures and the artifacts that reveal the progress of agricultural development and plant domestication. Domestication of the founder crops of the Fertile Crescent are described, together with markers in the archaeological record that distinguish wild plants from domesticated plants. The abundance of female figurines at the Neolithic village of Sha’ar Hagolan and the presence of cryptic agricultural symbols at Hacilar and Çatalhüyük, support a close association of women, cats, and agriculture, most famously exemplified by the so-called “grain bin goddess“ of Çatalhüyük.

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Pak, Chris. Terraforming. Liverpool University Press, 2016. http://dx.doi.org/10.5949/liverpool/9781781382844.001.0001.

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This book explores the emergence and development of terraforming in science fiction from H.G. Wells’s The War of the Worlds (1898) to James Cameron’s blockbuster Avatar (2009). Terraforming is the process of making other worlds habitable for human life. Its counterpart on Earth—geoengineering—has been positioned as a possible means of addressing the effects of climate change. This book asks how science fiction has imagined the ways we shape both our world and other planets and how stories of terraforming reflect on science, society and environmentalism. It traces the growth of the motif of terraforming in stories by such writers as H.G. Wells and Olaf Stapledon in the UK, American pulp science fiction by Ray Bradbury, Robert Heinlein and Arthur C. Clarke, the counter cultural novels of Frank Herbert, Ursula K. Le Guin and Ernest Callenbach, and Pamela Sargent’s Venus trilogy, Frederick Turner’s epic poem of terraforming, Genesis, and Kim Stanley Robinson’s acclaimed Mars trilogy. It explores terraforming as a nexus for environmental philosophy, the pastoral, ecology, the Gaia hypothesis, the politics of colonisation and habitation, tradition and memory. This book shows how contemporary environmental awareness and our understanding of climate change is influenced by science fiction, and how terraforming in particular has offered scientists, philosophers, and many other readers a motif to think in complex ways about the human impact on planetary environments. Amidst contemporary anxieties about climate change, terraforming offers an important vantage from which to consider the ways humankind shapes and is shaped by their world.

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