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Books on the topic 'Speleothems'

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1

Perkins, Andrew Mark. Magnetic studies of speleothems. Norwich: University of East Anglia, 1993.

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2

Kempe, Stephan. Die Baumannshöhle im Harz, ihre Bedeutung für die frühe Wissenschaftsgeschichte, ihre Darstellung durch Johann Friedrich Zückert, der Arzneygelahrtheit Doctor, 1763, und was heute noch davon zu sehen ist. München: Verband der Deutchen Höhlen- und Karstforscher, 1999.

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3

Symposium, Climate Change: the Karst Record (4th 2006 Băile Herculane, Romania). Archives of climate and environmental change in karst. Edited by Onac Bogdan P and Constantin Silviu. Amsterdam: Elsevier, 2008.

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4

Sattmann, Helmut, and Robert Seemann. Kahf al-Hūtah: Taḥta al-arḍ saqf min al-jannah bi-minṭaqat Jabal Shams. Edited by Oman Wizārat al-Siyāḥah. Salṭanat ʻUmān: Wizārat al-Siyāḥah, 2009.

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5

Singh, Anoop Kumar. High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73597-9.

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6

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

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7

Fairchild, Ian J., and Andy Baker. Speleothem Science. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781444361094.

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8

Fairchild, Ian J., and Andy Baker. Speleothem Science: From Process to Past Environments. Wiley & Sons, Limited, John, 2012.

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9

Fairchild, Ian J., and Andy Baker. Speleothem Science: From Process to Past Environments. Wiley & Sons, Incorporated, John, 2012.

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10

Fairchild, Ian J., and Andy Baker. Speleothem Science: From Process to Past Environments. Wiley & Sons, Incorporated, John, 2012.

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11

Fairchild, Ian J., and Andy Baker. Speleothem Science: From Process to Past Environments. Wiley & Sons, Incorporated, John, 2012.

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12

Tufas and speleothems: Unravelling the microbial and physical controls. London, UK: Geological Society of London, 2010.

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13

Sasowsky, Ira D., and John Mylroie. Studies of Cave Sediments: Physical and Chemical Records of Paleoclimate. Springer London, Limited, 2012.

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14

Singh, Anoop Kumar. High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems: Past Climatic Changes Using Cave Structures. Springer, 2018.

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15

Singh, Anoop Kumar. High Resolution Palaeoclimatic Changes in Selected Sectors of the Indian Himalaya by Using Speleothems: Past Climatic Changes Using Cave Structures. Springer, 2019.

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16

Bar-Yosef, Ofer, Miryam Bar-Matthews, and Avner Ayalon. 12,000–11,700 cal BP. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0002.

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We take up the question of “why” cultivation was adopted by the end of the Younger Dryas by reviewing evidence in the Levant, a sub-region of southwestern Asia, from the Late Glacial Maximum through the first millennium of the Holocene. Based on the evidence, we argue that the demographic increase of foraging societies in the Levant at the Terminal Pleistocene formed the backdrop for the collapse of foraging adaptations, compelling several groups within a particular “core area” of the Fertile Crescent to become fully sedentary and introduce cultivation alongside intensified gathering in the Late Glacial Maximum, ca. 12,000–11,700 cal BP. In addition to traditional hunting and gathering, the adoption of stable food sources became the norm. The systematic cultivation of wild cereals begun in the northern Levant resulted in the emergence of complex societies across the entire Fertile Crescent within several millennia. Results of archaeobotanical and archaeozoological investigations provide a basis for reconstructing economic strategies, spatial organization of sites, labor division, and demographic shifts over the first millennium of the Holocene. We draw our conclusion from two kinds of data from the Levant, a sub-region of southwestern Asia, during the Terminal Pleistocene and early Holocene: climatic fluctuations and the variable human reactions to natural and social calamities. The evidence in the Levant for the Younger Dryas, a widely recognized cold period across the northern hemisphere, is recorded in speleothems and other climatic proxies, such as Dead Sea levels and marine pollen records.
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17

Weiss, Harvey, ed. Megadrought and Collapse. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.001.0001.

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This is the first book to treat the major examples of megadrought and societal collapse, from the late Pleistocene end of hunter–gatherer culture and origins of cultivation to the 15th century AD fall of the Khmer Empire capital at Angkor, and ranging from the Near East to South America. Previous enquiries have stressed the possible multiple and internal causes of collapse, such overpopulation, overexploitation of resources, warfare, and poor leadership and decision-making. In contrast, Megadrought and Collapse presents case studies of nine major episodes of societal collapse in which megadrought was the major and independent cause of societal collapse. In each case the most recent paleoclimatic evidence for megadroughts, multiple decades to multiple centuries in duration, is presented alongside the archaeological records for synchronous societal collapse. The megadrought data are derived from paleoclimate proxy sources (lake, marine, and glacial cores; speleothems, or cave stalagmites; and tree-rings) and are explained by researchers directly engaged in their analysis. Researchers directly responsible for them discuss the relevant current archaeological records. Two arguments are developed through these case studies. The first is that societal collapse in different time periods and regions and at levels of social complexity ranging from simple foragers to complex empires would not have occurred without megadrought. The second is that similar responses to megadrought extend across these historical episodes: societal collapse in the face of insurmountable climate change, abandonment of settlements and regions, and habitat tracking to sustainable agricultural landscapes. As we confront megadrought today, and in the likely future, Megadrought and Collapse brings together the latest contributions to our understanding of past societal responses to the crisis on an equally global and diverse scale.
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18

Weiss, Harvey. Megadrought, Collapse, and Causality. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0001.

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Recent discoveries of megadroughts, severe periods of drought lasting decades or centuries, during the course of the Holocene have revolutionized our understanding of modern climate history. Through advances in paleoclimatology, researchers have identified these periods of climate change by analyzing high-resolution proxy data derived from lake sediment cores, marine cores, glacial cores, speleothem cores, and tree rings. Evidence that megadroughts occurred with frequency and abruptly over the last 12,000 years, a timespan long assumed to be stable compared to earlier glacial periods, has also altered our understanding of societies’ trajectories. The fact that severe, multi-decadal or century-scale droughts coincided with societal collapses well known to archaeologists has challenged established multi-causal analyses of these events. Megadroughts, impossible to predict and impossible to withstand, may have caused political collapse, regional abandonment, and habitat tracking to still-productive regions. The nine megadrought and societal collapse events presented in this volume extend from the foraging-to-agriculture transition at the dawn of the Holocene in West Asia to the fifteenth-century AD collapse of the Khmer Empire in Angkor (Cambodia). Inevitably, this collection of essays also raises challenges to causal analyses of societal collapse and for future paleoclimatic and archaeological research.
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