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1

Cecala, Andrew B. Pallet loading dust control system. Washington, DC: U.S. Bureau of Mines, 1988.

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2

Cecala, Andrew B. Pallet loading dust control system. [Washington, D.C.]: U.S. Dept. of the Interior, Bureau of Mines, 1988.

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3

Castiglioni, Carlo Andrea. Seismic Behavior of Steel Storage Pallet Racking Systems. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-28466-8.

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4

Laundrie, James F. Unitizing goods on pallets and slipsheets. Madison, WI: U.S. Dept. of Agriculture, Forest Service, Forest Products Laboratory, 1986.

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5

Wiseman, Regge N. Prehistory of the Berrendo River System in the southern plains of New Mexico. Santa Fe, NM: Museum of New Mexico, Office of Archaeological Studies, 2004.

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6

A, Lovis William, and Hambacher Michael J, eds. Modeling archaeolgical site burial in southern Michigan: A geoarchaeological synthesis. East Lansing: Michigan State University Press, 2005.

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7

United States. Bureau of Land Management. Palm Springs/South Coast Field Office. Draft supplemental EIS for the Palen Solar Electric Generating System (formerly Palen Solar Power Project): For the Palm Springs-South Coast Field Office. Palm Springs, Calif: U.S. Dept. of the Interior, Bureau of Land Management, Palm Springs-South Coast Field Office, 2011.

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8

Traduction, Collin Delavaud Henri, and Hennebault Carole Traduction, eds. Les grands bouleversements terrestres. Paris: Le jardin des livres, 2004.

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9

Sandler, Corey. Ultimate Sega Game Strategies, for the Master and Genesis Systems. New York, NY: Bantam Books, 1990.

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10

1963-, Ward Lesley A., ed. Harmonic analysis: From Fourier to wavelets. Providence, R.I: American Mathematical Society, 2012.

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11

Jefferson, Palmer A., and United States. Forest Service. Northeastern Research Station., eds. PCS: A Pallet Costing System for wood pallet manufacturers : version 1.0 for Windows. [Newtown Square, PA]: U.S. Dept. of Agriculture, Forest Service, Northeastern Research Station, 2002.

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12

Jefferson, Palmer A., and United States. Forest Service. Northeastern Research Station., eds. PCS: A Pallet Costing System for wood pallet manufacturers : version 1.0 for Windows. [Newtown Square, PA]: U.S. Dept. of Agriculture, Forest Service, Northeastern Research Station, 2002.

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13

Castiglioni, Carlo Andrea. Seismic Behavior of Steel Storage Pallet Racking Systems. Springer, 2016.

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14

Castiglioni, Carlo Andrea. Seismic Behavior of Steel Storage Pallet Racking Systems. Springer, 2018.

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15

A, Kernahan Desmond, and Rosenstein Sheldon W, eds. Cleft lip and palate: A system of management. Baltimore: Williams & Wilkins, 1990.

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16

Kernahan, Desmond A. Cleft Lip and Palate: A System of Management. Williams & Wilkins, 1990.

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17

Taylor, Tristan S. Legally Marginalised Groups—The Empire. Edited by Paul J. du Plessis, Clifford Ando, and Kaius Tuori. Oxford University Press, 2016. http://dx.doi.org/10.1093/oxfordhb/9780198728689.013.28.

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Until the mass citizenship grant of 212 CE, Roman law served Roman citizens almost exclusively. However, since the non-Romans’ legal systems generally sufficed, this marginalised status regarding Roman law was generally of little importance. Within the Roman citizen body, the Roman legal system marginalised many because of its expense and preferential treatment of the wealthy. In addition the culture, but not the legal system, through infamia marginalised some for what they did and the kind of person they were. While marginalised in modern eyes, Roman law treated women, freedmen, children and slaves as important participants in a wide range of societal functions, giving them specific abilities as well as disabilities. The most severe legal marginalisation occurred as the laws systematically and increasingly marginalised the humble citizens (humiliores) and evermore favoured the elite (honestiores). The system also treated outlaws, magicians, some cults and, later, Christians as outside the law’s Pale.
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18

Claussen, Martin, Anne Dallmeyer, and Jürgen Bader. Theory and Modeling of the African Humid Period and the Green Sahara. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.532.

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There is ample evidence from palaeobotanic and palaeoclimatic reconstructions that during early and mid-Holocene between some 11,700 years (in some regions, a few thousand years earlier) and some 4200 years ago, subtropical North Africa was much more humid and greener than today. This African Humid Period (AHP) was triggered by changes in the orbital forcing, with the climatic precession as the dominant pacemaker. Climate system modeling in the 1990s revealed that orbital forcing alone cannot explain the large changes in the North African summer monsoon and subsequent ecosystem changes in the Sahara. Feedbacks between atmosphere, land surface, and ocean were shown to strongly amplify monsoon and vegetation changes. Forcing and feedbacks have caused changes far larger in amplitude and extent than experienced today in the Sahara and Sahel. Most, if not all, climate system models, however, tend to underestimate the amplitude of past African monsoon changes and the extent of the land-surface changes in the Sahara. Hence, it seems plausible that some feedback processes are not properly described, or are even missing, in the climate system models.Perhaps even more challenging than explaining the existence of the AHP and the Green Sahara is the interpretation of data that reveal an abrupt termination of the last AHP. Based on climate system modeling and theoretical considerations in the late 1990s, it was proposed that the AHP could have ended, and the Sahara could have expanded, within just a few centuries—that is, much faster than orbital forcing. In 2000, paleo records of terrestrial dust deposition off Mauritania seemingly corroborated the prediction of an abrupt termination. However, with the uncovering of more paleo data, considerable controversy has arisen over the geological evidence of abrupt climate and ecosystem changes. Some records clearly show abrupt changes in some climate and terrestrial parameters, while others do not. Also, climate system modeling provides an ambiguous picture.The prediction of abrupt climate and ecosystem changes at the end of the AHP is hampered by limitations implicit in the climate system. Because of the ubiquitous climate variability, it is extremely unlikely that individual paleo records and model simulations completely match. They could do so in a statistical sense, that is, if the statistics of a large ensemble of paleo data and of model simulations converge. Likewise, the interpretation regarding the strength of terrestrial feedback from individual records is elusive. Plant diversity, rarely captured in climate system models, can obliterate any abrupt shift between green and desert state. Hence, the strength of climate—vegetation feedback is probably not a universal property of a certain region but depends on the vegetation composition, which can change with time. Because of spatial heterogeneity of the African landscape and the African monsoon circulation, abrupt changes can occur in several, but not all, regions at different times during the transition from the humid mid-Holocene climate to the present-day more arid climate. Abrupt changes in one region can be induced by abrupt changes in other regions, a process sometimes referred to as “induced tipping.” The African monsoon system seems to be prone to fast and potentially abrupt changes, which to understand and to predict remains one of the grand challenges in African climate science.
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19

Jacobsen, Dean, and Olivier Dangles. The high altitude environment. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0001.

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Chapter 1 gives a brief overview of the climatic and terrestrial environment in which high altitude waters are embedded. This context is necessary to understand the prevailing environmental conditions in the aquatic systems. The chapter begins by defining high altitude, alpine, and mountain, and provides an overview of the distribution of the world’s main high altitude regions. The overall picture of the climatic setting is drawn, from the inevitable consequences of high altitude (low temperature, low atmospheric pressure, and high solar radiation) to the highly region-specific patterns in precipitation and wind. The various ways that highland regions are formed, their temporal evolution, and climatic changes are treated in a section on the palaeo-environmental perspective. Finally, general patterns in high altitude (alpine) vegetation zones and treelines on different continents are synthesized, as well as major soil-forming processes in the catchments surrounding aquatic systems.
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20

Jacobsen, Dean, and Olivier Dangles. Organisms and diversity patterns at high altitudes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0004.

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Chapter 4 gives a group-by-group treatment from amphibians and fish to algae and microbes of what is known about altitudinal diversity patterns, dominant groups, and prominent species from high altitude waters around the world. This is accompanied by biogeographical considerations on dispersal, immigration, and local speciation processes. The general and well-known decrease in species richness with increasing altitude observed in the terrestrial environment is also the rule in aquatic systems. Yet, while some groups of organisms show very clear altitudinal patterns, others do not. Some groups even increase in richness towards high plateaus. Likewise, the proportion of endemics often increases with altitude. Patterns also vary globally and seem to depend on factors such as regional topography, catchment physiognomy, and palaeo-environmental and climatic history.
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21

Holm, Poul, Tim D. Smith, and David J. Starkey, eds. The Exploited Seas. Liverpool University Press, 2001. http://dx.doi.org/10.5949/liverpool/9780973007312.001.0001.

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The book combines the approaches of maritime history and ecological science to explore the evolution of life-forms and eco-systems in the ocean from a historical perspective, in order to establish and develop the sub-discipline of marine environmental history. Documentary records relating to the human activity, such as fishing, plus naturally occurring paleo-ecological data are analysed in order to determine the structure and function of exploited ecosystems. The book is divided into four chapter groups, the first concerned with Newfoundland and Grand Banks’ fisheries, the second with the potential of historical sources to provide a history of marine animal populations, the third explores the development of fisheries in the southern hemisphere during the twentieth century, and the final section explores the limitations of data and existing analysis of whale populations. The epilogue reiterates the suggestion that collaboration between historians and biologists is the key to furthering the sub-discipline.
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22

Pryor, Adam. Living with Tiny Aliens. Fordham University Press, 2020. http://dx.doi.org/10.5422/fordham/9780823288311.001.0001.

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Astrobiology forces us to realize how deeply tethered we are to this pale blue dot in the universe while also opening us to the exciting possibilities of existing in a fecund cosmos. Addressing both of these issues, this work offers a model for doing public theology attuned to astrobioloical humanities. It taps into theology’s capacity to develop societal goods by interpreting religious symbols as expressions of ultimacy that foster powerful moods for meaningfully ordering our ways of being-in and belonging-to the cosmos. Providing a series of specific examples drawn from astrobiology, doctrinal reflection on the imago Dei, and reflections on the Anthropocene, this book claims the Earth is not only a living planet but an artful one. Consequently, it suggests that the imago Dei be reframed in terms of planetarity: to be the imago Dei is to be a planetary system that opens up new possibilities for the flourishing of all creation by fostering technobiogeochemical cycles not subject to runaway, positive feedback. The imago Dei, then, is not something any one of us possesses; it is a symbol for what we live-into together as a species in intra-action with the wider habitable environment. Attentive to how this outlook can be fostered, the conclusion advocates for the development of presence, wonder, and play in the lives of individuals who seek to live as part of an artful planet.
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23

Inayatullah, Naeem, and David L. Blaney. Units, Markets, Relations, and Flow: Beyond Interacting Parts to Unfolding Wholes. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228637.013.272.

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Heterodox work in Global Political Economy (GPE) finds its motive force in challenging the ontological atomism of International Political Economy (IPE) orthodoxy. Various strains of heterodoxy that have grown out of dependency theory and World-Systems Theory (WST), for example, emphasize the social whole: Individual parts are given form and meaning within social relations of domination produced by a history of violence and colonial conquest. An atomistic approach, they stress, seems designed to ignore this history of violence and relations of domination by making bargaining among independent units the key to explaining the current state of international institutions. For IPE, it is precisely this atomistic approach, largely inspired by the ostensible success of neoclassical economics, which justifies its claims to scientific rigor. International relations can be modeled as a market-like space, in which individual actors, with given preferences and endowments, bargain over the character of international institutional arrangements. Heterodox scholars’ treatment of social processes as indivisible wholes places them beyond the pale of acceptable scientific practice. Heterodoxy appears, then, as the constitutive outside of IPE orthodoxy.Heterodox GPE perhaps reached its zenith in the 1980s. Just as heterodox work was being cast out from the temple of International Relations (IR), heterodox scholars, building on earlier work, produced magisterial studies that continue to merit our attention. We focus on three texts: K. N. Chaudhuri’s Asia Before Europe (1990), Eric Wolf’s Europe and the People Without History (1982), and L. S. Stavrianos’s Global Rift (1981). We select these texts for their temporal and geographical sweep and their intellectual acuity. While Chaudhuri limits his scope to the Indian Ocean over a millennium, Wolf and Stavrianos attempt an anthropology and a history, respectively, of European expansion, colonialism, and the rise of capitalism in the modern era. Though the authors combine different elements of material, political, and social life, all three illustrate the power of seeing the “social process” as an “indivisible whole,” as Schumpeter discusses in the epigram below. “Economic facts,” the region, or time period they extract for detailed scrutiny are never disconnected from the “great stream” or process of social relations. More specifically, Chaudhuri’s work shows notably that we cannot take for granted the distinct units that comprise a social whole, as does the IPE orthodoxy. Rather, such units must be carefully assembled by the scholar from historical evidence, just as the institutions, practices, and material infrastructure that comprise the unit were and are constructed by people over the longue durée. Wolf starts with a world of interaction, but shows that European expansion and the rise and spread of capitalism intensified cultural encounters, encompassing them all within a global division of labor that conditioned the developmental prospects of each in relation to the others. Stavrianos carries out a systematic and relational history of the First and Third Worlds, in which both appear as structural positions conditioned by a capitalist political economy. By way of conclusion, we suggest that these three works collectively inspire an effort to overcome the reification and dualism of agents and structures that inform IR theory and arrive instead at “flow.”
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