Discovering the birds of Europe, I

Author(s):  
Henry A. McGhie

This chapter introduces the ‘History of the Birds of Europe’, a great book project initiated by Richard Bowdler Sharpe, in partnership with Dresser. The chapter discusses scientific travellers and fieldwork, and the growth of formal and informal scientific travel through the nineteenth century. It describes the collecting manuals and instructions for collectors that were issued to encourage collectors to produce good-quality specimens that could enter into exchanging networks and museum collections. The chapter explores Dresser’s collecting network by discussing the activities of those who provided him with specimens from Europe, Northern Asia, North America and the Arctic. It emphasises and explores his personal relationships with field collectors.

Author(s):  
Michael D. Gordin

Dmitrii Mendeleev (1834–1907) is a name we recognize, but perhaps only as the creator of the periodic table of elements. Generally, little else has been known about him. This book is an authoritative biography of Mendeleev that draws a multifaceted portrait of his life for the first time. As the book reveals, Mendeleev was not only a luminary in the history of science, he was also an astonishingly wide-ranging political and cultural figure. From his attack on Spiritualism to his failed voyage to the Arctic and his near-mythical hot-air balloon trip, this is the story of an extraordinary maverick. The ideals that shaped his work outside science also led Mendeleev to order the elements and, eventually, to engineer one of the most fascinating scientific developments of the nineteenth century. This book is a classic work that tells the story of one of the world's most important minds.


Author(s):  
John J. W. Rogers ◽  
M. Santosh

Pangea, the most recent supercontinent, attained its condition of maximum packing at ~250 Ma. At this time, it consisted of a northern part, Laurasia, and a southern part, Gondwana. Gondwana contained the southern continents—South America, Africa, India, Madagascar, Australia, and Antarctica. It had become a coherent supercontinent at ~500 Ma and accreted to Pangea largely as a single block. Laurasia consisted of the northern continents—North America, Greenland, Europe, and northern Asia. It accreted during the Late Paleozoic and became a supercontinent when fusion of these continental blocks with Gondwana occurred near the end of the Paleozoic. The configuration of Pangea, including Gondwana, can be determined accurately by tracing the patterns of magnetic stripes in the oceans that opened within it (chapters 1 and 9). The history of accretion of Laurasia is also well known, but the development of Gondwana is highly controversial. Gondwana was clearly a single supercontinent by ~500 Ma, but whether it formed by fusion of a few large blocks or the assembly of numerous small blocks is uncertain. Figure 8.1 shows Gondwana divided into East and West parts, but the boundary between them is highly controversial (see below). We start this chapter by investigating the history of Gondwana, using appendix SI to describe detailed histories of orogenic belts of Pan-African age (600–500-Ma). Then we continue with the development of Pangea, including the Paleozoic orogenic belts that led to its development. The next section summarizes the paleomagnetically determined movement of blocks from the accretion of Gondwana until the assembly of Pangea, and the last section discusses the differences between Gondwana and Laurasia in Pangea. The patterns of dispersal and development of modern oceans are left to chapter 9, and the histories of continents following dispersal to chapter 10. By the later part of the 1800s, geologists working in the southern hemisphere realized that the Paleozoic fossils that occurred there were very different from those in the northern hemisphere. They found similar fossils in South America, Africa, Madagascar, India, and Australia, and in 1913 they added Antarctica when identical specimens were found by the Scott expedition.


2017 ◽  
Vol 17 (19) ◽  
pp. 11971-11989 ◽  
Author(s):  
Jun-Wei Xu ◽  
Randall V. Martin ◽  
Andrew Morrow ◽  
Sangeeta Sharma ◽  
Lin Huang ◽  
...  

Abstract. Black carbon (BC) contributes to Arctic warming, yet sources of Arctic BC and their geographic contributions remain uncertain. We interpret a series of recent airborne (NETCARE 2015; PAMARCMiP 2009 and 2011 campaigns) and ground-based measurements (at Alert, Barrow and Ny-Ålesund) from multiple methods (thermal, laser incandescence and light absorption) with the GEOS-Chem global chemical transport model and its adjoint to attribute the sources of Arctic BC. This is the first comparison with a chemical transport model of refractory BC (rBC) measurements at Alert. The springtime airborne measurements performed by the NETCARE campaign in 2015 and the PAMARCMiP campaigns in 2009 and 2011 offer BC vertical profiles extending to above 6 km across the Arctic and include profiles above Arctic ground monitoring stations. Our simulations with the addition of seasonally varying domestic heating and of gas flaring emissions are consistent with ground-based measurements of BC concentrations at Alert and Barrow in winter and spring (rRMSE  < 13 %) and with airborne measurements of the BC vertical profile across the Arctic (rRMSE  = 17 %) except for an underestimation in the middle troposphere (500–700 hPa).Sensitivity simulations suggest that anthropogenic emissions in eastern and southern Asia have the largest effect on the Arctic BC column burden both in spring (56 %) and annually (37 %), with the largest contribution in the middle troposphere (400–700 hPa). Anthropogenic emissions from northern Asia contribute considerable BC (27 % in spring and 43 % annually) to the lower troposphere (below 900 hPa). Biomass burning contributes 20 % to the Arctic BC column annually.At the Arctic surface, anthropogenic emissions from northern Asia (40–45 %) and eastern and southern Asia (20–40 %) are the largest BC contributors in winter and spring, followed by Europe (16–36 %). Biomass burning from North America is the most important contributor to all stations in summer, especially at Barrow.Our adjoint simulations indicate pronounced spatial heterogeneity in the contribution of emissions to the Arctic BC column concentrations, with noteworthy contributions from emissions in eastern China (15 %) and western Siberia (6.5 %). Although uncertain, gas flaring emissions from oilfields in western Siberia could have a striking impact (13 %) on Arctic BC loadings in January, comparable to the total influence of continental Europe and North America (6.5 % each in January). Emissions from as far as the Indo-Gangetic Plain could have a substantial influence (6.3 % annually) on Arctic BC as well.


1991 ◽  
Vol 47 (03) ◽  
pp. 337-348
Author(s):  
Michael P. Costeloe

In 1843, two friends, one Scottish and one American, published books about Mexico which were to become essential reading for students of Mexican history. Much the better known of the two is William Hickling Prescott whose History of the Conquest of Mexico became an instant best-seller and remains to this day one of the classics of Mexican historiography. Less well-known but equally valuable to historians of nineteenth-century Mexico is Frances Calderón de la Barca's vivid account of Life in Mexico based on her experiences during the two years from 1840-1841 when she lived in the country as the wife of the first Spanish ambassador. By coincidence, Prescott and Sra. Calderón were close personal friends and regular correspondents and they gave each other much assistance in preparing their respective books for publication. Both their works were greeted with critical and public acclaim in the English-speaking world of Europe and North America but reactions in Mexico were markedly different. While Prescott's book was received with qualified enthusiasm, Life in Mexico was the subject of hostile reviews and its author much vitriolic, personal abuse.


Author(s):  
María del Pilar Blanco ◽  
Joanna Page

The transnational transfers of ideas, technologies, materials, and people that have shaped the history of science in Latin America are marked, as in any region, by asymmetries of power. These are often replicated or even magnified in the narratives we have forged about that history. The journeys to Latin America of some of Europe’s most famous naturalists (Humboldt and Darwin, for example) are often depicted as the heroic overcoming by European science of savage local terrains and ways of life. Those epic explorers are recast, in other narratives, as the forerunners of (neo)colonial exploitation in the history of the ransacking of Latin America’s mineral riches to pay for European imperial ventures, repeated in the often-illegal plundering of the region’s dinosaur fossils to swell museum collections in Europe and North America. In such accounts, Latin America becomes the arena for European adventures, the testing ground for new scientific theories, or the passive victim of colonial profiteering, but rarely a place of innovation. It is certainly the case that over the centuries the flow of natural resources, data, and expertise from Latin America to more developed regions has generally been to the benefit of those regions and has not reduced an imbalance of power that dates back to the colonial period.


Author(s):  
Frank Towers

Today’s political map of North America took its basic shape in a continental crisis in the 1860s, marked by Canadian Confederation (1867), the end of the U.S. Civil War (1865), the restoration of the Mexican Republic (1867), and numerous wars and treaty regimes conducted between these states and indigenous peoples through the 1870s. This volume explores the tumultuous history of North American state-making in the mid-nineteenth century from a continental perspective that seeks to look across and beyond the traditional nation-centered approach. This introduction orients readers by first exploring the meaning of key terms—in particular sovereignty and its historical attachment to the concept of the nation state—and then previewing how contributors interrogate different themes of the mid-century struggles that remade the continent’s political order. Those themes fall into three main categories: the character of the states made and remade in the mid-1800s; the question of sovereignty for indigenous polities that confronted the European-settler descended governments of Canada, Mexico, and the United States; and the interaction between capitalist expansion and North American politics, and the concomitant implications of state making for sovereignty’s more diffuse meaning at the level of individual and group autonomy.


2021 ◽  
pp. 1-46
Author(s):  
Lieselotte Anderwald

This article challenges the accepted opinion that the American English perfect form HAVE gotten is a straightforward historical retention of an earlier British English form. Although HAVE gotten was presumably part of the settler input in North America, it (almost) died out in American English as well, but was then revived in the nineteenth century, as historical corpus data show. Contrary to expectations, this revival was not an innovation from below. Instead, the rise of HAVE gotten was promoted by careful writers who deliberately avoided the highly stigmatized stative HAVE got. This explains why perfect HAVE gotten appears in more formal text types first, and how it became specialized to dynamic contexts only. The morphological Americanism HAVE gotten is thus a curious case of an (unintended) side-effect of marginally successful prescriptivism.1


1988 ◽  
Vol 120 (S144) ◽  
pp. 93-107 ◽  
Author(s):  
Donald P. Schwert ◽  
Allan C. Ashworth

AbstractFossils from sites of Late Quaternary age in North America provide tangible evidence of temporal changes in the character of the northern beetle fauna. Based on a synthesis of the fossil data with analyses of the present distributions for northern species, a rudimentary model is proposed to explain the recent history of the fauna of the arctic and the boreal forest.An open-ground beetle fauna of arctic–subarctic affinities had become established along the southern margin of the Laurentide ice sheet in the midcontinent by 20 500 years before present (yr B.P.). Climatic warming decimated this fauna throughout lowland areas at some time between 16 700 and 15 300 yr B.P.; small populations of some arctic–subarctic species, however, survived within either alpine habitats of the Cordillera and Appalachians or specialized environments associated with stagnant ice.Populations of the same arctic–subarctic beetle species existed within the ice-free Alaska–Yukon refugium throughout the late Wisconsinan. During the Holocene, this region served as the principal centre-of-origin for the dispersal of the arctic–subarctic beetle fauna.The beetle fauna of the boreal forest was also displaced southward by Late Wisconsinan glaciation. By 15 300 yr B.P., however, this fauna had largely replaced the arctic–subarctic beetle fauna along the ice margin of the midcontinent. Evidence provided by fossils from a series of sites demonstrates that beetle species of the boreal forest dispersed northward into Canada as the ice front receded.


2019 ◽  
Vol 19 (4) ◽  
pp. 28-41
Author(s):  
Laurie K. Bertram

This article explores the history of vínarterta, a striped fruit torte imported by Icelandic immigrants to North America in the late nineteenth century and obsessively preserved by their descendants today. When roughly 20–25 percent of the population of Iceland relocated to North America between 1870 and 1914, they brought with them a host of culinary traditions, the most popular and enduring of which is this labor-intensive, spiced, layered dessert. Considered an essential fixture at any important gathering, including weddings, holidays, and funerals, vínarterta looms large in Icelandic–North American popular culture. Family recipes are often closely guarded, and any alterations to the “correct recipe,” including number of layers, inclusion or exclusion of cardamom or frosting, and the use of almond extract, are still hotly debated by community members who see changes to “original” recipes as a controversial, even offensive sign of cultural degeneration. In spite of this dedication to authenticity, this torte is an unusual ethnic symbol with a complex past. The first recipes for “Vienna torte” were Danish imports via Austria, originally popular with the Icelandic immigrant generation in the late nineteenth century because of their glamorous connections to continental Europe. Moreover, the dessert fell out of fashion in Iceland roughly at the same time as it ascended as an ethnic symbol in wartime and postwar North American heritage spectacles. Proceeding from recipe books, oral history interviews, memoirs, and Icelandic and English language newspapers, this article examines the complex history of this particular dessert.


Polar Record ◽  
1999 ◽  
Vol 35 (194) ◽  
pp. 193-206 ◽  
Author(s):  
Russell A. Potter ◽  
Douglas W. Wamsley

AbstractIn mid-nineteenth century America, the Arctic adventures of Elisha Kent Kane were a common and central subject for the emerging mass media. Kane's exploits were retold through illustrated newspapers, magazines, and books, but his narratives found one of their widest audiences through the medium of the ‘panorama.’ Initially presented in fixed locations, these panoramas later traveled across the country, combining large moving canvasses with a variety of visual and theatrical effects. Kane's two Arctic expeditions were among the most popular subjects represented by panoramas in the period before the American Civil War. This article examines the history of the panorama as it reflected and shaped public interest in the Arctic regions, including earlier polar expeditions, and gives a detailed account of the Kane panoramas. Other optical media that represented Kane's exploits are also considered. Because of its broad audience and widespread appeal, the panorama, along with other emergent visual technologies, played a vital yet overlooked part, both in disseminating Kane's accomplishments and in elevating Kane to prominence and fame in the mid-nineteenth century.


Sign in / Sign up

Export Citation Format

Share Document