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2021 ◽  
pp. 39-63
Author(s):  
Eli Lederhendler

The experiences of children during the process of migration are explored with reference to the Great Atlantic Migration, specifically the Jewish immigration from Eastern Europe around the turn of the 20th century. These experiences, as recorded by them later in their lives, are also represented in literary works penned by immigrant and second-generation authors. The subjective and representational aspects of child-immigrant lives add substance and perspective to an array of social data available about that era, including the proportion of children and youth in the migration stream, the effect of mass immigration on social services (including public education), employment of children and youth in industry, and welfare and institutional care. The article asserts that child-immigrants can be studied not only from the perspective of achievement outcomes in American society, as is currently common in the literature, but also in terms of assigning child-immigrants a separate voice in the historiography of U.S. migration.


2021 ◽  
pp. 002190962110084
Author(s):  
AKM Ahsan Ullah ◽  
Mallik Akram Hossain ◽  
Ahmed Shafiqul Huque

The circumstances prevailing in South Asia (SA) have led to a plateauing migration stream that has resulted in several categories of migrants. The underlying factors driving migration have been identical in all the countries of SA. In recent years, however, poverty, conflicts, political and religious persecution, natural disasters and climate change have emerged as the most prominent drivers. External migration flow from SA has more than doubled between 2000 and 2015. This is a dynamic region, with millions (over 38m in 2017) of people crossing borders, both intra-regionally and extra-regionally. In recent years, wealthy citizens from SA have begun to move out of their countries with the intention of settling down elsewhere. This tendency has raised concerns among the policy makers because they create the grounds for reverse remittance flows. This research is meant to identify and contribute to the discourse of a new category of migrants (non-conventional migration) who are different from those in the conventional migration stream that included economic and forced migration. This research has crucial policy implications for both origin and destination countries.


2021 ◽  
Vol 226 (2) ◽  
pp. 519-562 ◽  
Author(s):  
Elena Garcia-Calero ◽  
Lara López-González ◽  
Margaret Martínez-de-la-Torre ◽  
Chen-Ming Fan ◽  
Luis Puelles

AbstractWe focus this report on the nucleus of the lateral olfactory tract (NLOT), a superficial amygdalar nucleus receiving olfactory input. Mixed with its Tbr1-expressing layer 2 pyramidal cell population (NLOT2), there are Sim1-expressing cells whose embryonic origin and mode of arrival remain unclear. We examined this population with Sim1-ISH and a Sim1-tauLacZ mouse line. An alar hypothalamic origin is apparent at the paraventricular area, which expresses Sim1 precociously. This progenitor area shows at E10.5 a Sim1-expressing dorsal prolongation that crosses the telencephalic stalk and follows the terminal sulcus, reaching the caudomedial end of the pallial amygdala. We conceive this Sim1-expressing hypothalamo-amygdalar corridor (HyA) as an evaginated part of the hypothalamic paraventricular area, which participates in the production of Sim1-expressing cells. From E13.5 onwards, Sim1-expressing cells migrated via the HyA penetrate the posterior pallial amygdalar radial unit and associate therein to the incipient Tbr1-expressing migration stream which swings medially past the amygdalar anterior basolateral nucleus (E15.5), crosses the pallio-subpallial boundary (E16.5), and forms the NLOT2 within the anterior amygdala by E17.5. We conclude that the Tbr1-expressing NLOT2 cells arise strictly within the posterior pallial amygdalar unit, involving a variety of required gene functions we discuss. Our results are consistent with the experimental data on NLOT2 origin reported by Remedios et al. (Nat Neurosci 10:1141–1150, 2007), but we disagree on their implication in this process of the dorsal pallium, observed to be distant from the amygdala.


2020 ◽  
Vol 8 (4) ◽  
pp. 893-912
Author(s):  
Nathan J. Lyons ◽  
Pedro Val ◽  
James S. Albert ◽  
Jane K. Willenbring ◽  
Nicole M. Gasparini

Abstract. Drainages reorganise in landscapes under diverse conditions and process dynamics that impact biotic distributions and evolution. We first investigated the relative control that Earth surface process parameters have on divide migration and stream capture in scenarios of base-level fall and heterogeneous uplift. A model built with the Landlab toolkit was run 51 200 times in sensitivity analyses that used globally observed values. Large-scale drainage reorganisation occurred only in the model runs within a limited combination of parameters and conditions. Uplift rate, rock erodibility, and the magnitude of perturbation (base-level fall or fault displacement) had the greatest influence on drainage reorganisation. The relative magnitudes of perturbation and topographic relief limited landscape susceptibility to reorganisation. Stream captures occurred more often when the channel head distance to divide was low. Stream topology set by initial conditions strongly affected capture occurrence when the imposed uplift was spatially heterogeneous. We also integrated simulations of geomorphic and biologic processes to investigate relationships among topographic relief, drainage reorganisation, and riverine species diversification in the two scenarios described above. We used a new Landlab component called SpeciesEvolver that models species at landscape scale following macroevolutionary process rules. More frequent stream capture and less frequent stream network disappearance due to divide migration increased speciation and decreased extinction, respectively, especially in the heterogeneous uplift scenario in which final species diversity was often greater than the base-level fall scenario. Under both scenarios, the landscape conditions that led to drainage reorganisation also controlled diversification. Across the model trials, the climatic or tectonic perturbation was more likely in low-relief landscapes to drive more extensive drainage reorganisation that in turn increased the diversity of riverine species lineages, especially for the species that evolved more rapidly. This model result supports recent research on natural systems that implicates drainage reorganisation as a mechanism of riverine species diversification in lowland basins. Future research applications of SpeciesEvolver software can incorporate complex climatic and tectonic forcings as they relate to macroevolution and surface processes, as well as region- and taxon-specific organisms based in rivers and those on continents at large.


Author(s):  
Uzma Quraishi

In the early years of the Cold War, the United States mounted expansive public diplomacy programs in the Global South, including initiatives with the recently partitioned states of India and Pakistan. U.S. operations in these two countries became the second- and fourth-largest in the world, creating migration links that resulted in the emergence of American universities, such as the University of Houston, as immigration hubs for the highly selective, student-led South Asian migration stream starting in the 1950s. By the late twentieth century, Houston’s South Asian community had become one of the most prosperous in the metropolitan area and one of the largest in the country. Mining archives and using new oral histories, Uzma Quraishi traces this pioneering community from its midcentury roots to the early twenty-first century, arguing that South Asian immigrants appealed to class conformity and endorsed the model minority myth to navigate the complexities of a shifting Sunbelt South. By examining Indian and Pakistani immigration to a major city transitioning out of Jim Crow, Quraishi reframes our understanding of twentieth-century migration, the changing character of the South, and the tangled politics of race, class, and ethnicity in the United States


2020 ◽  
Vol 15 (4) ◽  
pp. 88-109

The paper deals with the analysis of Ukrainian migration into Russia, which has been remaining an important factor in Russia’s development during the post- Soviet period. Attraction of migrants with cultural characteristics similar to the native population makes it possible to simultaneously pursue two targets: promoting economic growth and preserving the nation’s cultural identity. Migrants from Ukraine are currently the only substantial source of potential migration into Russia that does not provoke a negative attitude among the Russian people. The paper provides an analysis of the main geographical directions of Ukrainian migration into Russia during the past eight years. These directions have proved to be resilient in spite of substantial changes of the socioeconomic conditions in both countries. It is shown that the “Ukrainian stream” demonstrates features common to international migration in other countries, at the same time having certain specifics, e.g. leaning toward big cities of the Russian South-West. The authors examine the distribution of migrants among the federal districts of Russia as well as among administrative centers and rural areas of receiving regions. The Ukrainian migration stream is considered to be the object of competition between Russian and Polish economic centers of gravity. In order for Russia to win in such a competition, the authors propose not to set an unrealistic goal of attracting Ukrainian migrants to the sparsely populated regions of Russia (e.g. the Far East), but rather to promote migration into regions which have already demonstrated their attractiveness for them, namely Belgorod, Voronezh and Krasnodar. In stimulating migration into these regions particular emphasis is to be made on the attraction of the Ukrainian youth, especially students. For that purpose, special programs targeting Ukrainian students should be elaborated at the universities of the Russian South-West.


2019 ◽  
Vol 13 (25) ◽  
pp. 36-53
Author(s):  
Víctor M. García-Guerrero ◽  
Claudia Masferrer ◽  
Silvia E. Giorguli-Saucedo

We analyze migration and demographic changes among the six countries of North America (NA) and the Northern Triangle of Central America (NTCA, i.e. Guatemala, Honduras and El Salvador). Together, they comprise a long-standing South-North migration stream, with the United States (US) and Canada being the main destinations for Mexico and the NTCA. Studies that analyze the demographic effects of international migration in origin and destination countries have been limited. In order to fill this gap and explain the implications of recent changes in migration trends and demographic dynamics of the six countries, we study the interrelationship between future changes in the age structure associated with different migration scenarios. We use data from the United Nations World Population Prospects 2017 to compare the main demographic indexes and age structure indicators under two prospective scenarios: with and without migration. Current and projected population dynamics suggest convergence in fertility below replacement levels, higher life expectancy, and an overall aging process in the NA-NTCA region. Future migration may slow down the aging process in Canada and the US, have a small effect in Mexico, and speed it up in El Salvador. Taking both the size of the populations and the decrease in young age groups for the main sending countries we have studied, it is unlikely that international migration to the US from Mexico and the NTCA will reach the historic peak observed during the first decade of the 21st century.


2019 ◽  
Author(s):  
Nathan J. Lyons ◽  
Pedro Val ◽  
James S. Albert ◽  
Jane K. Willenbring ◽  
Nicole M. Gasparini

Abstract. Drainages reorganise in landscapes under diverse conditions and process dynamics. We investigated the relative control that Earth surface process parameters have on divide migration and stream capture in scenarios of base level fall and heterogeneous uplift. A model built with the Landlab toolkit was run 51,200 times in a sensitivity analysis that used globally observed values. Large-scale drainage reorganisation occurred only in the model runs within a limited combination of parameters and conditions. Uplift rate, rock erodibility, and the magnitude of perturbation (base level fall or fault displacement) had the greatest influence on drainage reorganisation. The relative magnitudes of perturbation and topographic relief limited landscape susceptibility to reorganisation. Stream captures occurred more often when the channel head distance to divide was low. Stream topology set by initial conditions strongly affected capture occurrence when the imposed uplift was spatially heterogeneous. We also modelled riverine species lineages as they developed in response to the single topographic perturbation. We used a new Landlab component called SpeciesEvolver that models species lineages at landscape scale. Simulated species populated to the modelled landscape were tracked and evolved using macroevolutionary process rules. More frequent stream capture and less frequent stream network disappearance due to divide migration increased speciation and decreased extinction, respectively, in the heterogeneous uplift scenario where final species diversity was often greater than the base level fall scenario. Under both scenarios, the landscape conditions that led to drainage reorganisation following a single perturbation also controlled diversification, especially for the species that evolved more rapidly in some model trials. These results illustrate the utility of SpeciesEvolver to explore how life evolves alongside landscapes. Future research applications of SpeciesEvolver can incorporate more complex climatic and tectonic forcings as they relate to macroevolution and surface processes, as well as region- and taxon-specific organisms based in rivers as well as those on continents at large.


2019 ◽  
Vol 85 (1) ◽  
pp. 152-170 ◽  
Author(s):  
James L. Moore ◽  
Eric Blinman ◽  
M. Steven Shackley

Arakawa and colleagues (2011) use temporal changes in obsidian source patterns to link the late thirteenth-century abandonment of the Mesa Verde region to Ortman's (2010, 2012) model of Tewa migration to the northern Rio Grande. They employ Anthony's (1990) concept of reverse migration, inferring that an increase in Mesa Verde–region obsidian from a specific Jemez Mountain source reflects the scouting of an eventual migration path. Weaknesses of this inference are that only obsidian data from the Mesa Verde region were used in its development and that the model does not consider the complexities of previously documented patterns of settlement and stone raw material use in the northern Rio Grande. By examining source data from parts of northwestern and north-central New Mexico, we find that the patterning seen in the Mesa Verde obsidian data is widespread both geographically and temporally. The patterns are more indicative of a change in acquisition within a down-the-line exchange system than a reverse migration stream. Population trends on the southern Pajarito Plateau, the probable source of the acquisition change, suggest ancestral Keres rather than Tewa involvement in thirteenth-century obsidian distribution.


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