scholarly journals Phoretic mite associates of millipedes (Diplopoda, Julidae) in the northern Atlantic region (North America, Europe)

2012 ◽  
Vol 7 ◽  
pp. 69-91 ◽  
Author(s):  
Monica Farfan ◽  
Hans Klompen
1964 ◽  
Vol 44 (1) ◽  
pp. 34-37 ◽  
Author(s):  
K. K. Langmaid

Very little is found in the literature on the occurrence of earthworms in virgin podzols. The occurrence of earthworms in such soils, the rapidity of their invasion, and their effect on the soil profile is reported. The occurrence of L. festivus is recorded apparently for the first time in North America and D. octahedra for the first time in the Atlantic region of Canada.


2002 ◽  
Vol 57 (3) ◽  
pp. 371-381 ◽  
Author(s):  
Roger Y. Anderson ◽  
Bruce D. Allen ◽  
Kirsten M. Menking

AbstractEolian and subaqueous landforms composed of gypsum sand provide geomorphic evidence for a wet episode at the termination of glacial climate in southwestern North America. Drying of pluvial Lake Estancia, central New Mexico, occurred after ca. 12,000 14C yr B.P. Thereafter, eolian landforms on the old lake floor, constructed of gypsum sand, were overridden by rising lake water, modified by subaqueous processes, and organized into beach ridges along the lake's eastern shore. Preservation of preexisting eolian landforms in the shallow lake suggests abupt changes in lake level and climate. Available radiocarbon ages suggest that the final highstand recorded by beach ridges may have developed during the Younger Dryas (YD) stade. The beach ridges provide information about lake surface area, which was 45% of the lake area reached during the maximum highstands of the late Pleistocene. A similar proportional response has been reported for YD climate changes outside the North Atlantic region.


1960 ◽  
Vol 92 (9) ◽  
pp. 697-699
Author(s):  
Cornelius B. Philip

The species of the genus Hybomitra (Tylostypia) have been most vigorous of the family Tabanidae in colonizing the boreal regions. However, the number of holarctic Tabanidae of this genus is surprisingly few in consideration of the 53 species assigned to North America and the 86 to Eurasia. Only H. sexfasciata (Hine; borealis “Lw.” of authors), H. aequetincta (Becker) and H. epistates (O.S.) in addition to Chrysops nigripes Zett. have crossed the northern Atlantic and/or Pacific Oceans (Philip, 1956). It is not surprising therefore to discover that there is an additional holarctic species which has been known under two different names in the Old and New Worlds.


2014 ◽  
Vol 1 (3) ◽  
pp. 1-34 ◽  
Author(s):  
David Tilley ◽  
◽  
Serena Matt ◽  
Laura Schumann ◽  
Patrick Kangas ◽  
...  

2021 ◽  
Vol 49 (1) ◽  
pp. 171-195
Author(s):  
Jessie Reeder

This essay argues that scholarship being done under the sign of transatlantic studies, and Victorian transatlantic studies in particular, is problematically focused on the anglophone northern Atlantic region. Challenging both the essentialness and the disciplinary primacy of the “special relationship” between Britain and the United States, I argue instead that the entire nineteenth-century Atlantic world was a geographically and linguistically permeable space. Paying attention to crossings from north to south and vice versa is both methodologically and ethically necessary. From a methodological perspective, it can help us produce much more thorough answers to the questions transatlantic studies purports to ask about identity and community. But reading beyond anglophone British and U.S. American texts can also help us decolonize our reading and thinking. Of course, work like this requires scholars to read in second and third languages; as such, this essay discusses and denaturalizes the institutional barriers to multilingual English studies. It also offers a case study—a brief reading of a novel by Argentine writer Vicente Fidel López—demonstrating the insights that can be gained by expanding both our geographic perspective and our methodological toolbox.


2005 ◽  
Vol 84 (3) ◽  
pp. 241-245 ◽  
Author(s):  
W.B. Gallagher

AbstractThe Upper Cretaceous deposits of New Jersey and Delaware produced the first mosasaur specimens collected in North America. Recent recovery of mosasaur specimens from streambank exposures and new excavation sites has increased our knowledge of the stratigraphic distribution of these animals in the northern Atlantic coastal plain. Reassessment of the source and age of mosasaur specimens from the Big Brook site and other localities in Monmouth County (NJ) has greatly increased the number of known Campanian mosasaur specimens from this region. Two main taphonomic occurrence modes are noted: 1 - single, worn and broken bones and isolated teeth in mixed faunal deposits probably accumulated due to current action in nearshore environments; 2 - partial skeletons, skulls and single bones in deeper-water settings were the aftermath of biological modification of carcasses and deadfalls. The mosasaurs of the New Egypt Formation represent some of the last (i.e., stratigraphically highest) mosasaur fossils in North America. Mosasaur extinction was due to the collapse of the rich Late Cretaceous marine food web at the K/T boundary. Subsequently in the early Paleocene, with the disappearance of the mosasaurs, crocodilians became the apical predators of the marine environment in this area.


Antiquity ◽  
2014 ◽  
Vol 88 (340) ◽  
pp. 622-624 ◽  
Author(s):  
Michael J. O'Brien ◽  
Matthew T. Boulanger ◽  
Mark Collard ◽  
Briggs Buchanan ◽  
Lia Tarle ◽  
...  

The comments of Stanford and Bradley (above) do not address our criticisms and obfuscate the topic at hand with irrelevant data (e.g. the south-to-north movement of fluted points through the Ice Free Corridor), nonexistent data (e.g. ‘under the water’ or ‘destroyed sites’), and questionable data (e.g. Meadowcroft and Cactus Hill are by no means widely accepted, nor are Stanford and Bradley's ‘eight LGM sites’ in the mid-Atlantic region). Before touching on some of these points, we direct the reader to several recent articles (e.g. Morrow 2014; Raff & Bolnick 2014) that provide new evidence or arguments inconsistent with a trans-Atlantic migration, including the fact that DNA from the Clovis Anzick child (Montana) shows no European ancestry (Rasmussenet al. 2014). Although Stanford and Bradley describe their Solutrean ‘solution’ (Stanford & Bradley 1999) to the Pleistocene colonisation of North America as ‘testable’, their position is that the idea is correct until falsified. They propose that their colleagues have yet to provide sufficient ‘critiques’ or ‘challenges’ to discount it (see also Collins 2012; Collinset al. 2013). Yet they are the ones proposing a hypothesis inconsistent with overwhelming multidisciplinary evidence, and they ignore results of tests that do not support their claims.


2005 ◽  
Vol 21 (53-54) ◽  
pp. 243-268 ◽  
Author(s):  
Colin H. Williams

The name Acadia, given to a portion of the Atlantic region of North America, connotes a wide variety of territorial referents. From the results of a survey of a sample of New Brunswick high school students, it was determined that the exact nature and extent of the area known under the name of Acadia varied, depending on the sample location and ethnic affiliation of the respondants. But a core area common to all samples is centered on Moncton and its immediate hinterland.


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