scholarly journals Frequency of PRRS live vaccine virus (European and North American genotype) in vaccinated and non-vaccinated pigs submitted for respiratory tract diagnostics in North-Western Germany

2009 ◽  
Vol 92 (1-2) ◽  
pp. 31-37 ◽  
Author(s):  
Elisabeth grosse Beilage ◽  
Heiko Nathues ◽  
Diana Meemken ◽  
Timm C. Harder ◽  
Marcus G. Doherr ◽  
...  
2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Bryan D. Griffin ◽  
Mable Chan ◽  
Nikesh Tailor ◽  
Emelissa J. Mendoza ◽  
Anders Leung ◽  
...  

AbstractWidespread circulation of SARS-CoV-2 in humans raises the theoretical risk of reverse zoonosis events with wildlife, reintroductions of SARS-CoV-2 into permissive nondomesticated animals. Here we report that North American deer mice (Peromyscus maniculatus) are susceptible to SARS-CoV-2 infection following intranasal exposure to a human isolate, resulting in viral replication in the upper and lower respiratory tract with little or no signs of disease. Further, shed infectious virus is detectable in nasal washes, oropharyngeal and rectal swabs, and viral RNA is detectable in feces and occasionally urine. We further show that deer mice are capable of transmitting SARS-CoV-2 to naïve deer mice through direct contact. The extent to which these observations may translate to wild deer mouse populations remains unclear, and the risk of reverse zoonosis and/or the potential for the establishment of Peromyscus rodents as a North American reservoir for SARS-CoV-2 remains unknown.


PLoS ONE ◽  
2020 ◽  
Vol 15 (6) ◽  
pp. e0234044 ◽  
Author(s):  
J. Liebing ◽  
I. Völker ◽  
N. Curland ◽  
P. Wohlsein ◽  
W. Baumgärtner ◽  
...  

2012 ◽  
Vol 86 ◽  
pp. 138-149 ◽  
Author(s):  
C. Münsterer ◽  
J. Fohlmeister ◽  
M. Christl ◽  
A. Schröder-Ritzrau ◽  
V. Alfimov ◽  
...  

1997 ◽  
Vol 43 (145) ◽  
pp. 495-502 ◽  
Author(s):  
Jan A. Piotrowski ◽  
Anna M. Kraus

AbstractLaboratory tests on sediment over-ridden by the last ice sheet in north-western Germany reveal very low ice-induced pre-consolidation and high palaeo-pore-water pressures. Sediment consolidation at the base of the glacier was largely controlled by hydraulic properties of the substratum. Generally low permeabilities of the bed caused sustained high pore-water pressure in over-ridden sediments close to the flotation point. This implies a serious possibility of hydraulic lifting of the ice sheet. It is believed that the reduced basal coupling limited the transformation of glacier shear stress on to the bed sediments, which is indicated by a lack of sedimentological evidence for widespread pervasive bed deformation. Ice motion was probably focused at the glacier sole by some combination of sliding and ploughing. However, isolated spots with deformation occur, so that the subglacial system in the study area can be characterized as a stable/deforming mosaic.


1994 ◽  
Vol 12 (2) ◽  
pp. 137-179 ◽  
Author(s):  
S. Brakensiek

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