Using geological history of the Laurentian Great Lakes to better understand their future

2010 ◽  
Vol 13 (2) ◽  
pp. 118-126
Author(s):  
C. F.M. Lewis ◽  
D. K. Rea ◽  
J. B. Hubeny ◽  
T. A. Thompson ◽  
S. M. Blasco ◽  
...  
2019 ◽  
Vol 45 (6) ◽  
pp. 1011-1035 ◽  
Author(s):  
R.A. Sturtevant ◽  
D.M. Mason ◽  
E.S. Rutherford ◽  
A. Elgin ◽  
E. Lower ◽  
...  

2020 ◽  
Author(s):  
Megan D. Niner ◽  
Carol A. Stepien ◽  
Bartolomeo Gorgoglione ◽  
Douglas W. Leaman

AbstractViral Hemorrhagic Septicemia Virus (VHSV) (=Piscine novirhabdovirus) appeared in the Laurentian Great Lakes in 2005, constituting a unique and highly virulent genogroup (IVb), which killed >32 fish species in large 2005 and 2006. Periods of apparent dormancy punctuated smaller outbreaks in 2007, 2008, and 2017. We conducted the first whole genome analysis of IVb, evaluating its evolutionary changes using 46 isolates, in reference to immunogenicity in cell culture, and the genomes of other VHS genogroups (I–IVa) and other Novirhabdoviruses. IVb isolates had 253 genomic nucleotide substitutions (2.3% of the total 11,158 nucleotides), with 85 (16.6%) being non-synonymous. The greatest number of substitutions occurred in the non-coding region (NCDS; 4.3%) followed by the Nv- (3.8%), and M- (2.8%) genes. The M-gene possessed the greatest proportions of amino acid changes (52.9%), followed by the Nv- (50.0%), G- (48.6%), N- (35.7%) and L- (23.1%) genes. Among VHS genogroups, IVa from the northeastern Pacific exhibited the fastest substitution rate (2.01×10-3), followed by Ivb (6.64×10−5), and I/III from Europe (4.09×10−5). A 2016 gizzard shad isolate from Lake Erie was the most divergent IVb isolate (38 NT, 15.0%, 15 AA), yet exhibited reduced virulence with in vitro immunogenicity analyses, as did other 2016 isolates, in comparison to the first IVb isolate (2003). The 2016 isolates exhibited lower impact on innate antiviral responses, suggesting phenotypic effects. Results suggest continued sequence change and lower virulence over the history of IVb, which may facilitate its long-term persistence in fish host populations.


Author(s):  
John Lekki ◽  
R. Anderson ◽  
Q.-V. Nguyen ◽  
J. Demers ◽  
J. Flatico ◽  
...  

2000 ◽  
Vol 30 (3) ◽  
pp. 474-476 ◽  
Author(s):  
LUIZ JOSÉ TOMAZELLI ◽  
SÉRGIO REBELLO DILLENBURG ◽  
JORGE ALBERTO VILLWOCK

2018 ◽  
Vol 938 (8) ◽  
pp. 38-43
Author(s):  
S.A. Kotler ◽  
I.D. Zolnikov ◽  
D.V. Pchelnikov

The types of geological and geomorphological structure of the Katun valley are distinguished in the work. For this, a method of geoinformation mapping using morphometric indicators of the valley’s width and meandering of the channel was developed. The morphometric parameter of the valley’s width was calculated as the total area of terraces. As the morphometric parameters of the channel’s meandering, the angles of the river segments’ deviation relative to each other were calculated. Conjugated analysis of these morphometric indicators enabled identifying 18 morphotypes. These morphotypes according to the geological and geomorphological structure of the valley were combined into 4 classes. Separation of the Katun valley in certain classes and morphotypes is due to the different geological history of these sites during the Quaternary period. The most important reasons predetermining the modern variety of geological and geomorphological types of the valley are neotectonic movements and exogenous phenomena (glaciers, dam lakes, landslides, etc.) naturally localized in the space from the upstream of the river to its exit into the foothills. The developed method can be applied for quantitative morphometric classification of the mountain rivers’ valleys in other regions.


2016 ◽  
Author(s):  
Celine Martin ◽  
◽  
George E. Harlow ◽  
George E. Harlow ◽  
George E. Harlow ◽  
...  

2017 ◽  
Author(s):  
John W. Johnston ◽  
◽  
Erin P. Argyilan ◽  
Steve J. Baedke ◽  
Sean Morrison ◽  
...  

Author(s):  
Edward S. Rutherford ◽  
Hongyan Zhang ◽  
Yu‐Chun Kao ◽  
Doran M. Mason ◽  
Ali Shakoor ◽  
...  

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