On the biology of the Japanese swimming crab Charybdis japonica (Portunidae) in waters of primorye at the northern boundary of their range

2011 ◽  
Vol 37 (7) ◽  
pp. 570-578 ◽  
Author(s):  
N. V. Kolpakov ◽  
E. V. Kolpakov
Keyword(s):  
Swimming Crab ◽  
Northern Boundary ◽  
Charybdis Japonica

Mitochondrial prohibitin and its ubiquitination during spermatogenesis of the swimming crab Charybdis japonica

Gene ◽  
2017 ◽  
Vol 627 ◽  
pp. 137-148 ◽  
Author(s):  
Ya-Ru Xu ◽  
Yun-Shu Fan ◽  
Wan-Xi Yang
Keyword(s):  
Swimming Crab ◽  
Charybdis Japonica

The effect of two pot types on entrance rate and entrance behavior of the invasive Japanese swimming crab Charybdis japonica

2006 ◽  
Vol 77 (3) ◽  
pp. 271-274 ◽  
Author(s):  
Miguel Vazquez Archdale ◽  
Lika Kariyazono ◽  
Cherry Pilapil Añasco
Keyword(s):  
Swimming Crab ◽  
Charybdis Japonica

Ribosomal DNA Intergenic Spacer of the Swimming Crab, Charybdis japonica

1999 ◽  
Vol 49 (6) ◽  
pp. 806-809 ◽  
Author(s):  
Seong Ho Ryu ◽  
Yoon Kyung Do ◽  
Ui Wook Hwang ◽  
Chong Pyo Choe ◽  
Won Kim
Keyword(s):  
Ribosomal Dna ◽  
Intergenic Spacer ◽  
Swimming Crab ◽  
Charybdis Japonica

Ages of carbonatites and other alkaline rocks in Quebec

1968 ◽  
Vol 5 (6) ◽  
pp. 1401-1407 ◽  
Author(s):  
Ronald Doig ◽  
Jackson M. Barton Jr.
Keyword(s):  
Northern Boundary ◽  
Alkaline Rocks ◽  
Continuous Structure ◽  
Boundary Fault ◽  
Igneous Activity ◽  
Lowland Area

Potassium-argon ages have been determined for alkaline rocks, including carbonatites, from some fifteen localities in Quebec. Nine centers of intrusion, including two previously documented localities, yield ages in the range 400 to 600 million years. All but two of these are located on or very near the northern boundary fault of the St. Lawrence graben system. Included in this group are four carbonatites with remarkably similar ages of intrusion (565 m.y.). The existence of this widespread coeval igneous activity along a 1200-mile segment of the lowland area and its westward extension supports the hypothesis that the St. Lawrence graben is a continuous structure, and indicates that the system has been active for at least 600 million years.

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