Primary production of phytoplankton at a frontal zone located at the northern slope of the Dogger Bank (North Sea)

1990 ◽  
Vol 105 (2) ◽  
pp. 329-336 ◽  
Author(s):  
R. Riegman ◽  
H. Malschaert ◽  
F. Colijn
2011 ◽  
Vol 159 (2) ◽  
pp. 239-253 ◽  
Author(s):  
Jessica R. Frost ◽  
Anneke Denda ◽  
Clive J. Fox ◽  
Charles A. Jacoby ◽  
Rolf Koppelmann ◽  
...  

2013 ◽  
Vol 113 (1-3) ◽  
pp. 153-166 ◽  
Author(s):  
Liam Fernand ◽  
Keith Weston ◽  
Tom Morris ◽  
Naomi Greenwood ◽  
Juan Brown ◽  
...  

2018 ◽  
Vol 198 ◽  
pp. 181-207 ◽  
Author(s):  
David H. Roberts ◽  
David J.A. Evans ◽  
S. Louise Callard ◽  
Chris D. Clark ◽  
Mark D. Bateman ◽  
...  

1878 ◽  
Vol 5 (3) ◽  
pp. 97-100
Author(s):  
William Davies

Of the many private collections of vertebrate fossils found on or off the coast of the Eastern counties, none surpass in palæontological and also in geological interest the fine collection made with much zeal and care by Mr. J. J. Owles, of Yarmouth, inasmuch as the larger portion of the specimens are exclusively the remains of Postglacial Mammals, and were brought up in the fishermen’s dredge, either from, or in close proximity to the well-known Dogger Bank, thus proving conclusively the existence of submerged Pleistocene or Postglacial land lying off the Eastern coast in the North Sea. Prof. Boyd Dawkins is the only author, as far as I am at present aware, who has made any reference to this really valuable series of remains, and then only incidentally in his memoir, “On the Distribution of Postglacial Mammals.”


Geosciences ◽  
2019 ◽  
Vol 9 (8) ◽  
pp. 344 ◽  
Author(s):  
Andreas Neumann ◽  
H. Christian Hass ◽  
Jürgen Möbius ◽  
Céline Naderipour

Suspended, organic matter, especially in the form of adhesive extracellular polymers (EPS), tends to form flocs, which may also incorporate suspended lithogenic particles in coastal environments. With an increased settling velocity, these ballasted flocs form in a narrow zone along the coast and potentially represent a major source of pelagic primary production for the benthic community. We sought support for this hypothesis by examining our measurements of the mud content, porosity, permeability, pigment content, and specific respiration rate of sediment from the German Bight (North Sea) for signs that the pelagic zone of ballasted floc formation is affecting the local sediment characteristics. Based on a simple bottom-shear stress model and by employing empirical correlations of sediment characteristics we were able to find strong indications that this is actually the case. Our results demonstrate how ballasted flocs contribute to the benthic pelagic coupling in a high turbulence environment.


2005 ◽  
Vol 27 (9) ◽  
pp. 909-922 ◽  
Author(s):  
K. Weston ◽  
L. Fernand ◽  
D. K. Mills ◽  
R. Delahunty ◽  
J. Brown

1991 ◽  
Vol 22 (5) ◽  
pp. 241-244 ◽  
Author(s):  
Catherine F. Fileman ◽  
M. Althaus ◽  
R.J. Law ◽  
I. Haslam

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