Spawning migration and larval drift of anadromous North Sea houting (Coregonus oxyrinchus) in the River IJssel, the Netherlands

2013 ◽  
Vol 23 (2) ◽  
pp. 161-170 ◽  
Author(s):  
Jost Borcherding ◽  
André W. Breukelaar ◽  
Hendrik V. Winter ◽  
Ulrike König
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Spawning Migration ◽  
Larval Drift ◽  
River Ijssel

scholarly journals A southern North Sea Miocene dinoflagellate cyst zonation

2004 ◽  
Vol 83 (4) ◽  
pp. 267-285 ◽  
Author(s):  
D.K. Munsterman ◽  
H. Brinkhuis
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
North Atlantic ◽  
The South ◽  
Dinoflagellate Cyst ◽  
South Eastern ◽  
Southern North Sea ◽  
Age Model

AbstractAn integrated stratigraphical analysis emphasizing organic-walled dinoflagellate cyst (dinocyst) distribution has been carried out on multiple boreholes penetrating the Miocene in the subsurface of the Netherlands (southern North Sea Basin). The bulk of the investigated successions is attributed to the Breda Formation, a regional lithostatigraphical unit most complete in the south-eastern part of the Netherlands. In concert with a first regional integrated bio (chrono) sequence-stratigraphical framework, fourteen informal dinocyst zones for the southern North Sea Miocene (SNSM), and three subzones are proposed for the Breda Formation. By also integrating (chrono)stratigraphic information from Mediterranean and North Atlantic dinocyst studies a first ever detailed age-model is here proposed for the Miocene in the subsurface of the Netherlands.

Comparative Analysis of Salt Structures in the Southern North Sea, Dutch Offshore, the Netherlands

Geotectonics ◽  
2020 ◽  
Vol 54 (6) ◽  
pp. 807-820
Author(s):  
M. A. F. Miraj ◽  
A. Ali ◽  
N. Ahsan ◽  
Sh. Afgan ◽  
R. F. Saleem
Keyword(s):  
Comparative Analysis ◽  
The Netherlands ◽  
North Sea ◽  
Southern North Sea

Ontstaan en vroege ontwikkeling van Kampen

2020 ◽  
Vol 5 (2) ◽  
pp. 66-87
Author(s):  
JOHANS C.G. KREEK
Keyword(s):  
North Sea ◽  
Bulk Carrier ◽  
The Baltic Sea ◽  
The North ◽  
12Th Century ◽  
The North Sea ◽  
Ex Nihilo ◽  
The Baltic ◽  
The Town ◽  
River Ijssel

The emergence and early development of Kampen The town Kampen, at the mouth of the river IJssel (The Netherlands), seems to have originated in the 12th century ex nihilo. To explain this enigmatic start, many theories have been proposed. This article attributes its origin to a series of events, that started with the silting up of the Limjefjord after 1120 in the north of Jutland. This fjord was an important connection between the North Sea and the Baltic Sea for the small boats of the Frisian trade. The silting up of the fjord was a direct reason for the creation of the cog, a larger bulk carrier, that could circumnavigate Cape Skagen. Moreover, it could also take a shortcut over high seas to the mouth of the Vlie, and over the Almere to the mouth of the river IJssel. From there, the smaller Frisian ships used to sail over the IJssel to the German Rhine area, which was impossible for the seagoing cog. Therefore, the introduction of the cog prompted the foundation of a port for transshipment in the first half of the 12th century. This means Kampen did already exist as a settlement, when a storm surge in 1170 turned the Almere into the Zuiderzee and the settlement could take advantage of this environmental change.

Blame the Barbarians

2021 ◽  
pp. 39-82
Author(s):  
Arika Okrent ◽  
Sean O’Neill
Keyword(s):  
The Netherlands ◽  
Old English ◽  
North Sea ◽  
Religious Texts ◽  
The North ◽  
The People ◽  
Latin Language ◽  
The North Sea ◽  
Germanic Languages ◽  
Over Time

This chapter tells the story of how English got to be the weird way it is, which begins with the Germanic languages and the barbarians who spoke them. During the 5th century, an assortment of them poured across the North Sea, from what is today Denmark, the Netherlands, and Northern Germany, and conquered most of England. After about a century of the Germanic tribes taking over and settling in, the Romans returned. This time it was not soldiers but missionaries who arrived. The monks who came to convert the island to Christianity brought their Latin language with them, and they also brought the Latin alphabet. They set about translating religious texts into the language of the people they encountered, a language that by this time had coalesced into something that was Old English. However, there is another group of barbarians to blame: the Vikings. Their language was similar enough to Old English that they could communicate with the Anglo-Saxons without too much difficulty, and over time their own way of speaking mixed into the surrounding language, leaving vocabulary and expressions behind that do not quite fit the rest of the pattern at the old Germanic layer.

Migration history of North Sea houting (Coregonus oxyrinchus L.) caught in Lake IJsselmeer (The Netherlands) inferred from scale transects of 88Sr:44Ca ratios

2008 ◽  
Vol 70 (1) ◽  
pp. 47-56 ◽  
Author(s):  
Jost Borcherding ◽  
Carola Pickhardt ◽  
Hendrik V. Winter ◽  
J. Sabine Becker
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Migration History ◽  
History Of

Benthic Habitat Variations over Tidal Ridges, North Sea, the Netherlands

2012 ◽  
pp. 241-249 ◽  
Author(s):  
Thaiënne A.G.P. van Dijk ◽  
Jan A. van Dalfsen ◽  
Vera Van Lancker ◽  
Ronnie A. van Overmeeren ◽  
Sytze van Heteren ◽  
...  
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Benthic Habitat

scholarly journals STABILITY PARAMETERS OF WESTERN SCHELDT ESTUARY

1984 ◽  
Vol 1 (19) ◽  
pp. 205 ◽  
Author(s):  
H. De Jong ◽  
F. Gerritsen
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Scheldt Estuary ◽  
Stability Parameters ◽  
The North ◽  
The North Sea ◽  
The City

The Western Scheldt is a major estuary in the Southern part of The Netherlands and the Northern part of Belgium. It is an important navigational route connecting the city of Antwerp with the North Sea. At the entrance Vlissingen is a major Dutch port.

scholarly journals Towards an improved lithostratigraphic subdivision of the Chalk Group in the Netherlands North Sea area - A seismic stratigraphic approach

2007 ◽  
Vol 86 (2) ◽  
pp. 131-143 ◽  
Author(s):  
A.S. van der Molen ◽  
Th.E. Wong
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
Well Log ◽  
Seismic Sequence ◽  
Stratigraphic Analysis ◽  
Lithostratigraphic Units ◽  
Sequence Boundaries ◽  
Sea Area ◽  
2D And 3D ◽  
Stratigraphic Sequences

AbstractIn the Netherlands North Sea area, the Chalk Group has thus far been subdivided into the Cenomanian Texel Formation, the Turonian to Maastrichtian Ommelanden Formation and the Danian Ekofisk Formation. This paper describes the attempt to arrive at a more detailed lithostratigraphic subdivision for this area, particularly of the Ommelanden Formation. To this end, a seismic stratigraphic analysis was carried out on a regional 2D and 3D seismic dataset. The Chalk Group was subdivided into eleven seismic stratigraphic sequences, named CK1 through CK11, based on the mapping and correlation of unconformities. The identified seismic sequence boundaries were used as the main chronostratigraphic markers in the Chalk Group interval. The seismic dataset was subsequently expanded with well log data of 45 boreholes. These were tied to the seismic dataset by constructing a synthetic seismogram for each borehole, after which the seismic sequence boundaries were noted and correlated on the logs. Finally, micropaleonthological data available in 15 boreholes were used to date the seismic sequences. The sequences were interpreted to be of Cenomanian (CK1), Turonian (CK2), Coniacian (CK3), Santonian (CK4), Early Campanian (CK5; CK6), Middle to Late Campanian (CK7), Early Maastrichtian (CK8; CK9), Late Maastrichtian (CK10) and Danian (CK11) age. The seismic units recognised in this study were compared with formal lithostratigraphic units defined in the Chalk Group in the surrounding North Sea sectors. Based on this comparison, a revision of the formal lithostratigraphic scheme, recognising Tor Formation and Herring Formation equivalents, is suggested for the Netherlands North Sea area.

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