Vertical and spatial distribution of biogenic silica in the sediment of the gulf of Riga, Baltic Sea

1997 ◽  
Vol 60 (1-4) ◽  
pp. 245-259 ◽  
Author(s):  
Rolf Carman ◽  
Juris Aigars
2021 ◽  
Vol 172 ◽  
pp. 112860
Author(s):  
Juris Aigars ◽  
Marta Barone ◽  
Natalija Suhareva ◽  
Ieva Putna-Nimane ◽  
Inta Dimante-Deimantovica

2000 ◽  
Vol 35 (4) ◽  
pp. 373-385 ◽  
Author(s):  
S. Vilbaste ◽  
K. Sundbäck ◽  
C. Nilsson ◽  
J. Truu

1986 ◽  
Vol 23 (9) ◽  
pp. 1442-1449 ◽  
Author(s):  
Daniel J. Conley ◽  
Claire L. Schelske ◽  
Brian G. Dempsey ◽  
Charles D. Campbell ◽  
Teresa L. Newberry

The spatial distribution of biogenic silica (BSi) in the surficial sediments of Lake Michigan is described from Shipek grab samples collected in 1975 and gravity cores obtained in 1983. Significantly smaller surficial BSi concentrations in the 1975 samples were attributed primarily to the inability of a Shipek grab to collect intact surficial sediment samples. Lower concentrations o.f BSi were found in nondepositional and transitional areas of sediment accumulation than in depositional basins. Therefore, BSi accumulation is restricted primarily to the 40% of the lake bottom where sediments are presently accumulating. High concentrations found in Green Bay surficial sediments are related to high productivity in the bay coupled with inputs of new silica from the Fox River. In the open lake, BSi concentrations of surficial sediments in depositional basins appeared to vary inversely with sedimentation rate in that lower BSi concentrations were found in areas with higher sedimentation rates.


2018 ◽  
Vol 207 ◽  
pp. 82-92 ◽  
Author(s):  
Kolja Beisiegel ◽  
Alexander Darr ◽  
Michael L. Zettler ◽  
René Friedland ◽  
Ulf Gräwe ◽  
...  

1997 ◽  
Vol 203 (2) ◽  
pp. 93-104 ◽  
Author(s):  
Jerzy Falandysz ◽  
Lidia Strandberg ◽  
Per-Anders Bergqvist ◽  
Bo Strandberg ◽  
Christoffer Rappe

2017 ◽  
Vol 14 (8) ◽  
pp. 2113-2131 ◽  
Author(s):  
Ye Liu ◽  
H. E. Markus Meier ◽  
Kari Eilola

Abstract. Long-term oxygen and nutrient transports in the Baltic Sea are reconstructed using the Swedish Coastal and Ocean Biogeochemical model (SCOBI) coupled to the Rossby Centre Ocean model (RCO). Two simulations with and without data assimilation covering the period 1970–1999 are carried out. Here, the weakly coupled scheme with the Ensemble Optimal Interpolation (EnOI) method is adopted to assimilate observed profiles in the reanalysis system. The reanalysis shows considerable improvement in the simulation of both oxygen and nutrient concentrations relative to the free run. Further, the results suggest that the assimilation of biogeochemical observations has a significant effect on the simulation of the oxygen-dependent dynamics of biogeochemical cycles. From the reanalysis, nutrient transports between sub-basins, between the coastal zone and the open sea, and across latitudinal and longitudinal cross sections are calculated. Further, the spatial distributions of regions with nutrient import or export are examined. Our results emphasize the important role of the Baltic proper for the entire Baltic Sea, with large net transport (export minus import) of nutrients from the Baltic proper into the surrounding sub-basins (except the net phosphorus import from the Gulf of Riga and the net nitrogen import from the Gulf of Riga and Danish Straits). In agreement with previous studies, we found that the Bothnian Sea imports large amounts of phosphorus from the Baltic proper that are retained in this sub-basin. For the calculation of sub-basin budgets, the location of the lateral borders of the sub-basins is crucial, because net transports may change sign with the location of the border. Although the overall transport patterns resemble the results of previous studies, our calculated estimates differ in detail considerably.


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