Recent benthic foraminiferal distribution in the Elbe Estuary (North Sea, Germany): A response to environmental stressors

2021 ◽  
Vol 251 ◽  
pp. 107198
Author(s):  
Fabio Francescangeli ◽  
Yvonne Milker ◽  
Dorothea Bunzel ◽  
Helmuth Thomas ◽  
Mona Norbisrath ◽  
...  
2021 ◽  
Author(s):  
Mona Norbisrath ◽  
Jeannette Hansen ◽  
Kirstin Dähnke ◽  
Tina Sanders ◽  
Justus E. E. van Beusekom ◽  
...  

<p>The Elbe is the largest river entering the German Bight. Its estuary is a heavily used waterway connecting the sea to Germany’s biggest port in Hamburg. The Elbe navigation channel is continuously dredged, and agricultural fertilizer input from the catchment ensuing large phytoplankton blooms in the river Elbe exerts additional anthropogenic pressure. Biogeochemistry in the estuary is additionally governed by the North Sea and its strong tidal cycles, which ensure an exchange of fresh and marine waters.</p><p>The aims were to quantify the release of the carbon species total alkalinity (TA) and dissolved inorganic carbon (DIC) along the Elbe estuary, and to estimate the contribution of aerobe and anaerobe metabolic processes. Therefore, we used water samples collected continuously during a cruise in June 2019, to measure TA and DIC, and the stable isotopes of nitrate. We applied mass balances, to characterize the metabolic activity and detect their effect on the carbon species</p><p>The Elbe estuary could be subdivided into two parts: 1) an outer marine driven part, which is dominated by conservative mixing, also visible in higher TA than DIC values, and 2) an inner fresh water part in which metabolic processes play an important role.</p><p>We found a strong increase in TA and DIC (several hundred µmol kg<sup>-1</sup>) in the Hamburg port area, with higher DIC than TA values. We unraveled the water column impacts of nitrification and denitrification on TA and DIC by analyzing the stable isotopes δ<sup>15</sup>N-NO<sub>3</sub><sup>-</sup> and δ<sup>18</sup>O-NO<sub>3</sub><sup>-</sup>, and identified water column nitrification as a dominant pelagic process in the port of Hamburg and in the fresh water part further downstream. Because nitrification cannot explain the significant increase of TA and DIC in the port region, anaerobic processes such as denitrification in the sediment also appear to play an important role.</p><p> </p>


1970 ◽  
Vol 1 (12) ◽  
pp. 130
Author(s):  
Harold Gohren

Along gently sloping coasts of seas having rotary tidal currents, the symmetry of the rotary current is interrupted where the water is shallow As a result, residual counter currents are formed The dynamics of such a current system are described based on current measurements in the Elbe Estuary (southeastern North Sea) The residual currents of this area result in the movement of bottom sediment and are most likely responsible for a series of similar appearing morphologic features.


Nematology ◽  
2010 ◽  
Vol 12 (6) ◽  
pp. 809-826 ◽  
Author(s):  
Dieter Sturhan ◽  
Johannes Hallmann

Abstract Four Hirschmanniella species are known to occur in Europe: H. gracilis, H. loofi, H. behningi and H. zostericola; a fifth species, H. halophila sp. n., is described from Germany, where it was found along the Elbe estuary and on the adjoining coast of the North Sea. Three other species reported for Europe are considered as species inquirendae or appear to be misidentified. Based on sampling material from Germany, detailed morphological descriptions of H. gracilis, H. loofi and H. behningi are given; H. zostericola has not been found since its first description. The variability, even of characters of diagnostic significance, may be enormous, which makes correct identification difficult if little material is available. Hirschmanniella halophila sp. n. is morphologically very close to H. caudacrena, which has been isolated several times from aquarium plants imported from East Asia to Germany and for which morphological details are given. In Germany, H. gracilis is the most common species and is widely distributed; it is also known from many other European countries. Hirschmanniella loofi (also known from The Netherlands, Belgium, Poland and Italy) is less common. Hirschmanniella behningi, previously reported only from Russia and Sweden, was identified from nine places in Germany, including several coastal sites. Most of the Hirschmanniella records refer to moist soils with reed and other grasses or sedges; only H. gracilis was found exceptionally in arable soil. At many sampling sites, two or even three Hirschmanniella species co-occurred. A table for distinguishing the five European species is presented.


1983 ◽  
Vol 52 (1-2) ◽  
pp. 75-99 ◽  
Author(s):  
Tjeerd C.E Van Weering ◽  
Gunnbjørg Qvale

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