Analyzing the causes for the persistence of chironomids in floodplain lake sediments

2005 ◽  
Vol 162 (2) ◽  
pp. 211-228 ◽  
Author(s):  
Elske M. de Haas ◽  
R. van Haaren ◽  
Albert A. Koelmans ◽  
Michiel H.S. Kraak ◽  
W. Admiraal
Keyword(s):  
Lake Sediments ◽  
Floodplain Lake

scholarly journals Evaluation of the Siltation of River Taquari, Pantanal, Brazil, through 210Pb Geochronology of Floodplain Lake Sediments

2002 ◽  
Vol 13 (1) ◽  
pp. 71-77 ◽  
Author(s):  
José M. Godoy ◽  
Carlos R. Padovani ◽  
Jean R. D. Guimarães ◽  
José C. A. Pereira ◽  
Luis M. Vieira ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Floodplain Lake ◽  
210Pb Geochronology

Responses of benthic invertebrates to combined toxicant and food input in floodplain lake sediments

2002 ◽  
Vol 21 (10) ◽  
pp. 2165-2171 ◽  
Author(s):  
Elske M. De Haas ◽  
Bas Reuvers ◽  
Caroline T. A. Moermond ◽  
Albert A. Koelmans ◽  
Michiel H. S. Kraak
Keyword(s):  
Lake Sediments ◽  
Benthic Invertebrates ◽  
Floodplain Lake ◽  
Food Input

Holocene floodplain lake sediments in the Amazon: 14C dating and palaeoecological use

1991 ◽  
Vol 10 (4) ◽  
pp. 363-372 ◽  
Author(s):  
Matti E. Räsänen ◽  
Jukka S. Salo ◽  
Högne Jungner
Keyword(s):  
Lake Sediments ◽  
Floodplain Lake ◽  
14C Dating

Influence of liming on metal burdens in lake sediments

2003 ◽  
Vol 107 ◽  
pp. 1349-1351
Author(s):  
T. Wällstedt ◽  
H. Borg
Keyword(s):  
Lake Sediments

Application of graphical analysis of taxonomical structure of diatom complexes in identification of critical conditions of the Neopleistocene lakes (on the example of Bibirevo section)

2019 ◽  
pp. 78-87
Author(s):  
Elena V. Bespalova
Keyword(s):  
Lake Sediments ◽  
Critical Points ◽  
Graphical Analysis ◽  
Volga Region ◽  
Critical Conditions ◽  
Ancient Lake ◽  
Diatom Complexes

Ancient lake sediments of Bibirevo section in the Yaroslavl and Kostroma Volga region are studied by means of graphical analysis of taxonomical structure of diatom complexes. This method allowed to record critical points (change of areas of stability) in the development of a Neopleistocene lake during the transition from stage to stage, as well as from phase to phase.

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