The influence of sea animals on selenium distribution in tundra soils and lake sediments in maritime Antarctica

Chemosphere ◽  
2021 ◽  
pp. 132748
Author(s):  
Wenjuan Ye ◽  
Renbin Zhu ◽  
Linxi Yuan ◽  
Wanying Zhang ◽  
Huawei Zang ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Tundra Soils ◽  
Maritime Antarctica

scholarly journals Selenium volatilization from tundra soils in maritime Antarctica

2021 ◽  
Vol 146 ◽  
pp. 106189
Author(s):  
Wenjuan Ye ◽  
Linxi Yuan ◽  
Renbin Zhu ◽  
Xuebin Yin ◽  
Gary Bañuelos
Keyword(s):  
Tundra Soils ◽  
Maritime Antarctica

scholarly journals ANALYSIS OF SHALLOW LAKE SEDIMENTS IN THE FILDES PENINSULA, KING GEORGE ISLAND, MARITIME ANTARCTICA

2020 ◽  
Vol 21 (2) ◽  
Author(s):  
Janayna Cynthia De Medeiros Galvão ◽  
Rosemary Vieira ◽  
Kátia Kellem Da Rosa ◽  
Carina Petsch ◽  
Fabrício Ferreira ◽  
...  
Keyword(s):  
Lake Sediments ◽  
Shallow Lake ◽  
King George Island ◽  
Maritime Antarctica ◽  
Fildes Peninsula

scholarly journals Effects of sea animal colonization on the coupling between dynamics and activity of soil ammonia-oxidizing bacteria and archaea in maritime Antarctica

2019 ◽  
Vol 16 (20) ◽  
pp. 4113-4128 ◽  
Author(s):  
Qing Wang ◽  
Renbin Zhu ◽  
Yanling Zheng ◽  
Tao Bao ◽  
Lijun Hou
Keyword(s):  
Ammonia Oxidation ◽  
Amoa Gene ◽  
Ammonia Oxidizing Bacteria ◽  
Nitrogen Transformations ◽  
Tundra Soils ◽  
Maritime Antarctica ◽  
Soil C ◽  
Oxidation Rates ◽  
Ammonia Oxidizing Archaea ◽  
Tundra Ecosystem

Abstract. The colonization by a large number of sea animals, including penguins and seals, plays an important role in the nitrogen cycle of the tundra ecosystem in coastal Antarctica. However, little is known about the effects of sea animal colonization on ammonia-oxidizing archaea (AOA) and bacteria (AOB) communities involved in nitrogen transformations. In this study, we chose active seal colony tundra soils (SSs), penguin colony soils (PSs), adjacent penguin-lacking tundra soils (PLs), tundra marsh soils (MSs), and background tundra soils (BSs) to investigate the effects of sea animal colonization on the abundance, activity, and diversity of AOA and AOB in maritime Antarctica. Results indicated that AOB dominated over AOA in PS, SS, and PL, whereas AOB and AOA abundances were similar in MS and BS. Penguin or seal activities increased the abundance of soil AOB amoA genes but reduced the abundance of AOA amoA genes, leading to very large ratios (1.5×102 to 3.2×104) of AOB to AOA amoA copy numbers. Potential ammonia oxidation rates (PAORs) were significantly higher (P=0.02) in SS and PS than in PL, MS, and BS and were significantly positively correlated (P<0.001) with AOB amoA gene abundance. The predominance of AOB over AOA and their correlation with PAOR suggested that AOB play a more important role in the nitrification in animal colony soils. Sequence analysis for gene clones showed that AOA and AOB in tundra soils were from the Nitrososphaera and Nitrosospira lineages, respectively. Penguin or seal activities led to a predominance of AOA phylotypes related to Nitrososphaera cluster I and AOB phylotypes related to Nitrosospira clusters I and II but very low relative abundances in AOA phylotypes related to cluster II, and AOB phylotypes related to clusters III and IV. The differences in AOB and AOA community structures were closely related to soil biogeochemical processes under the disturbance of penguin or seal activities: soil C : N alteration and sufficient input of NH4+–N and phosphorus from animal excrements. The results significantly enhanced the understanding of ammonia-oxidizing microbial communities in the tundra environment of maritime Antarctica.

scholarly journals Effects of Sea Animal Colonization on the Coupling between Dynamics and Activity of Soil Ammonia-oxidizing Bacteria and Archaea in Maritime Antarctica

2019 ◽  
Author(s):  
Qing Wang ◽  
Renbin Zhu ◽  
Yanling Zheng ◽  
Tao Bao ◽  
Lijun Hou
Keyword(s):  
Ammonia Oxidation ◽  
Amoa Gene ◽  
Ammonia Oxidizing Bacteria ◽  
Nitrogen Transformations ◽  
Tundra Soils ◽  
Maritime Antarctica ◽  
Oxidation Rates ◽  
Ammonia Oxidizing Archaea ◽  
Copy Numbers ◽  
Tundra Ecosystem

Abstract. The colonization of a large number of sea animal, including penguins and seals, plays an important role in the nitrogen cycle of the tundra ecosystem in coastal Antarctica. However, little is known about the effects of sea animal colonization on ammonia-oxidizing archaea (AOA) and bacteria (AOB) communities involved in nitrogen transformations. In this study, we chose active seal colony tundra soils (STS), penguin colony soils (PTS), adjacent penguin-lacking tundra soils (PLS), tundra marsh soils (MS), and background tundra soils (BS), to investigate the effects of sea animal colonization on the abundance, activity, and diversity of AOA and AOB in maritime Antarctica. Results indicated that AOB dominated over AOA in PTS, STS, and PLS; whereas AOB and AOA abundances were similar in MS and BS. Penguin or seal activities increases the abundance of soil AOB amoA genes, but reduced the abundance of AOA amoA genes, leading to very large ratios (1.5 × 102 to 3.2 × 104) of AOB to AOA amoA copy numbers. Ammonia oxidation rates were significantly higher (P = 0.02) in STS and PTS than in PLS, MS, and BS, and were significantly positively correlated (P < 0.001) with AOB amoA gene abundance suggesting that AOB are more important in the nitrification in animal colony soils. Sequence analysis for gene clones showed that AOA and AOB in tundra soils were from the Nitrosospira and Nitrososphaera lineages, respectively. Seal or penguin activities led to the predominant existence of AOA phylotypes related to Nitrososphaera cluster I and AOB phylotypes related to Nitrosospira clusters I and II, but very low relative abundances in AOA phylotypes related to cluster II, and AOB phylotypes related to cluster III and IV. The differences in AOB and AOA community structures were closely related to soil biogeochemical processes under the disturbance of penguin or seal activities: soil C:N alteration and sufficient input of NH4+–N and phosphorus from animal excrements. The results provide insights into the mechanisms how microbes drive nitrification in maritime Antarctica.

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.

Sedimentation of Pb-210 in Laurentian Shield Lakes

1984 ◽  
Vol 19 (2) ◽  
pp. 97-109 ◽  
Author(s):  
R.J. Cornett ◽  
L. Chant ◽  
D. Link
Keyword(s):  
Lake Sediments ◽  
Water Column ◽  
Rate Constant ◽  
Bottom Sediments ◽  
Atmospheric Fallout ◽  
Small Lakes ◽  
Fractional Rate ◽  
Total Input ◽  
Shield Lakes ◽  
Annual Flux

Abstract The average annual flux of Pb-210 from the atmosphere to lake surfaces and to the bottom sediments was measured in seven small lakes located on the Laurentian Shield. Direct atmospheric fallout of Pb-210 was 136 ± 16 Bq m-2 a-1 Streams from the lakes' catchments input an additional 5 to 473 Bq m-2 a-1. Only 16 to 80 percent of the total input was found in the lake sediments. The fractional rate constant for Pb-210 sedimentation from the water column ranged from 0.25 to 5.3 per annum.

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