scholarly journals Chroococcoid cyanobacteria: a significant component in the food web dynamics of the open ocean

1986 ◽  
Vol 28 ◽  
pp. 291-297 ◽  
Author(s):  
R Iturriaga ◽  
BG Mitchell
2021 ◽  
Vol 251 ◽  
pp. 107259
Author(s):  
D. Szalaj ◽  
M.A. Torres ◽  
T. Veiga-Malta ◽  
M.M. Angélico ◽  
L. Sobrinho-Gonçalves ◽  
...  

2000 ◽  
Vol 12 (4) ◽  
pp. 414-417 ◽  
Author(s):  
Harvey Marchant ◽  
Andrew Davidson ◽  
Simon Wright ◽  
John Glazebrook

The concentrations of viruses, bacteria, chroococcoid cyanobacteria and chlorophyll a were determined in surface waters of the Southern Ocean during spring. Viral concentrations declined southward from around 4 × 106 ml−1 near Tasmania to a minimum of around 1 × 106 ml−1 at the Polar Front. South of the Front, virus concentrations increased again, reaching around 4 × 106 ml−1 in the sea-ice zone south of 60°S. Bacterial concentration decreased southwards across the Southern Ocean from around 6.5 × 105 ml−1 near Tasmania to < 1.0 × 105 ml−1 in the sea-ice zone. Cyanobacteria accounted for < 8% of the prokaryotes. There was no significant relationship between viral abundance and eithercyanobacterial or chl a concentration. Viral and bacterial concentrations were not significantly correlated north (P {0.10 < r < 0.20}) or south (P {0.20 < r < 0.5}) of the Polar Front. The virus to bacteria ratio (VBR) was between 3 and 15 in the open ocean but varied between 15 and 40 in the sea-ice region. These virus concentrations and VBRs indicate that viruses are no less important in Southern Ocean ecosystems than elsewhere in the world's oceans.


1991 ◽  
Vol 36 (2) ◽  
pp. 219-234 ◽  
Author(s):  
Gary L. Fahnenstiel ◽  
Hunter J. Carrick ◽  
Rodolfo Iturriaga

Ecology ◽  
1995 ◽  
Vol 76 (8) ◽  
pp. 2361-2372 ◽  
Author(s):  
Timothy B. Mihuc ◽  
G. Wayne Minshall
Keyword(s):  
Food Web ◽  

2018 ◽  
Vol 50 (1) ◽  
pp. S100016 ◽  
Author(s):  
Heather L. Mariash ◽  
Matteo Cazzanelli ◽  
Milla Rautio ◽  
Ladislav Hamerlik ◽  
Matthew J. Wooller ◽  
...  

Ecography ◽  
2009 ◽  
Vol 32 (2) ◽  
pp. 354-368 ◽  
Author(s):  
Candan U. Soykan ◽  
John L. Sabo
Keyword(s):  
Food Web ◽  

Author(s):  
Andrew Cohen ◽  
Pieter Verburg ◽  
Robert Hecky ◽  
Catherine O'Reilly ◽  
Pierre-Denis Plisnier

2011 ◽  
Vol 8 (11) ◽  
pp. 3283-3294 ◽  
Author(s):  
J. Esperschütz ◽  
A. Pérez-de-Mora ◽  
K. Schreiner ◽  
G. Welzl ◽  
F. Buegger ◽  
...  

Abstract. Microbial food webs are critical for efficient nutrient turnover providing the basis for functional and stable ecosystems. However, the successional development of such microbial food webs and their role in "young" ecosystems is unclear. Due to a continuous glacier retreat since the middle of the 19th century, glacier forefields have expanded offering an excellent opportunity to study food web dynamics in soils at different developmental stages. In the present study, litter degradation and the corresponding C fluxes into microbial communities were investigated along the forefield of the Damma glacier (Switzerland). 13C-enriched litter of the pioneering plant Leucanthemopsis alpina (L.) Heywood was incorporated into the soil at sites that have been free from ice for approximately 10, 60, 100 and more than 700 years. The structure and function of microbial communities were identified by 13C analysis of phospholipid fatty acids (PLFA) and phospholipid ether lipids (PLEL). Results showed increasing microbial diversity and biomass, and enhanced proliferation of bacterial groups as ecosystem development progressed. Initially, litter decomposition proceeded faster at the more developed sites, but at the end of the experiment loss of litter mass was similar at all sites, once the more easily-degradable litter fraction was processed. As a result incorporation of 13C into microbial biomass was more evident during the first weeks of litter decomposition. 13C enrichments of both PLEL and PLFA biomarkers following litter incorporation were observed at all sites, suggesting similar microbial foodwebs at all stages of soil development. Nonetheless, the contribution of bacteria, especially actinomycetes to litter turnover became more pronounced as soil age increased in detriment of archaea, fungi and protozoa, more prominent in recently deglaciated terrain.


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