Biomineralization of iron-phosphates in the water column of Lake Pavin (Massif Central, France)

2014 ◽  
Vol 126 ◽  
pp. 78-96 ◽  
Author(s):  
Julie Cosmidis ◽  
Karim Benzerara ◽  
Guillaume Morin ◽  
Vincent Busigny ◽  
Oanez Lebeau ◽  
...  
2009 ◽  
Vol 266 (3-4) ◽  
pp. 311-317 ◽  
Author(s):  
Elvira Bura-Nakić ◽  
Eric Viollier ◽  
Didier Jézéquel ◽  
Alassane Thiam ◽  
Irena Ciglenečki

2010 ◽  
Vol 192 (7) ◽  
pp. 559-567 ◽  
Author(s):  
Guillaume Borrel ◽  
Anne-Catherine Lehours ◽  
Corinne Bardot ◽  
Xavier Bailly ◽  
Gérard Fonty

2018 ◽  
Vol 497 ◽  
pp. 218-233 ◽  
Author(s):  
Léo Chassiot ◽  
Yannick Miras ◽  
Emmanuel Chapron ◽  
Anne-Lise Develle ◽  
Fabien Arnaud ◽  
...  

2005 ◽  
Vol 71 (10) ◽  
pp. 5935-5942 ◽  
Author(s):  
Marie Lefranc ◽  
Aurélie Thénot ◽  
Cécile Lepère ◽  
Didier Debroas

ABSTRACT Small eukaryotes, cells with a diameter of less than 5 μm, are fundamental components of lacustrine planktonic systems. In this study, small-eukaryote diversity was determined by sequencing cloned 18S rRNA genes in three libraries from lakes of differing trophic status in the Massif Central, France: the oligotrophic Lake Godivelle, the oligomesotrophic Lake Pavin, and the eutrophic Lake Aydat. This analysis shows that the least diversified library was in the eutrophic lake (12 operational taxonomic units [OTUs]) and the most diversified was in the oligomesotrophic lake (26 OTUs). Certain groups were present in at least two ecosystems, while the others were specific to one lake on the sampling date. Cryptophyta, Chrysophyceae, and the strictly heterotrophic eukaryotes, Ciliophora and fungi, were identified in the three libraries. Among the small eukaryotes found only in two lakes, Choanoflagellida and environmental sequences (LKM11) were not detected in the eutrophic system whereas Cercozoa were confined to the oligomesotrophic and eutrophic lakes. Three OTUs, linked to the Perkinsozoa, were detected only in the Aydat library, where they represented 60% of the clones of the library. Chlorophyta and Haptophyta lineages were represented by a single clone and were present only in Godivelle and Pavin, respectively. Of the 127 clones studied, classical pigmented organisms (autotrophs and mixotrophs) represented only a low proportion regardless of the library's origin. This study shows that the small-eukaryote community composition may differ as a function of trophic status; certain lineages could be detected only in a single ecosystem.


2010 ◽  
Vol 10 (9) ◽  
pp. 1815-1827 ◽  
Author(s):  
E. Chapron ◽  
P. Albéric ◽  
D. Jézéquel ◽  
W. Versteeg ◽  
J.-L. Bourdier ◽  
...  

Abstract. Sedimentation processes occurring in the most recent maar lake of the French Massif Central (Lake Pavin) are documented for the first time based on high resolution seismic reflection and multibeam bathymetric surveys and by piston coring and radiocarbon dating on a sediment depocentre developed on a narrow sub aquatic plateau. This new data set confirms the mid Holocene age of maar lake Pavin formation at 6970±60 yrs cal BP and highlights a wide range of gravity reworking phenomena affecting the basin. In particular, a slump deposit dated between AD 580–640 remoulded both mid-Holocene lacustrine sediments, terrestrial plant debris and some volcanic material from the northern crater inner walls. Between AD 1200 and AD 1300, a large slide scar mapped at 50 m depth also affected the southern edge of the sub aquatic plateau, suggesting that these gas-rich biogenic sediments (laminated diatomite) are poorly stable. Although several triggering mechanisms can be proposed for these prehistoric sub-aquatic mass wasting deposits in Lake Pavin, we argue that such large remobilisation of gas-rich sediments may affect the gas stability in deep waters of meromictic maar lakes. This study highlights the need to further document mass wasting processes in maar lakes and their impacts on the generation of waves, favouring the development of dangerous (and potentially deadly) limnic eruptions.


Geomorphology ◽  
2021 ◽  
Vol 382 ◽  
pp. 107663
Author(s):  
J.-C. Thouret ◽  
P. Boivin ◽  
D. Miallier ◽  
F. Donnadieu ◽  
J.-P. Dumoulin ◽  
...  

2022 ◽  
Vol 12 ◽  
Author(s):  
Cécile C. Bidaud ◽  
Caroline L. Monteil ◽  
Nicolas Menguy ◽  
Vincent Busigny ◽  
Didier Jézéquel ◽  
...  

Magnetotactic bacteria (MTB) are microorganisms thriving mostly at oxic–anoxic boundaries of aquatic habitats. MTB are efficient in biomineralising or sequestering diverse elements intracellularly, which makes them potentially important actors in biogeochemical cycles. Lake Pavin is a unique aqueous system populated by a wide diversity of MTB with two communities harbouring the capability to sequester not only iron under the form of magnetosomes but also phosphorus and magnesium under the form of polyphosphates, or calcium carbonates, respectively. MTB thrive in the water column of Lake Pavin over a few metres along strong redox and chemical gradients representing a series of different microenvironments. In this study, we investigate the relative abundance and the vertical stratification of the diverse populations of MTB in relation to environmental parameters, by using a new method coupling a precise sampling for geochemical analyses, MTB morphotype description, and in situ measurement of the physicochemical parameters. We assess the ultrastructure of MTB as a function of depth using light and electron microscopy. We evidence the biogeochemical niche of magnetotactic cocci, capable of sequestering large PolyP inclusions below the oxic–anoxic transition zone. Our results suggest a tight link between the S and P metabolisms of these bacteria and pave the way to better understand the implication of MTB for the P cycle in stratified environmental conditions.


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