Ocean acidification and viral replication cycles: Frequency of lytically infected and lysogenic cells during a mesocosm experiment in the NW Mediterranean Sea

2017 ◽  
Vol 186 ◽  
pp. 139-151 ◽  
Author(s):  
Anastasia Tsiola ◽  
Paraskevi Pitta ◽  
Antonia Giannakourou ◽  
Guillaume Bourdin ◽  
Sophie Marro ◽  
...  
Keyword(s):  
Viral Replication ◽  
Ocean Acidification ◽  
Mediterranean Sea ◽  
Mesocosm Experiment ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Copepod response to ocean acidification in a low nutrient-low chlorophyll environment in the NW Mediterranean Sea

2017 ◽  
Vol 186 ◽  
pp. 152-162 ◽  
Author(s):  
S. Zervoudaki ◽  
E. Krasakopoulou ◽  
T. Moutsopoulos ◽  
M. Protopapa ◽  
S. Marro ◽  
...  
Keyword(s):  
Ocean Acidification ◽  
Mediterranean Sea ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

scholarly journals Concomitant ocean acidification and increasing total alkalinity at a coastal site in the NW Mediterranean Sea (2007-2015)

2016 ◽  
Author(s):  
Lydia Kapsenberg ◽  
Samir Alliouane ◽  
Frédéric Gazeau ◽  
Laure Mousseau ◽  
Jean-Pierre Gattuso
Keyword(s):  
Ocean Acidification ◽  
Mediterranean Sea ◽  
Dissolved Inorganic Carbon ◽  
Coastal Ocean ◽  
Total Alkalinity ◽  
Global Ocean ◽  
Coastal Zones ◽  
Carbonate Chemistry ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Abstract. Monitoring of global ocean change is necessary in coastal zones due to their physical and biological complexity. Here, we document changes in coastal carbonate chemistry at the coastal time-series station, Point B, in the NW Mediterranean Sea from 2007 through 2015 at 1 and 50 m. The rate of surface ocean acidification (−0.0028 ± 0.0003 units pHT yr−1) was faster-than-expected based on atmospheric carbon dioxide forcing alone. Changes in carbonate chemistry were predominantly driven by an increase in total dissolved inorganic carbon (CT, +2.97 ± 0.20 μmol kg−1 yr−1), > 50 % of which was buffered by a synchronous increase in total alkalinity (AT, +2.08 ± 0.19 μmol kg−1 yr−1). The increase in AT was unrelated to salinity and its cause remains to be identified. Interestingly, concurrent increases in AT and CT were most rapid from May to July. Changes at 50 m were slower compared to 1 m. It seems therefore likely that changes in coastal AT cycling via a shallow coastal process gave rise to these observations. This study exemplifies the importance of understanding coastal ocean acidification through localized biogeochemical cycling that extends beyond simple air-sea gas exchange dynamics, in order to make relevant predictions about future coastal ocean change and ecosystem function.

Impact of ocean acidification on the biogeochemistry and meiofaunal assemblage of carbonate-rich sediments: Results from core incubations (Bay of Villefranche, NW Mediterranean Sea)

2018 ◽  
Vol 203 ◽  
pp. 102-119 ◽  
Author(s):  
Jens Rassmann ◽  
Bruno Lansard ◽  
Frédéric Gazeau ◽  
Laurence Guidi-Guilvard ◽  
Lara Pozzato ◽  
...  
Keyword(s):  
Ocean Acidification ◽  
Mediterranean Sea ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

scholarly journals Effects of Saharan dust on the microbial community during a large in situ mesocosm experiment in the NW Mediterranean Sea

2011 ◽  
Vol 62 (2) ◽  
pp. 201-213 ◽  
Author(s):  
M Laghdass ◽  
S Blain ◽  
M Besseling ◽  
P Catala ◽  
C Guieu ◽  
...  
Keyword(s):  
Microbial Community ◽  
Mediterranean Sea ◽  
Mesocosm Experiment ◽  
Saharan Dust ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Main drivers of spatial change in the biomass of commercial species between summer and winter in the NW Mediterranean Sea

2020 ◽  
pp. 105227
Author(s):  
Elena Lloret-Lloret ◽  
Maria Grazia Pennino ◽  
Daniel Vilas ◽  
José María Bellido ◽  
Joan Navarro ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Spatial Change ◽  
Commercial Species ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea
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