Patterns of wide-scale substitution within meadows of the seagrass Posidonia oceanica in NW Mediterranean Sea: invaders are stronger than natives

2010 ◽  
Vol 20 (5) ◽  
pp. 507-515 ◽  
Author(s):  
Monica Montefalcone ◽  
Giancarlo Albertelli ◽  
Carla Morri ◽  
Carlo Nike Bianchi
Keyword(s):  
Mediterranean Sea ◽  
Posidonia Oceanica ◽  
Nw Mediterranean ◽  
Wide Scale ◽  
Nw Mediterranean Sea

scholarly journals Seagrass as major source of transparent exopolymer particles in the oligotrophic Mediterranean coast

2017 ◽  
Vol 14 (22) ◽  
pp. 5069-5075 ◽  
Author(s):  
Francesca Iuculano ◽  
Carlos Maria Duarte ◽  
Núria Marbà ◽  
Susana Agustí
Keyword(s):  
Mediterranean Sea ◽  
Leaf Litter ◽  
Coastal Waters ◽  
Posidonia Oceanica ◽  
Mediterranean Coast ◽  
Transparent Exopolymer Particles ◽  
Coastal Beach ◽  
Nw Mediterranean ◽  
The Mediterranean ◽  
Nw Mediterranean Sea

Abstract. The role of seagrass, Posidonia oceanica, meadows as a source of transparent exopolymer particles (TEPs) to Mediterranean coastal waters was tested by comparing the TEP dynamics in two adjacent coastal waters in the oligotrophic NW Mediterranean Sea, one characterized by oligotrophic open-sea waters and the other accumulating seagrass leaf litter, together with an experimental examination of TEP release by seagrass litter. TEP concentrations ranged from 4.6 to 90.6 µg XG (xanthan gum) Eq L−1, with mean (±SE) values of 38.7 (± 2.02) µg XG Eq L−1 in the site devoid of seagrass litter, whereas the coastal beach site accumulating leaf litter had > 10-fold mean TEP concentrations of 487.02 (± 72.8) µg XG Eq L−1. Experimental evaluation confirmed high rates of TEP production by P. oceanica litter, allowing calculations of the associated TEP yield. We demonstrated that P. oceanica is an important source of TEPs to the Mediterranean Sea, contributing an estimated 76 Gg C as TEPs annually. TEP release by P. oceanica seagrass explains the elevated TEP concentration relative to the low chlorophyll a concentration in the Mediterranean Sea.

scholarly journals Seagrass as major source of transparent exopolymer particles in the oligotrophic Mediterranean coast

2017 ◽  
Author(s):  
Francesca Iuculano ◽  
Carlos M. Duarte ◽  
Núria Marbà ◽  
Susana Augustí
Keyword(s):  
Mediterranean Sea ◽  
Leaf Litter ◽  
Coastal Waters ◽  
Posidonia Oceanica ◽  
Mediterranean Coast ◽  
Transparent Exopolymer Particles ◽  
Coastal Beach ◽  
Nw Mediterranean ◽  
The Mediterranean ◽  
Nw Mediterranean Sea

Abstract. The role of seagrass, Posidonia oceanica, meadows as a source of transparent exopolymer particles (TEP) to Mediterranean coastal waters was tested by comparing the TEP dynamics in two adjacent coastal waters in the oligotrophic NW Mediterranean Sea, one characterized by oligotrophic open-sea waters and the other accumulating seagrass leaf litter, together with an experimental examination of TEP release by seagrass litter. TEP concentrations ranged from 4.6 µg XG Eq L−1 to 90.6 µg XG Eq L−1, with mean (±SE) values of 38.7 (±2.02) µg XG Eq L−1 in the site devoid of seagrass litter, whereas the coastal beach site accumulating leaf litter had > 10-fold mean TEP concentrations of 487.02 (±72.8) µg XG Eq L−1 . Experimental evaluation confirmed high rates of TEP production by P. oceanica litter, allowing calculations of the associated TEP yield. We demonstrated that P. oceanica is an important source of TEP to the Mediterranean Sea, contributing an estimated 0.10 Tg C as TEP annually. TEP release by P. oceanica seagrass explains the elevated TEP concentration relative to the low chlorophyll a concentration in the Mediterranean Sea.

Substitution and phase shift within the Posidonia oceanica seagrass meadows of NW Mediterranean Sea

2007 ◽  
Vol 75 (1-2) ◽  
pp. 63-71 ◽  
Author(s):  
M. Montefalcone ◽  
C. Morri ◽  
A. Peirano ◽  
G. Albertelli ◽  
C.N. Bianchi
Keyword(s):  
Phase Shift ◽  
Mediterranean Sea ◽  
Posidonia Oceanica ◽  
Seagrass Meadows ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Nematodes as indicators of environmental quality in seagrass (Posidonia oceanica) meadows of the NW Mediterranean Sea

2012 ◽  
Vol 3 (1) ◽  
pp. 69-91 ◽  
Author(s):  
Valentina Losi ◽  
Monica Montefalcone ◽  
Mariapaola Moreno ◽  
Elisa Giovannetti ◽  
Luigi Gaozza ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
Environmental Quality ◽  
Posidonia Oceanica ◽  
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

Composition and provenance of terrigenous organic matter transported along submarine canyons in the Gulf of Lion (NW Mediterranean Sea)

2013 ◽  
Vol 118 ◽  
pp. 81-94 ◽  
Author(s):  
Catalina Pasqual ◽  
Miguel A. Goñi ◽  
Tommaso Tesi ◽  
Anna Sanchez-Vidal ◽  
Antoni Calafat ◽  
...  
Keyword(s):  
Organic Matter ◽  
Mediterranean Sea ◽  
Submarine Canyons ◽  
Terrigenous Organic Matter ◽  
Gulf Of Lion ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

7000 years of paleostorm activity in the NW Mediterranean Sea in response to Holocene climate events

2012 ◽  
Vol 77 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Pierre Sabatier ◽  
Laurent Dezileau ◽  
Christophe Colin ◽  
Louis Briqueu ◽  
Frédéric Bouchette ◽  
...  
Keyword(s):  
Mediterranean Sea ◽  
North Atlantic ◽  
Clay Mineralogy ◽  
Mediterranean Coast ◽  
Ice Age ◽  
Storm Activity ◽  
The North ◽  
Nw Mediterranean ◽  
The North Atlantic ◽  
Nw Mediterranean Sea

A high-resolution record of paleostorm events along the French Mediterranean coast over the past 7000 years was established from a lagoonal sediment core in the Gulf of Lions. Integrating grain size, faunal analysis, clay mineralogy and geochemistry data with a chronology derived from radiocarbon dating, we recorded seven periods of increased storm activity at 6300–6100, 5650–5400, 4400–4050, 3650–3200, 2800–2600, 1950–1400 and 400–50 cal yr BP (in the Little Ice Age). In contrast, our results show that the Medieval Climate Anomaly (1150–650 cal yr BP) was characterised by low storm activity.The evidence for high storm activity in the NW Mediterranean Sea is in agreement with the changes in coastal hydrodynamics observed over the Eastern North Atlantic and seems to correspond to Holocene cooling in the North Atlantic. Periods of low SSTs there may have led to a stronger meridional temperature gradient and a southward migration of the westerlies. We hypothesise that the increase in storm activity during Holocene cold events over the North Atlantic and Mediterranean regions was probably due to an increase in the thermal gradient that led to an enhanced lower tropospheric baroclinicity over a large Central Atlantic-European domain.

Transformation of PBDE mixtures during sediment transport and resuspension in marine environments (Gulf of Lion, NW Mediterranean Sea)

2012 ◽  
Vol 168 ◽  
pp. 87-95 ◽  
Author(s):  
Joan A. Salvadó ◽  
Joan O. Grimalt ◽  
Jordi F. López ◽  
Xavier Durrieu de Madron ◽  
Serge Heussner ◽  
...  
Keyword(s):  
Sediment Transport ◽  
Mediterranean Sea ◽  
Marine Environments ◽  
Gulf Of Lion ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea
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