Persistent Organic Pollutants Burden, Trophic Magnification and Risk in a Pelagic Food Web from Coastal NW Mediterranean Sea

2021 ◽  
Author(s):  
Javier Castro-Jiménez ◽  
Daniela Bănaru ◽  
Chia-Ting Chen ◽  
Begoña Jiménez ◽  
Juan Muñoz-Arnanz ◽  
...  
Keyword(s):  
Food Web ◽  
Mediterranean Sea ◽  
Organic Pollutants ◽  
Persistent Organic Pollutants ◽  
Pelagic Food Web ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Food web structure and vulnerability of a deep-sea ecosystem in the NW Mediterranean Sea

2013 ◽  
Vol 75 ◽  
pp. 1-15 ◽  
Author(s):  
Samuele Tecchio ◽  
Marta Coll ◽  
Villy Christensen ◽  
Joan B. Company ◽  
Eva Ramírez-Llodra ◽  
...  
Keyword(s):  
Food Web ◽  
Mediterranean Sea ◽  
Deep Sea ◽  
Food Web Structure ◽  
Web Structure ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Decadal changes in a NW Mediterranean Sea food web in relation to fishing exploitation

2009 ◽  
Vol 220 (17) ◽  
pp. 2088-2102 ◽  
Author(s):  
Marta Coll ◽  
Isabel Palomera ◽  
Sergi Tudela
Keyword(s):  
Food Web ◽  
Mediterranean Sea ◽  
Nw Mediterranean ◽  
Nw Mediterranean Sea

Trophic transfer of persistent organic pollutants through a pelagic food web: The case of Lake Como (Northern Italy)

2018 ◽  
Vol 640-641 ◽  
pp. 98-106 ◽  
Author(s):  
Michela Mazzoni ◽  
Emanuela Boggio ◽  
Marina Manca ◽  
Roberta Piscia ◽  
Silvia Quadroni ◽  
...  
Keyword(s):  
Food Web ◽  
Organic Pollutants ◽  
Persistent Organic Pollutants ◽  
Trophic Transfer ◽  
Northern Italy ◽  
Pelagic Food Web

scholarly journals 210 Po and 210 Pb trophic transfer within the phytoplankton–zooplankton–anchovy/sardine food web: a case study from the Gulf of Lion (NW Mediterranean Sea)

2015 ◽  
Vol 143 ◽  
pp. 141-151 ◽  
Author(s):  
Emilie Strady ◽  
Mireille Harmelin-Vivien ◽  
Jean François Chiffoleau ◽  
Alain Veron ◽  
Jacek Tronczynski ◽  
...  
Keyword(s):  
Food Web ◽  
Mediterranean Sea ◽  
Trophic Transfer ◽  
Gulf Of Lion ◽  
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.

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