@article {Cameselle2014,
	title = {{Late Miocene sedimentary architecture of the Ebro Continental Margin (Western Mediterranean): implications to the Messinian Salinity Crisis}},
	journal = {International Journal of Earth Sciences},
	volume = {103},
	number = {2},
	year = {2014},
	pages = {423{\textendash}440},
	keywords = {Ebro, Erosion, Mediterranean, Messinian, Miocene, Sea level},
	issn = {1437-3254},
	doi = {10.1007/s00531-013-0966-5},
	url = {http://link.springer.com/10.1007/s00531-013-0966-5},
	author = {Cameselle, Alejandra L and Urgeles, R and De Mol, B and Camerlenghi, Angelo and Canning, Jason C}
}
@article {Cameselle2013,
	title = {{Late Miocene sedimentary architecture of the Ebro Continental Margin (Western Mediterranean): implications to the Messinian Salinity Crisis}},
	journal = {International Journal of Earth Sciences},
	volume = {103},
	number = {2},
	year = {2013},
	month = {nov},
	pages = {423{\textendash}440},
	abstract = {The Messinian Salinity Crisis (MSC) resulted from a significant multi-phase drop and subsequent reflooding of the Mediterranean Sea from 5.96 to 5.33 Ma. Well-developed drainage networks, characterized by step-like profiles and abrasion platforms, are associated to this event. The Ebro Continental Margin (Western Mediterranean) presents an additional complexity since the capture of the drainage of the adjacent subaerial Ebro Basin took place sometime prior to the Messinian stage. Using 3D seismic reflection data, this work provides new insights into the origin of the step-like profile of the Messinian erosional surface (MES) and timing of the capture of the subaerial Ebro Basin. The results obtained indicate a sedimentary-active continental slope and delta progradation during Middle-Late Miocene, in a normal regressive context associated to a pre-Messinian proto-Ebro River. The mature development attained by the Messinian Ebro River network during the MSC corroborates that the capture of the Ebro Basin occurred prior to the MSC. The configuration of the clinoforms below the MES suggests that deltaic sediments of the Messinian Paleo-Ebro River deposited during the Tortonian and initial Messinian sea-level drawdown. The MES formed at the top of the Tortonian Highstand, where a fluvial network was deeply carved, and in the topset region of the Messinian Falling Stage Systems Tract, where minor erosion occurred. Fluvial deposits are outstandingly preserved on the main valleys of the MES. Therefore, the step-like profile of the MES was not created during Zanclean inundation, but during the latest stages of the main Messinian sea-level fall and lowstand. {\textcopyright} 2013 Springer-Verlag Berlin Heidelberg.},
	keywords = {Ebro, Erosion, Mediterranean, Messinian, Miocene, Sea level},
	issn = {1437-3254},
	doi = {10.1007/s00531-013-0966-5},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84894260158\&partnerID=tZOtx3y1},
	author = {Cameselle, Alejandra L. and Urgeles, Roger and De Mol, Ben and Camerlenghi, Angelo and Canning, Jason C.}
}
@conference {Camerlenghi2010,
	title = {{A database on submarine landslides of the mediterranean sea}},
	booktitle = {Submarine Mass Movements and Their Consequences - 4th International Symposium},
	year = {2010},
	pages = {503{\textendash}513},
	publisher = {Kluwer Academic Publishers},
	organization = {Kluwer Academic Publishers},
	abstract = {Submarine landslides are ubiquitous along the continental margins of the Mediterranean basin and occur on tectonically-dominated margins as well as on passive margins and volcanic island flanks. Tectonically quiet zones seem to have the highest density of known events. Most landslides occur as long run-out distance debris flows, but slumps and deep-seated failures are also relatively common. In abyssal plains the distal product of massive failures is recorded as large megatur-bidites, while on volcanic islands the dominant failure type is flank-collapse with development of debris avalanches. Submarine landslides, excluding megaturbidites, appear to occur in all water depths between the coastline and about 2000 m. Most landslides occupy areas ranging from a few to about 600 km2 and volumes up to 220 km3. Abyssal plain megaturbidites can attain 60, 000 km2 and 1, 000 km3. The landslides headwall height are clustered around two modes: 0 to 40 m for relatively small landslides and 160 to 200 m for the largest ones. Most recorded submarine landslides are relatively young in age and several events appear to group near the Pleistocene to Holocene transition. {\textcopyright} Springer Science + Business Media B.V. 2010.},
	keywords = {Geohazard, Holocene, Mass wasting, Mediterranean, Megaturbidite, Pleistocene, Submarine landslide},
	isbn = {9789048130702},
	url = {http://www.scopus.com/inward/record.url?eid=2-s2.0-84903488503\&partnerID=tZOtx3y1},
	author = {Camerlenghi, A. and Urgeles, R. and Fantoni, L.}
}
