Vertical crustal motion along the Mediterranean and Black Sea coast derived from ocean altimetry and tide gauge data

Tide gauge (TG) data along the northern Mediterranean and Black Sea coasts are compared to the sea-surface height (SSH) anomaly obtained from ocean altimetry (TOPEX/Poseidon and ERS-1/2) for a period of nine years (1993–2001). The TG measures the SSH relative to the ground whereas the altimetry does so with respect to the geocentric reference frame; therefore their difference would be in principle a vertical ground motion of the TG sites, though there are different error sources for this estimate as is discussed in the paper. In this study we estimate such vertical ground motion, for each TG site, from the slope of the SSH time series of the (non-seasonal) difference between the TG record and the altimetry measurement at a point closest to the TG. Where possible, these estimates are further compared with those derived from nearby continuous Global Positioning System (GPS) data series. These results on vertical ground motion along the Mediterranean and Black Sea coasts provide useful source data for studying, contrasting, and constraining tectonic models of the region. For example, in the eastern coast of the Adriatic Sea and in the western coast of Greece, a general subsidence is observed which may be related to the Adriatic lithosphere subducting beneath the Eurasian plate along the Dinarides fault.

New Mediterranean Biodiversity Records (June 2012)

The present work reports on the extended distribution of nineteen species in the Mediterranean. These are: Upeneus pori (Fish:Turkey), Bursatella leachii (Mollusca, Opisthobranchia: eastern coast of Spain), Sparisoma cretense (Fish: Ionian coast of Greece), Pseudobryopsis myura (Chlorophyta:Turkey), Aplysia dactylomela (Mollusca, Opisthobranchia: Karpathos island, and Kyklades Archipelago, Greece), Asparagopsis armata and Botryocladia madagascariensis (Rhodophyta: South Peloponnesos, Greece), Oxynotus centrina (Fish: Greece), Caulerpa racemosa var. cylindracea (Chlorophyta ), Stypopodium schimperi (Phaeophyta ) Siganus luridus and Stephanolepis diaspros (Fish) Percnon gibbesi (Decapoda, Brachyura) (Kyklades Archipelago, Greece), Cerithium scabridum (Mollusca, Prosobranchia: Anavissos: Greece) and Cerithium renovatum (Mollusca, Prosobranchia: N. Κriti), Cassiopea andromeda (Scyphomedusa: Rhodos Island, Greece), Abra tenuis (Mollusca Bivalvia: Vouliagmeni Lake, Greece) Lagocephalus lagocephalus (Fish: Calabrian coast, Italy) and Plocamopherus ocellatus (Mollusca, Opisthobranchia: İskenderun Bay, Turkey).

Una nueva rábita en la playa de Guardamar del Segura: la rábita de El Moncayo

Se publican las noticias que ha arrojado la excavación en 2004 de unos muros situados en la denominada playa de El Moncayo. Los hallazgos se sitúan a unos 3 kilómetros al Sur del casco urbano de Guardamar del Segura; a unos 135 m. en dirección Norte está la Torre del Descargador (torre almenara de los siglos IV/X y V/XI), a unos 3,5 kilómetros se localiza El Castillo de Guardamar (de los siglos VIII a.C. al XIX) y, un poco más al Norte, a unos 4 kilómetros, en las proximidades de la desembocadura del Segura, los oratorios o rábitas de las dunas de Guardamar. Se dan a conocer los restos arquitectónicos y cerámicos aparecidos en la excavación del 2004 que se interpretan como de restos del recinto de una rábita o mezquitilla (cuando se excave más se verá si está aislada o hay más edificios similares), se presentan unos apuntes al hilo de la orientación de la rábita de El Moncayo y un estudio de la moneda andalusí hallada en la excavación de El Moncayo (datables entre en 429/1037-8 y 433/1041-2).