The bottom samples (Quaternary in age) of two cores (CS1 and Caro1) collected at 60 and 122 m water depth in the marine area near Ponza Island (Pontine Archipelago, Tyrrhenian Sea) are investigated. In particular, benthic foraminifers and siliceous sponge spicules are considered. The coralline red algae (pralines, boxworks and unattached branches) are abundant in both samples and, particularly, in the CS1 bottom as well as the benthic foraminifers. The siliceous sponge spicules also are very diversified and abundant in the CS1 bottom sample, while in the Caro1 bottom they are rare and fragmented. Benthic foraminiferal assemblage of two samples is dominated by Asterigerinata mamilla and Lobatula lobatula, typical epiphytic species but also a...
Shell-rich biodetrital carbonate lithosomes punctuate the Plio-Pleistocene marine shallow-water succ...
The results of a multidisciplinary study conducted on the circali- ttoral soft bottom assemblages at...
This work focuses on the carbonate factories constituting the Pietra di Finale Fm cropping out in th...
The seabed of the Pontine Archipelago (Tyrrhenian Sea) insular shelf is peculiar as it is characteri...
Ponza Island is located in the western sector of the Pontine volcanic Archipelago, on a structural h...
The Tyrrhenian Sea is in the central part of the Mediterranean Sea between the mainland of Italy and...
The soft bottom of the Mediterranean continental shelf is characterized by a heterozoan skeletal ass...
Sedimentological and micropaleontological characterisation of bottom sediments from two Latium conti...
In the Mediterranean, build-ups (created by coralline algae, Cladocora caespitosa, deep-water corals...
In the Mediterranean, build-ups (created by coralline algae, Cladocora caespitosa, deep-water corals...
Sponges generally live firmly attached on firm-and hardgrounds but a few species are known to coloni...
Sponge assemblages associated with coralligenous outcrops were studied with the aim of describing an...
The Messinian Salinity Crisis (MSC) created a substantial negative impact on the Mediterranean marin...
During the Pliocene and Pleistocene, the Monte Cetona (Northern Apennines, central Italy) was part o...
The demosponge siliceous spicules, entrapped in the Mediterranean coralligenous bioherms, are a good...
Shell-rich biodetrital carbonate lithosomes punctuate the Plio-Pleistocene marine shallow-water succ...
The results of a multidisciplinary study conducted on the circali- ttoral soft bottom assemblages at...
This work focuses on the carbonate factories constituting the Pietra di Finale Fm cropping out in th...
The seabed of the Pontine Archipelago (Tyrrhenian Sea) insular shelf is peculiar as it is characteri...
Ponza Island is located in the western sector of the Pontine volcanic Archipelago, on a structural h...
The Tyrrhenian Sea is in the central part of the Mediterranean Sea between the mainland of Italy and...
The soft bottom of the Mediterranean continental shelf is characterized by a heterozoan skeletal ass...
Sedimentological and micropaleontological characterisation of bottom sediments from two Latium conti...
In the Mediterranean, build-ups (created by coralline algae, Cladocora caespitosa, deep-water corals...
In the Mediterranean, build-ups (created by coralline algae, Cladocora caespitosa, deep-water corals...
Sponges generally live firmly attached on firm-and hardgrounds but a few species are known to coloni...
Sponge assemblages associated with coralligenous outcrops were studied with the aim of describing an...
The Messinian Salinity Crisis (MSC) created a substantial negative impact on the Mediterranean marin...
During the Pliocene and Pleistocene, the Monte Cetona (Northern Apennines, central Italy) was part o...
The demosponge siliceous spicules, entrapped in the Mediterranean coralligenous bioherms, are a good...
Shell-rich biodetrital carbonate lithosomes punctuate the Plio-Pleistocene marine shallow-water succ...
The results of a multidisciplinary study conducted on the circali- ttoral soft bottom assemblages at...
This work focuses on the carbonate factories constituting the Pietra di Finale Fm cropping out in th...