Middle Eocene seagrass facies from Apennine carbonate platforms (Italy).

Two stratigraphic sections located in the Latium-Abruzzi (Monte Porchio, Central Apennines, Central Italy) and in the Apulian carbonate platform (S. Cesarea-Torre Tiggiano, Salento, Southern Italy) were measured and sampled to document the sedimentological characteristic and the faunistic assemblages of Middle Eocene seagrass deposits. The faunistic assemblages are dominated by porcellaneous foraminifera Orbitolites , Alveolina, Idalina , Spiroloculina , Quinqueloculina , Triloculina and abundant hooked-shaped gypsinids, associated with hooked red algae and green algae Halimeda . Fabiania , rotaliids and textulariids as well as nummulitids are subordinated. The samples were assigned to Lutetian (SBZ13–16) according to the occurrence of Nummulites cf. lehneri , Alveolina ex. gr. elliptica , Idalina berthelini , Orbitolites complanatus , Slovenites decastroi and Medocia blayensis . At Santa Cesarea reticulate nummulites occur in association with Alveolina spp. and Halkyardia minima marking the lower Bartonian (SBZ17). Three main facies associations have been recognised: I) larger porcellaneous foraminiferal grainstones with orbitolitids and alveolinids deposited into high-energy shallow-water settings influenced by wave processes that reworked the sediments associated with a seagrass; II) grainstone to packstone with small porcellaneous foraminifera and abundant permanently-attached gypsinids deposited in a more protected (e.g., small embayment) in situ vegetated environment; III) bioclastic packstone with parautochthonous material reworked from the seagrass by rip currents and accumulated into rip channels in a slightly deeper environment. The biotic assemblages suggest that the depositional environment is consistent with tropical to subtropical vegetated environments within oligotrophic conditions. [ABSTRACT FROM AUTHOR]