La Famiglia Tellinidae Blainville, 1814, nel Plio-Pleistocene dell’Europa meridionale, parte seconda:i generi Asbjornsenia Friele, 1886, Strigilla W. Turton, 1822, Bosemprella M. Huber, Langleit &amp; Kreipl, 2015, Fabulina Gray, 1851, Macomangulus Nordsieck, 1969, Oudardia Monterosato, 1884, Peronaea Poli, 1791, Peronidia Dall, 1900, Serratina Pallary, 1920, con descrizione di 3 nuove specie

Brunetti, M. Mauro; Bella, Giano Della

doi:10.53559/bollmalacol.2022.10

Cited by 1 publication

(2 citation statements)

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“…2018; Pimentel et al . 2021; Brunetti & Della Bella 2022a). Moreover, we modified the chronological attribution of some fossil sites according to recent biochronological evidence.…”

Section: Methodsmentioning

confidence: 99%

“…We revised the bivalve fossil lists in terms of species presence/absence and accounted for the most recent taxonomic and systematic attributions. Indeed, recent articles provided new clarification about bivalve nomenclature and taxonomy (Mikkelsen & Bieler 2003;La Perna & D'Abramo 2011;La Perna et al 2018;Pimentel et al 2021;Brunetti & Della Bella 2022a). Moreover, we modified the chronological attribution of some fossil sites according to recent biochronological evidence.…”

Section: Species-level Datasetmentioning

confidence: 99%

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Response of Mediterranean Sea bivalves to Pliocene–Pleistocene environmental changes

Mondanaro,

Dominici,

Danise

2024

Palaeontology

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The Mediterranean Sea is recognized as a hotspot of marine biodiversity. Analysing its past biodiversity can help in understanding species' response to climate change. We built a species‐level dataset of bivalve occurrences across the Zanclean–Calabrian interval, a time characterized by significant changes in climate, and by bivalve extinctions. The dataset includes more than 400 species distributed from the eastern to the western Mediterranean Sea. We measured changes in richness and turnover through time, for the entire dataset, and for different palaeoenvironments and combinations of tiering and feeding categories to test if specific environmental conditions and different lifestyles were correlated to species extinction or survival through time. We also compared niche breadth, geographical range size, and species abundance of extinct and extant species, to test which of these parameters potentially affected extinction risk. Our results confirm a loss of biodiversity between 3 Ma and the Early Pleistocene, although this loss was less intense and more gradual than previously estimated. We also found significant differences in niche breadth and geographical range size between extinct and extant species. Suspension feeders lost a higher proportion of species and suffered a higher reduction of geographical range compared to infaunal deposit feeders. Species loss was more protracted and higher on the shoreface than on the shelf, which is probably related to the reduction of shallow‐water vegetated environments and to the disaggregation of heterozoan carbonate ramp habitats with cooling and sea‐level drop at the onset of the northern hemisphere glaciation.

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“…2018; Pimentel et al . 2021; Brunetti & Della Bella 2022a). Moreover, we modified the chronological attribution of some fossil sites according to recent biochronological evidence.…”

Section: Methodsmentioning

confidence: 99%