Giuliano Ciampo

University of Naples Federico II

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Bjørg Stabell

University of Oslo

Jason R. Ali

Senckenberg Natural History Collections Dresden

Valentino Di Donato

University of Naples Federico II

Hirokazu Maekawa

Osaka Prefecture University

Yves Lagabrielle

Géosciences Rennes

Dietrich Heling

Lomonosov Moscow State University

P. Esposito

Hôpital Nord

G J Milner

University of Western Australia

Teruaki Ishii

Shizuoka University

Yulin Xu

Tsinghua University

Cooperative Institutions

University of Naples Federico II

Terra

University of Sannio

University of Palermo

Lamont-Doherty Earth Observatory

Istituto Nazionale di Geofisica e Vulcanologia

University of Milan

Istituto Nazionale di Fisica Nucleare, Sezione di Napoli

Federico II University Hospital

University of Hawaii System

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An integrated micropalaeontological approach applied to Late Pleistocene-Holocene palaeoclimatic and palaeoenvironmental changes (Gaeta Bay, Tyrrhenian Sea)

Geological Society London Special Publications (2000)

Filomena Ornella Amore Giuliano Ciampo Valentino Di Donato P. Esposito Elda Russo Ermolli

Abstract An integrated micropalaeontological approach has been used to characterize the last climatic cycle in the Tyrrhenian Sea. Three gravity cores, drilled in the Gaeta Bay continental shelf, have been analysed by means of quantitative methods applied to different taxonomic groups. In particular, calcareous nannofossils, planktonic Foraminifera, ostracods and palynomorphs have been studied to detect palaeoclimatic trends. The Last Glacial period has been identified in the lower part of two cores (C8 and C9), and an older cold period is represented in the lower part of the more proximal core (C5). The upper part of all the cores clearly records the Holocene period, whereas the Late Glacial period is not always easily detectable. Pollen seems to precede the Holocene climatic optimum. Climatic curves have been reconstructed for all the taxonomic groups and high-resolution palaeobathymetric reconstruction has been inferred on the basis of the ostracod assemblages.

10.1144/gsl.sp.2000.181.01.10

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Citations (17)

(Table 2) Percent distribution of calcareous nannofossils at ODP Hole 125-782A

Giuliano Ciampo

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Macroevolution

10.1594/pangaea.729511

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(Table 8) Percent distribution of calcareous nannofossils at ODP Hole 125-781A

Giuliano Ciampo

Table (database)

10.1594/pangaea.729517

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Citations (82)

(Table 1) Biostratigraphic and magnetostratigraphic events of ODP Hole 125-782A

Bjørg Stabell Jason R. Ali Giuliano Ciampo G J Milner Yujing Wang

Table (database)

Magnetostratigraphy

10.1594/pangaea.771113

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ODP Leg 125, Hole 782B - Well Logging Data

Zenodo (CERN European Organization for Nuclear Research) (2020)

Julian A. Pearce P. Fryer Laura B. Stokking Jason R. Ali Richard Arculus

Logging data are measurements of physical properties of the formation surrounding a borehole, acquired in situ after completion of coring (wireline logging) or during drilling (Logging-While-Drilling, LWD). The range of data (resistivity, gamma radiation, velocity, density, borehole images,…) in any hole depends on the scientific objectives and operational constraints.

10.5281/zenodo.3942304

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Late Miocene (CN9b Subzone) to Holocene Calcareous Nannofossils from the Western and Northwestern Pacific Ocean, Leg 125

Proceedings of the Ocean Drilling Program. Scientific results (1992)

Giuliano Ciampo

During Leg 125 of the Ocean Drilling Program, nine sites were drilled in the Mariana and Izu-Bonin areas.The sediments recovered range in age from early Pliocene to late Pleistocene in the Mariana Region and from middle Eocene to late Pleistocene in the Izu-Bonin region.This contribution concerns the biostratigraphic study of the latest Miocene (CN9b Subzone) to late Pleistocene interval.Aquantitative analysis of all calcareous nannofossil associations was conducted for the interval encompassing late Miocene to the top of the early Pliocene.Moreover, the genera Discoaster, Amaurolithus, and Ceratolithus were quantitatively investigated from the late Miocene to late Pliocene interval.Some bioevents were identified, and variations in the composition of assemblages were linked to climatic changes.

Neogene

10.2973/odp.proc.sr.125.141.1992

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Summary of results from Leg 125

P.B. Fryer J.A. Pearce L.B. Stokking J.R. Ali R.J. Arculus

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Tectono-sedimentary evolution of the Pliocene to Lower Pleistocene succession of the Apricena-Lesina-Poggio Imperiale quarrying district (western Gargano, southern Italy)

Italian Journal of Geosciences (2010)

Giulio Pavia Carlo Bertok Giuliano Ciampo Valentino Di Donato Luca Martire

The post-Miocene marine succession of the «Apricena horst» is described with the purpose to verify the chronostratigraphic constraints for the type-locality of the Pirro Nord Faunal Unit. The stratigraphic succession has been subdivided in four units bounded by ubiquitous unconformities with evidence of subaerial exposure.The two basal units (dated late Zanclean to at most early Piacenzian) are formally grouped in the Lago di Varano Fm. that on the whole consists of sediments ranging from lagoonal to circalittoral environments.Within the lowermost unit, a megabreccia is interpreted as the product of a tsunami event. The third unit, Gelasian in age, is informally cited as Calcari a Briozoi Fm. The last unit, the Lower Pleistocene Serracapriola Fm., consists of siliciclastic deltaic sediments and represents the closure of the marine cycle. Conspicuous lateral facies and thickness changes, and the frequency of unconformities are the consequence of an intense synsedimentary tectonic activity developed in the frame of the southern Apulia foredeep closure.In the study area, such activity is documented by two E-W trending normal faults which, during Zanclean and at least the earliest Gelasian, controlled the Pliocene horst-graben system of the Apricena-Poggio Imperiale area.

Horst

Siliciclastic

Early Pleistocene

Subaerial

10.3301/ijg.2009.11

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Citations (17)

ODP Leg 125, Hole 786B - Well Logging Data

Zenodo (CERN European Organization for Nuclear Research) (2020)

Julian A. Pearce P. Fryer Laura B. Stokking Jason R. Ali Richard Arculus

10.5281/zenodo.3942307

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