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250 Million Years of Earth History in Central Italy: Celebrating 25 Years of the Geological Observatory of Coldigioco

Contents Preface............................................................................ v 1.... more Contents Preface............................................................................ v 1. Cenozoic mass extinctions in the deep sea: What perturbs the largest habitat on Earth?......... 1 Ellen Thomas 2. A major Pliocene coccolithophore turnover: Change in morphological strategy in the photic zone..................... ...

13th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 26–29 August 2013, 2013

A new planktonic foraminiferal species, Hedbergella rhinoceros, from the Late Aptian to the Early... more A new planktonic foraminiferal species, Hedbergella rhinoceros, from the Late Aptian to the Early Albian sediments of the Marne a Fucoidi formation (Umbro —Marchean Apennines, central Italy) is described and illustrated

Journal of Geophysical Research, 2019

Data sets include the osmium and carbon isotopic information of the limestone samples collected f... more Data sets include the osmium and carbon isotopic information of the limestone samples collected from the Fiume Bosso section (43°31'07.2N 12°34'15.4E), central Italy. Os and carbon isotopic measurements were conducted from December 2019 to October 2020 to reconstruct paleo-marine Os and carbon isotopic variations. Os isotopic ratios were measured with thermal ionization mass spectrometry (TRITON, Thermo Fisher Scientific, USA) and carbon isotopic ratio were measured with isotope ratio mass spectrometry (Delta V plus, Thermo Fisher Scientific, USA). Our data covers from the upper Hauterivian to the lower Barremian of the Lower Cretaceous.

Data sets include the osmium and carbon isotopic information of the limestone samples collected f... more Data sets include the osmium and carbon isotopic information of the limestone samples collected from the Fiume Bosso section (43°31'07.2N 12°34'15.4E), central Italy. Os and carbon isotopic measurements were conducted from December 2019 to October 2020 to reconstruct paleo-marine Os and carbon isotopic variations. Os isotopic ratios were measured with thermal ionization mass spectrometry (TRITON, Thermo Fisher Scientific, USA) and carbon isotopic ratio were measured with isotope ratio mass spectrometry (Delta V plus, Thermo Fisher Scientific, USA). Our data covers from the upper Hauterivian to the lower Barremian of the Lower Cretaceous.

Micropaleontology

Three Paleocene-Eocene (P-E) stratigraphic transect sections namely, from the north to south, Ain... more Three Paleocene-Eocene (P-E) stratigraphic transect sections namely, from the north to south, Ain Maqfi, Farafra-Ain Dalla road, and El-Quess Abu Said in the northern Farafra Oasis,Western Desert (Egypt) are described and interpreted based upon field observations, microfacies analysis, chronostratigraphy and foraminiferal paleobathymetry, to detect the effect of the Syrian Arc Fold System (SAFS) on the lateral and vertical facies changes, various stratigraphic breaks and to reconstruct the depositional paleoenvironments. Lithostratigraphically, the P-E successions are composed of the upper part of the Dakhla Formation, Tarawan Chalk and Esna Shale Formation. Vertical and lateral facies changes are noted between tectonic paleo-highs and paleo-lows in the Farafra Oasis. Eight microfacies types are recognized. The larger benthic and planktonic foraminiferal zones are here used to correlate the shallow and deeper facies. Two larger benthic (SBZ4 and SBZ6), six planktonic foraminiferal (...

250 Million Years of Earth History in Central Italy: Celebrating 25 Years of the Geological Observatory of Coldigioco

Contents Preface............................................................................ v 1.... more Contents Preface............................................................................ v 1. Cenozoic mass extinctions in the deep sea: What perturbs the largest habitat on Earth?......... 1 Ellen Thomas 2. A major Pliocene coccolithophore turnover: Change in morphological strategy in the photic zone..................... ...

13th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 26–29 August 2013, 2013

A new planktonic foraminiferal species, Hedbergella rhinoceros, from the Late Aptian to the Early... more A new planktonic foraminiferal species, Hedbergella rhinoceros, from the Late Aptian to the Early Albian sediments of the Marne a Fucoidi formation (Umbro —Marchean Apennines, central Italy) is described and illustrated

Journal of Geophysical Research, 2019

Data sets include the osmium and carbon isotopic information of the limestone samples collected f... more Data sets include the osmium and carbon isotopic information of the limestone samples collected from the Fiume Bosso section (43°31'07.2N 12°34'15.4E), central Italy. Os and carbon isotopic measurements were conducted from December 2019 to October 2020 to reconstruct paleo-marine Os and carbon isotopic variations. Os isotopic ratios were measured with thermal ionization mass spectrometry (TRITON, Thermo Fisher Scientific, USA) and carbon isotopic ratio were measured with isotope ratio mass spectrometry (Delta V plus, Thermo Fisher Scientific, USA). Our data covers from the upper Hauterivian to the lower Barremian of the Lower Cretaceous.

Data sets include the osmium and carbon isotopic information of the limestone samples collected f... more Data sets include the osmium and carbon isotopic information of the limestone samples collected from the Fiume Bosso section (43°31'07.2N 12°34'15.4E), central Italy. Os and carbon isotopic measurements were conducted from December 2019 to October 2020 to reconstruct paleo-marine Os and carbon isotopic variations. Os isotopic ratios were measured with thermal ionization mass spectrometry (TRITON, Thermo Fisher Scientific, USA) and carbon isotopic ratio were measured with isotope ratio mass spectrometry (Delta V plus, Thermo Fisher Scientific, USA). Our data covers from the upper Hauterivian to the lower Barremian of the Lower Cretaceous.

Micropaleontology

Three Paleocene-Eocene (P-E) stratigraphic transect sections namely, from the north to south, Ain... more Three Paleocene-Eocene (P-E) stratigraphic transect sections namely, from the north to south, Ain Maqfi, Farafra-Ain Dalla road, and El-Quess Abu Said in the northern Farafra Oasis,Western Desert (Egypt) are described and interpreted based upon field observations, microfacies analysis, chronostratigraphy and foraminiferal paleobathymetry, to detect the effect of the Syrian Arc Fold System (SAFS) on the lateral and vertical facies changes, various stratigraphic breaks and to reconstruct the depositional paleoenvironments. Lithostratigraphically, the P-E successions are composed of the upper part of the Dakhla Formation, Tarawan Chalk and Esna Shale Formation. Vertical and lateral facies changes are noted between tectonic paleo-highs and paleo-lows in the Farafra Oasis. Eight microfacies types are recognized. The larger benthic and planktonic foraminiferal zones are here used to correlate the shallow and deeper facies. Two larger benthic (SBZ4 and SBZ6), six planktonic foraminiferal (...

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