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1 Parente, 1 30 N Ir P V 20 N A G Emerged land Terrigenous shelf and shallow basin Platform limestone Slope and basin above CCD Deep basin Active spreading ridge Oceanic subduction Thrust, fault 10 N Figure DR1 - Paleogeographic map for the Cenomanian-Turonian boundary interval, showing the location of the studied sections (A: southern Apennines Platform) and of other localities cited in the text (P - Pyrenees; Ir - Iberian range; V - Vergons; G - Gavrovo). Bari Napoli Rome N Pliocene-Quaternary terrigenous deposits Volcanoes and magmatic deposits. Ligurides and Sicilides internal units. Apulia carbonate platform units and related foredeep deposits Apennine carbonate platform and by-pass margins, and related foredeep deposits Molise-Sannio-Lagonegro pelagic basin and associated slopes, and related foredeep km 1 Main thrusts fronts Main faults Main buried thrusts Studied sections Figure DR2 - Schematic geological map of the southern Apennines (modified from Butler et al., 2004, AAPG Mem., vol. 82, pp ) with location of studied sections. 1 - Monte Coccovello, 2 - Monte Varchera, 3 - Raia del Pedale. The insert in the upper right corner gives the location of the area shown in the geological map.
2 Table DR1 Monte Coccovello (40 02'50''N; 15 42'24''E) Sample (m) δ 13 C δ 18 O P P P P P P 293 A P 293 b P 293 c P 293 e P 294 F P 294 e P 294 d P 294 c P 294 b P 294 a P 295 a P 296 B P 296 a P 297 F P 297 e P 297 d P 297 c P 297 b P 297 a P P P P P P P 304a P P P P P P P P P P P P P P P P P P P P P P P Parente, 2
3 Table DR1 Monte Coccovello (40 02'50''N; 15 42'24''E) Sample (m) δ 13 C δ 18 O P P P P P P P P P P P P P P P Parente, 3 Analytical details Monte Coccovello and Monte Varchera. About 2 3 mg of powder were obtained for each sample by microdrilling a polished slab under the binocular microscope, taking care to avoid cement-filled veins and cavities and larger bioclasts. A 0.8 mm bit was used for lime mudstones whereas a 0.5 mm bit was employed for the micritic matrix of bioclastic facies. Stable isotope analyses were performed at the Isotopen-labor of the Institut fü r Geologie, Mineralogie und Geophysik at the Ruhr University (Bochum). Approximately 0.5 mg of sample powder was heated for 18 h at 105 C. Samples were reacted online by individual acidic (H 3 PO 4 ) addition with a Finnigan Gas Bench II. Stable isotope ratios were measured with a Finnigan Delta S mass spectrometer. The results are reported in per mil (&) deviation from the Pee Dee Belemnite standard (VPDB). Precision (1σ), monitored by repeated analyses of international standards and of a laboratory standard, was 0.09 for carbon isotopes. Replicate measurements gave a reproducibility in the range of 0.1 for δ 13 C.
4 RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP Parente, 4
5 Parente, 5 RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP
6 Parente, 6 RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP
7 Parente, 7 RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP
8 Parente, 8 RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP RP
9 Parente, 9 RP RP RP RP RP RP RP RP RP RP RP RP RP Analytical details Raia del Pedale. Stable isotope analyses were performed at Oxford University. Powdered bulkcarbonate samples were reacted with orthophosphoric acid at 90 C. The resulting CO 2 was analysed by a VG Isogas Series II Prism mass spectrometer [Vacuum Generators (VG), Winsford, Cheshire] and results are reported in per mil ( ) deviation from the Pee Dee Belemnite standard (VPDB). Analytical reproducibility of carbon-isotope analyses of replicate standards (Carrara Marble) for the above process was less than 0.1.
10 Table DR3 Monte Varchera (40 12'45''N; 15 37'18''E) Sample (m) δ 13 C δ 18 O GF GF GF GF GF GF GF GF GF GF GF GF GF GF 20 B GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF GF Parente, 10
11 Parente, 11 M.Coccovello ä 13 C carb Raia del Pedale M. Varchera 100 ä 13 C carb end ä 13 C excursion L.O. P. dubia 50 L.O. C. fraasi 50 0m mwpg r/f onset CTB ä 13 C excursion F.O. C. fraasi ä 13 C carb Ostracod/miliolid mudstonewackestone Radiolitid floatstone Brecciated/laminated dolomites and laminated mudstone/wackestone with fenestrae and birdseyes Wackestone-floatstone with rudist fragments and finegrained echinoid debris 0m m w pg r/f 0m mwpg r/f Foraminiferal wackestonepackstone Bio/chemo-stratigraphic datum Dark-grey laminated mudstone-wackestone Subaerial exposure surface Thalassinoides burrows Figure DR3 - Sedimentologic logs and bio-chemostratigraphic correlation of the studied sections.
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