Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/3940| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Speranza, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.authorall | Satolli, S.; Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | en |
| dc.contributor.authorall | Mattioli, E.; Centre de Sciences de la Terre, Université Claude Bernard Lyon 1, Villeurbanne, France | en |
| dc.contributor.authorall | Calamita, F.; Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | en |
| dc.date.accessioned | 2008-07-08T08:10:57Z | en |
| dc.date.available | 2008-07-08T08:10:57Z | en |
| dc.date.issued | 2005 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/3940 | en |
| dc.description.abstract | The magnetic stratigraphy of the Maiolica and Calcari ad Aptici pelagic limestones is documented from four Umbro-Marchean land sections (Italy). The overall biostratigraphic age of the sampled strata encompasses the whole Kimmeridgian–Lower Aptian. The data were gathered from two new sections (Arcevia, Contessa) and by resampling more densely than in the past two additional classical sections (Bosso, Gorgo a Cerbara). A detailed record of the polarity chrons M21n-M14 and M9-M0 was derived, and no difference was observed with respect to the sequence of M polarity chrons inferred from oceanic magnetic anomalies. Barely measurable remanent magnetization from chron M14 to M10n at Contessa concurred with previous evidence from Bosso, indicating that the Maiolica from Umbria-Marche is characterized by a "recording gap" during chrons M14n to M11, possibly due to diagenetic magnetite dissolution related to the Late Valanginian carbon isotope event. At Arcevia and Bosso, the boundary between Maiolica and Calcari ad Aptici occurs at the top of chron M19n and in the upper part of chron M20n, respectively, showing that the onset of Maiolica sedimentation may be diachronous by 1.5–2 Myr along the Umbria-Marche domain. Arcevia is the most expanded Mid-Upper Tithonian land section documented so far. Here, the subchrons M20n-1 and M19n-1 are found to represent 3.2% and 10.1% in time of chrons M20n and M19n, respectively. Evidence is also provided for a reversal excursion occurring within the M20n-1 subchron. At Bosso, an excursion and a reversal excursion were found within chrons M16n and M16, respectively. | en |
| dc.language.iso | English | en |
| dc.publisher.name | AGU | en |
| dc.relation.ispartof | Journal of Geophysical Research | en |
| dc.relation.ispartofseries | / 110 (2005) | en |
| dc.subject | Umbria | en |
| dc.subject | Marche | en |
| dc.subject | Magnetic stratigraphy | en |
| dc.subject | Mesozoic | en |
| dc.subject | M polarity sequence | en |
| dc.subject | Maiolica | en |
| dc.title | Magnetic stratigraphy of Kimmeridgian-Aptian sections from Umbria-Marche (Italy): New details on the M polarity sequence | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | B12109 | en |
| dc.subject.INGV | 04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetism | en |
| dc.identifier.doi | 10.1029/2005JB003884 | en |
| dc.relation.references | Abdul Aziz, H., and C. G. Langereis (2004), Astronomical tuning and duration of three new subchrons (C5r.2r-1n, C5r.2r-2n and C5r.3r-1n) recorded in a middle Miocene continental sequence from NE Spain, in Timescales of the Paleomagnetic Field, Geophys. Monogr. Ser., vol. 145, edited by J. E. T. Channell et al., pp. 141–160, AGU, Washington, D. C. Alvarez, W., M. A. Arthur, A. G. Fisher, W. Lowrie, G. Napoleone, I. Premoli Silva, and W. Roggenthen (1977), Late Cretaceous-Paleocene geomagnetic reversal time scale: V. Type section in the pelagic limestone sequence at Gubbio, Italy, Geol. Soc. Am. Bull., 88, 383– 389. Baudin, F., P. Faraoni, A. Marini, and G. Pallini (1997), Organic matter characterisation of the ‘‘Faraoni Level’’ from northern Italy (Lessini Mountains and Trento Plateau): Comparison with that from Umbria- Marche Apennines, Palaeopelagos, 7, 41– 51. Baumgartner, P. O. (1987), Genesis of Jurassic Tethyan radiolarites—The example of Monte Nerone (Umbria-Marche Apennines), paper presented at the II International ‘‘Fossili, Evoluzione, Ambiente’’ Congr., Pergola, Italy. Baumgartner, P. O., L. O’Dogherty, S. Gorican, E. Urquhart, A. Pillevuit, and P. De Wever (Eds.) (1995), Middle Jurassic to Lower Cretaceous Radiolaria of Tethys: Occurrences, Systematics, Biochronology, Me´m. Ge´ol., 23, 1172 pp. Bornemann, A., U. Aschwer, and J. Mutterlose (2003), The impact of calcareous nannofossils on the pelagic carbonate accumulation across the Jurassic/Cretaceous boundary, Palaeogeogr. Palaeoclimatol. Palaeoecol., 199, 187–228. Bown, P. R., and M. K. E. Cooper (1998), Jurassic, in Calcareous Nannofossil Biostratigraphy, edited by P. R. Bown, pp. 34 – 54, Cambridge Univ. Press, New York. Bralower, T. J., S. Monechi, and H. R. Thierstein (1989), Calcareous nannofossil zonation of the Jurassic-Cretaceous boundary interval and correlation with the geomagnetic polarity timescale, Mar.Micropaleontol., 14, 153–235. Busson, G., D. Noe¨l, and A. Corne´e (1992), Les coccolithes en ‘‘boutons de manchette’’ et la gene`se des calcaires lithographiques du Jurassique supe´rieur, Rev. Paleobiol., 11, 255–271. Busson,G.,D.Noe¨l,D. Contini,A.-M.Mangin,A.Corne´e,andP.Hantzpergue (1993), Omnipre´sence de coccolithes dans des calcaires lagunaires du Jurassique moyen et supe´rieur de France, Bull. Cent. Rech. Explor. Prod. Elf Aquitaine, 17, 291– 301. Cecca, F., S. Cresta, G. Pallini, and M. Santantonio (1987), Il Giurassico di Monte Nerone (Appennino marchigiano, Italia Centrale): Biostratigrafia, litostratigrafia ed evoluzione paleogeografica, paper presented at the II International ‘‘Fossili, Evoluzione, Ambiente’’ Congress, Pergola, Italy. Cecca, F., G. Pallini, E. Erba, I. Premoli Silva, and R. Coccioni (1994a), Hauterivian-Barremian chronostratigraphy based on ammonites, nannofossils, planktonic foraminifera and magnetic chrons from the Mediterranean domain, Cretaceous Res., 15, 457– 467. Cecca, F., A. Marini, G. Pallini, F. Baudin, and V. Begouen (1994b), A guide-level of the uppermost Hauterivian (Lower Cretaceous) in the pelagic succession of the Umbria-Marche Apennines (central Italy): the Faraoni level, Riv. Ital. Paleontol. Stratigr., 99, 551– 568. Channell, J. E. T., and E. Erba (1992), Early Cretaceous polarity chrons CM0 to CM11 recorded in northern Italian land sections near Brescia, Earth Planet. Sci. Lett., 108, 161– 179. Channell, J. E. T., and P. Grandesso (1987), A revised correlation of Mesozoic polarity chrons and calpionellid zones, Earth Planet. Sci. Lett., 85, 222–240. Channell, J. E. T., and C. McCabe (1994), Comparison of magnetic hysteresis parameters of unremagnetized and remagnetized limestones, J. Geophys. Res., 99, 4613– 4623. Channell, J. E. T., W. Lowrie, and F. Medizza (1979), Middle and Early Cretaceous magnetic stratigraphy from the Cismon section, northern Italy, Earth Planet. Sci. Lett., 42, 133– 166. Channell, J. E. T., W. Lowrie, P. Pialli, and F. Venturi (1984), Jurassic magnetic stratigraphy from Umbrian (Italian) land sections, Earth Planet. Sci. Lett., 68, 309–325. Channell, J. E. T., T. J. Bralower, and P. Grandesso (1987), Biostratigraphic correlation of Mesozoic polarity chrons CM1 to CM23 at Capriolo and Xausa (Southern Alps, Italy), Earth Planet. Sci. Lett., 85, 203– 221. Channell, J. E. T., E. Erba, and A. Lini (1993), Magnetostratigraphic calibration of the Late Valanginian carbon isotope event in pelagic limestones from northern Italy and Switzerland, Earth Planet. Sci. Lett., 118, 145–166. Channell, J. E. T., F. Cecca, and E. Erba (1995a), Correlation of Hauterivian and Barremian (Early Cretaceous) stage boundaries to polarity chrons, Earth Planet. Sci. Lett., 134, 125– 140. Channell, J. E. T., E. Erba, M. Nakanishi, and K. Tamaki (1995b), Late Jurassic-Early Cretaceous time scales and oceanic magnetic anomaly block models, in Geochronology Time Scales and Global Stratigraphic Correlation, SEPM Spec. Publ., 54, 51– 63. Channell, J. E. T., E. Erba, G. Muttoni, and F. Tremolada (2000), Early Cretaceous magnetic stratigraphy in the APTICORE drill core and adjacent outcrop at Cismon (Southern Alps, Italy), and correlation to the proposed Barremian-Aptian boundary stratotype, Geol. Soc. Am. Bull., 112, 1430–1443. Cirilli, S., P. Marton, and L. Vigliotti (1984), Implications of a combined biostratigraphic and palaeomagnetic study of the Umbrian Maiolica Formation, Earth Planet. Sci. Lett., 69, 203– 214. Coccioni, R., E. Erba, and I. Premoli-Silva (1992), Barremian-Aptian calcareous plankton biostratigraphy from the Gorgo a Cerbara section (Marche, central Italy) and implications for plankton evolution, Cretaceous Res., 13, 517–537. Consiglio Nazionale delle Ricerche (1991), Progetto finalizzato geodinamica. structural model of Italy map, scale 1:500,000, edited by G. Bigi et al., Rome. Galbrun, B. (1985), Magnetostratigraphy of the Berriasian stratotype section (Berrias, France), Earth Planet. Sci. Lett., 74, 130– 136. Giraud, F., S. Renaud, B. Pittet, E. Mattioli, and V. Audouin (2003), Variations de la morphologie et de l’abondance chez Watznaueria britannica (coccolithophoride´s) en relation avec les parame`tres pale´oenvironnementaux au Jurassique, paper presented at 3e`me Symposium de Morphome´trie et e´volution des formes, Groupement de Rech., Cent. de la Natl. Rech. Sci., Paris, 13 and 14 March. Gradstein, F. M., F. P. Agterberg, J. G. Ogg, J. Hardenbol, P. van Veen, J. Thierry, and Z. Huang (1994), A Mesozoic time scale, J. Geophys. Res., 99, 24,051– 24,074. Gradstein, F. M., et al. (2005), A Geologic Time Scale 2004, 610 pp., Cambridge Univ. Press, New York. Hay, W. W. (1972), Probabilistic stratigraphy, Eclogae Geol. Helv., 65, 255– 266. Housa, V., M. Krs, M. Krsova, O. Man, P. Pruner, and D. Venhodova (1999), High-resolution magnetostratigraphy and micropalaeontology across the J/K boundary strata at Brodno near Zilina, western Slovakia: summary of results, Cretaceous Res., 20, 699–717. Housa, V., M. Krs, O. Man, P. Pruner, D. Venhodova, F. Cecca, G. Nardi, and M. Piscitello (2004), Combined magnetostratigraphic, palaeomagnetic and calpionellid investigations across Jurassic/Cretaceous boundary strata in the Bosso Valley, Umbria, central Italy, Cretaceous Res., 25, 771– 785. Istituto Nazionale di Geofisica e Vulcanologia (2001), Italian Magnetic Network and Geomagnetic field maps of Italy at year 2000.0, Boll. Geod. Sci. Affini, 60. Kirschvink, J. L. (1980), The least-square line and plane and the analysis of paleomagnetic data, Geophys. J. R. Astron. Soc., 62, 699–718. Lees, J. A., P. R. Bown, J. R. Young, and J. B. Riding (2004), Evidence for annual records of phytoplankton productivity in the Kimmeridge Clay Formation coccolith stone bands (Upper Jurassic, Dorset, UK), Mar. Micropaleontol., 52, 29– 49. Lowrie, W., and W. Alvarez (1984), Lower Cretaceous magnetic stratigraphy in Umbrian pelagic limestone sections, Earth Planet. Sci. Lett., 71, 315– 328. Lowrie, W., and J. E. T. Channell (1984), Magnetostratigraphy of the Jurassic-Cretaceous boundary in the Maiolica limestone (Umbria, Italy), Geology, 12, 44–47. Lowrie, W., W. Alvarez, I. Premoli Silva, and S. Monechi (1980), Lower Cretaceous magnetic stratigraphy in Umbrian pelagic carbonate rocks, Geophys. J. R. Astron. Soc., 60, 263– 281. Lowrie, W., W. Alvarez, G. Napoleone, K. Perch-Nielsen, I. Premoli Silva, and M. Toumarkine (1982), Paleogene magnetic stratigraphy in Umbrian pelagic carbonate rocks: The Contessa sections, Gubbio, Geol. Soc. Am. Bull., 93, 414–432. McFadden, P. L., and M. W. McElhinny (1990), Classification of the reversal test in palaeomagnetism, Geophys. J. Int., 103, 725– 729. Micarelli, A., M. Potetti, and M. Chiocchini (1977), Ricerche microbiostratigrafiche sulla Maiolica della regione umbro-marchigiana, Stud. Geol. Camerti, 3, 57– 86. Morettini, E., M. Santantonio, A. Bartolini, F. Cecca, P. O. Baumgartner, and J. C. Hunziker (2002), Carbon isotope stratigraphy and carbonate production during the Early-Middle Jurassic: examples from the Umbria- Marche-Sabina Apennines (central Italy), Palaeogeogr. Palaeoclimatol. Palaeoecol., 184, 251– 273. Ogg, J. G. (1981), Sedimentology and paleomagnetism of Jurassic pelagic limestones: ‘‘Ammonitico Rosso’’ facies, Ph.D. thesis, 212 pp., Scripps Inst. of Oceanogr., Univ. of Calif., San Diego. Ogg, J. G., M. B. Steiner, F. Oloriz, and J. M. Tavera (1984), Jurassic magnetostratigraphy, 1. Kimmeridgian-Tithonian of Sierra Gorda and Carcabuey, southern Spain, Earth Planet. Sci. Lett., 71, 147–162. Ogg, J. G., M. B. Steiner, M. Company, and J. M. Tavera (1988), Magnetostratigraphy across the Berriasian-Valanginian stage boundary (Early Cretaceous), at Cehegin (Murcia Province, southern Spain), Earth Planet Sci. Lett., 87, 205– 215. Ogg, J. G., R. W. Hasenyager, W. A. Wimbledon, J. E. T. Channell, and T. J. Bralower (1991), Magnetostratigraphy of the Jurassic-Cretaceous boundary interval-Tethyan and English faunal realms, Cretaceous Res., 12, 455– 482. Olivier, N., B. Pittet, and E. Mattioli (2004), Palaeoenvironmental control on sponge-reefs and contemporaneous deep-shelf marl-limestone deposition (Late Oxfordian, southern Germany), Palaeogeogr. Palaeoclimatol. Palaeoecol., 212, 233–263. Opdyke, N. D., and J. E. T. Channell (1996), Magnetic Stratigraphy, Int. Geophys. Ser., vol. 64, 346 pp., Elsevier, New York. Pittet, B., and E. Mattioli (2002), The carbonate signal and calcareous nannofossil distribution in an Upper Jurassic section (Balingen-Tieringen, Late Oxfordian, southern Germany), Paleogeogeogr. Paleoclimatol. Paleoecol., 179, 71– 96. Roth, P. H. (1984), Preservation of calcareous nannofossils and fine-grained carbonate particles in Mid-Cretaceous sediments from the southern Angola Basin, Initial Rep. Deep Sea Drill. Proj., 75, 651– 655. Santantonio, M. (1993), Facies association and evolution of pelagic carbonate platform/basin systems: Examples from the Italian Jurassic, Sedimentology, 40, 1039– 1067. Tarduno, J. A., W. Lowrie, W. V. Sliter, T. J. Bralower, and F. Heller (1992), Reversed polarity characteristic magnetizations in the Albian Contessa sections, Umbrian Apennines, Italy: Implications for the existence of a Mid-Cretaceous mixed polarity interval, J. Geophys. Res., 97, 241– 271. Tribovillard, N. P., G. Gorin, S. Belin, G. Hopfgartner, and R. Pichon (1992), Organic-rich biolaminated facies from a Kimmeridgian lagoonal environment in the French Southern Jura mountains: Away of estimating accumulation rate variations, Palaeogeogr. Palaeoclimatol. Palaeoeco., 99, 163– 177. Williams, J. R., and T. J. Bralower (1995), Nannofossil assemblage, fine fraction stable isotopes, and the paleoceanography of the Valanginian- Barremian (Early Cretaceous) North Sea Basin, Paleoceanography, 10, 815– 839. Zijderveld, J. D. A. (1967), AC demagnetization of rocks: Analysis of results, in Methods in Palaeomagnetism, edited by S. K. Runcorn, K. M. Creer, and D. W. Collinson, pp. 254– 286, Elsevier, New York. | en |
| dc.description.obiettivoSpecifico | 2.2. Laboratorio di paleomagnetismo | en |
| dc.description.journalType | JCR Journal | en |
| dc.description.fulltext | reserved | en |
| dc.contributor.author | Speranza, F. | en |
| dc.contributor.author | Satolli, S. | en |
| dc.contributor.author | Mattioli, E. | en |
| dc.contributor.author | Calamita, F. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
| dc.contributor.department | Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | en |
| dc.contributor.department | Centre de Sciences de la Terre, Université Claude Bernard Lyon 1, Villeurbanne, France | en |
| dc.contributor.department | Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | restricted | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
| crisitem.author.dept | Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | - |
| crisitem.author.dept | Centre de Sciences de la Terre, Université Claude Bernard Lyon 1, Villeurbanne, France | - |
| crisitem.author.dept | Dipartimento di Scienze della Terra, Università di Chieti, Chieti, Italy | - |
| crisitem.author.orcid | 0000-0001-5492-8670 | - |
| crisitem.author.orcid | 0000-0002-1966-3061 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
Files in This Item:
| File | Description | Size | Format | Existing users please Login |
|---|---|---|---|---|
| 2005JB003884.pdf | 2.92 MB | Adobe PDF |
WEB OF SCIENCETM
Citations
50
36
checked on Feb 10, 2021
Page view(s) 50
154
checked on Apr 20, 2024
Download(s)
28
checked on Apr 20, 2024
