2000
DOI: 10.1006/cres.2000.0201
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The Aptian–Albian of the Apulia Carbonate Platform (Gargano Promontory, southern Italy): evidence of palaeoceanographic and tectonic controls on the stratigraphic architecture of the platform margin

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Cited by 56 publications
(62 citation statements)
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“…(C) Location of the studied outcrops, projected on the geological map modified from Moisiu and Gurabardhi (2004). calciturbidites of mixed pelagic and benthic fauna (Skourtsis-Coroneou et al, 1995;Karakitsios, 2013) compose the Senonian limestones. In Italy, the Ionian Basin deposits of the Gargano promontory expose megabreccias attesting syn-sedimentary tectonics affecting the Apulian platform during Aptian-Albian (Bosellini et al, 1993(Bosellini et al, , 1999Borgomano, 2000;Graziano, 2000;Hairabian et al, 2014-in this volume). During the Late Cretaceous, base-of-slope deposits composed of carbonate breccias and bioclastic grainstones are reported during the Cenomanian and Coniacian-Maastrichtian (Monte San Angelo, Nevarra, Caramanica Formations) while the Turonian corresponds to a sedimentary hiatus in the basin, related to an emersion phase of the platform (Borgomano, 1987(Borgomano, , 2000.…”
Section: Introductionmentioning
confidence: 86%
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“…(C) Location of the studied outcrops, projected on the geological map modified from Moisiu and Gurabardhi (2004). calciturbidites of mixed pelagic and benthic fauna (Skourtsis-Coroneou et al, 1995;Karakitsios, 2013) compose the Senonian limestones. In Italy, the Ionian Basin deposits of the Gargano promontory expose megabreccias attesting syn-sedimentary tectonics affecting the Apulian platform during Aptian-Albian (Bosellini et al, 1993(Bosellini et al, , 1999Borgomano, 2000;Graziano, 2000;Hairabian et al, 2014-in this volume). During the Late Cretaceous, base-of-slope deposits composed of carbonate breccias and bioclastic grainstones are reported during the Cenomanian and Coniacian-Maastrichtian (Monte San Angelo, Nevarra, Caramanica Formations) while the Turonian corresponds to a sedimentary hiatus in the basin, related to an emersion phase of the platform (Borgomano, 1987(Borgomano, , 2000.…”
Section: Introductionmentioning
confidence: 86%
“…The latter exposes resedimented deposits that have been extensively studied by a number of authors in a small area, i.e. the Gargano promontory, exposing an example of a platform-to-basin relation (Borgomano, 1987(Borgomano, , 2000Bosellini et al, 1993Bosellini et al, , 1999Graziano, 2000Graziano, , 2001Hairabian et al, 2014-in this volume). In contrast, little information exists with regard to the sedimentary processes involved in the sedimentation of a thick succession of about 300 m of Upper Cretaceous deposits outcropping in Albania.…”
Section: Introductionmentioning
confidence: 99%
“…The Cretaceous pelagic succession across these areas consists of three superimposed stratigraphic units: Maiolica (Valanginian-early Aptian), Marne a Fucoidi (early Aptian-late Albian), and Scaglia (late Albian-Coniacian). Near the margin of the platform, the Mattinata Formation, rich in gravity-displaced deposits, laterally replaces the Maiolica (Bernoulli 1972;Bosellini et al 1993;Luciani & Cobianchi 1994;Cobianchi et al 1997;Graziano 2000). The Apulian Platform, during the Late Jurassic-Early Cretaceous interval, was a productive carbonate platform with the rim colonized by bioconstructors and the inner area characterized by typical peritidal environments.…”
Section: Geological and Stratigraphical Settingmentioning
confidence: 99%
“…On the other hand, lowstand carbonate platforms commonly correspond to a bottom massive thick bed (up to few tens-of-metres thickness), which is capped by a drowning surface (i.e., hardground) and/or evolves upwards to decimetre to metre thick retrograding strata and/or to basin marls (Bover-Arnal et al, 2009, 2011a, 2014 Caprinidae disappeared from the Tethyan and Atlantic regions at the boundary between the Early and Late Aptian (Masse, 1989;Skelton and Gili, 2012). Caprinid lithosomes of late Early Aptian age are rare in carbonate platform deposits formed on the northern margin of the Tethys (Skelton and Gili, 2012), but common in those of isolated central Tethyan platforms such as the Southern Apennines (D'Argenio et al, 1992;Masse et al, 1993;Carannante et al, 2009), Apulia (Masse, 1992;Graziano, 1999Graziano, , 2000Graziano, , 2013Luciani et al, 2006) and Adriatic…”
Section: Accepted Manuscriptmentioning
confidence: 99%