Articles | Volume 3, issue 2
https://doi.org/10.5194/se-3-225-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-3-225-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Shallow water carbonate platforms (Late Aptian–Early Albian, Southern Apennines) in the context of supraregional to global changes: re-appraisal of palaeoecological events as reflectors of carbonate factory response
A. Raspini
Istituto di Geoscienze e Georisorse (IGG), CNR, Via Giorgio La Pira, 4, 50121, Firenze, Italy
Related subject area
Sedimentology
What does it take to restore geological models with “natural” boundary conditions?
Impact of stress regime change on the permeability of a naturally fractured carbonate buildup (Latemar, the Dolomites, northern Italy)
Fold localization at pre-existing normal faults: field observations and analogue modelling of the Achental structure, Northern Calcareous Alps, Austria
The influence of extraction of various solvents on chemical properties on Chang 7 shale, Ordos Basin, China
Deep vs. shallow – two contrasting theories? A tectonically activated Late Cretaceous deltaic system in the axial part of the Mid-Polish Trough: a case study from southeast Poland
Miocene high elevation in the Central Alps
What makes seep carbonates ignore self-sealing and grow vertically: the role of burrowing decapod crustaceans
Dawn and dusk of Late Cretaceous basin inversion in central Europe
Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam scanning electron microscopy imaging
Birth and closure of the Kallipetra Basin: Late Cretaceous reworking of the Jurassic Pelagonian–Axios/Vardar contact (northern Greece)
High-resolution analysis of the physicochemical characteristics of sandstone media at the lithofacies scale
Sediment history mirrors Pleistocene aridification in the Gobi Desert (Ejina Basin, NW China)
Tectonic processes, variations in sediment flux, and eustatic sea level recorded by the 20 Myr old Burdigalian transgression in the Swiss Molasse basin
Miocene basement exhumation in the Central Alps recorded by detrital garnet geochemistry in foreland basin deposits
Can anaerobic oxidation of methane prevent seafloor gas escape in a warming climate?
Fault-controlled dolomitization in the Montagna dei Fiori Anticline (Central Apennines, Italy): record of a dominantly pre-orogenic fluid migration
Precipitation of dolomite from seawater on a Carnian coastal plain (Dolomites, northern Italy): evidence from carbonate petrography and Sr isotopes
The Ogooue Fan (offshore Gabon): a modern example of deep-sea fan on a complex slope profile
Formation of linear planform chimneys controlled by preferential hydrocarbon leakage and anisotropic stresses in faulted fine-grained sediments, offshore Angola
From oil field to geothermal reservoir: assessment for geothermal utilization of two regionally extensive Devonian carbonate aquifers in Alberta, Canada
Sedimentary mechanisms of a modern banded iron formation on Milos Island, Greece
X-ray computed tomography investigation of structures in Opalinus Clay from large-scale to small-scale after mechanical testing
Porosity and permeability determination of organic-rich Posidonia shales based on 3-D analyses by FIB-SEM microscopy
4-D imaging of sub-second dynamics in pore-scale processes using real-time synchrotron X-ray tomography
X-ray CT analyses, models and numerical simulations: a comparison with petrophysical analyses in an experimental CO2 study
Syn-eruptive, soft-sediment deformation of deposits from dilute pyroclastic density current: triggers from granular shear, dynamic pore pressure, ballistic impacts and shock waves
Record of Early Toarcian carbon cycle perturbations in a nearshore environment: the Bascharage section (easternmost Paris Basin)
Phanerozoic environments of black shale deposition and the Wilson Cycle
Particle size distributions by laser diffraction: sensitivity of granular matter strength to analytical operating procedures
Melchior Schuh-Senlis, Guillaume Caumon, and Paul Cupillard
Solid Earth, 15, 945–964, https://doi.org/10.5194/se-15-945-2024, https://doi.org/10.5194/se-15-945-2024, 2024
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This paper presents the application of a numerical method for restoring models of the subsurface to a previous state in their deformation history, acting as a numerical time machine for geological structures. The method is applied to a model based on a laboratory experiment. The results show that using force conditions in the computation of the deformation allows us to assess the value of some previously unknown physical parameters of the different materials inside the model.
Onyedika Anthony Igbokwe, Jithender J. Timothy, Ashwani Kumar, Xiao Yan, Mathias Mueller, Alessandro Verdecchia, Günther Meschke, and Adrian Immenhauser
Solid Earth, 15, 763–787, https://doi.org/10.5194/se-15-763-2024, https://doi.org/10.5194/se-15-763-2024, 2024
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We present a workflow that models the impact of stress regime change on the permeability of fractured Latemar carbonate buildup using a displacement-based linear elastic finite-element method (FEM) and outcrop data. Stress-dependent heterogeneous apertures and effective permeability were calculated and constrained by the study area's stress directions. Simulated far-field stresses at NW–SE subsidence deformation and N–S Alpine deformation increased the overall fracture aperture and permeability.
Willemijn Sarah Maria Theresia van Kooten, Hugo Ortner, Ernst Willingshofer, Dimitrios Sokoutis, Alfred Gruber, and Thomas Sausgruber
Solid Earth, 15, 91–120, https://doi.org/10.5194/se-15-91-2024, https://doi.org/10.5194/se-15-91-2024, 2024
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Extensional deformation creates structures that may be reactivated during subsequent shortening. The Achental structure within the Northern Calcareous Alps fold-and-thrust belt is a natural example of a basin margin that was inverted during Alpine orogeny. We have studied the influence of such inherited inhomogeneities in the field and as an analogue model. We find that oblique shortening can create structures outlining pre-existing faults within a single deformation event.
Yan Cao, Zhijun Jin, Rukai Zhu, and Kouqi Liu
Solid Earth, 14, 1169–1179, https://doi.org/10.5194/se-14-1169-2023, https://doi.org/10.5194/se-14-1169-2023, 2023
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Fourier transform infrared (FTIR) was performed on shale before and after solvent extraction. The extraction yield from shale with THF is higher than other solvents. The organic-C-normalized yield of a mature sample is higher than other samples. The aromaticity of organic matter increases, and the length of organic matter aliphatic chains does not vary monotonically with increasing maturity. The results will help in the selection of organic solvents for oil-washing experiments of shale.
Zbyszek Remin, Michał Cyglicki, and Mariusz Niechwedowicz
Solid Earth, 13, 681–703, https://doi.org/10.5194/se-13-681-2022, https://doi.org/10.5194/se-13-681-2022, 2022
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Traditionally, the axial part of the Polish Basin, i.e. the Mid-Polish Trough, was interpreted as the deepest and most subsiding part of the basin during the Cretaceous times. We interpret this area conversely, as representing a landmass – the Łysogóry–Dobrogea Land. Inversion-related tectonics, uplift on the one hand and enhanced subsidence on the other, drove the development of the Szozdy Delta within the axial part of the basin. New heavy mineral data suggest different burial histories.
Emilija Krsnik, Katharina Methner, Marion Campani, Svetlana Botsyun, Sebastian G. Mutz, Todd A. Ehlers, Oliver Kempf, Jens Fiebig, Fritz Schlunegger, and Andreas Mulch
Solid Earth, 12, 2615–2631, https://doi.org/10.5194/se-12-2615-2021, https://doi.org/10.5194/se-12-2615-2021, 2021
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Here we present new surface elevation constraints for the middle Miocene Central Alps based on stable and clumped isotope geochemical analyses. Our reconstructed paleoelevation estimate is supported by isotope-enabled paleoclimate simulations and indicates that the Miocene Central Alps were characterized by a heterogeneous and spatially transient topography with high elevations locally exceeding 4000 m.
Jean-Philippe Blouet, Patrice Imbert, Sutieng Ho, Andreas Wetzel, and Anneleen Foubert
Solid Earth, 12, 2439–2466, https://doi.org/10.5194/se-12-2439-2021, https://doi.org/10.5194/se-12-2439-2021, 2021
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Biochemical reactions related to hydrocarbon seepage are known to induce carbonates in marine sediments. Seep carbonates may act as seals and force lateral deviations of rising hydrocarbons. However, crustacean burrows may act as efficient vertical fluid channels allowing hydrocarbons to pass through upward, thereby allowing the vertical growth of carbonate stacks over time. This mechanism may explain the origin of carbonate columns in marine sediments throughout hydrocarbon provinces worldwide.
Thomas Voigt, Jonas Kley, and Silke Voigt
Solid Earth, 12, 1443–1471, https://doi.org/10.5194/se-12-1443-2021, https://doi.org/10.5194/se-12-1443-2021, 2021
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Basin inversion in central Europe is believed to have started during Late Cretaceous (middle Turonian) and probably proceeded until the Paleogene. Data from different marginal troughs in central Europe point to an earlier start of basin inversion (in the Cenomanian). The end of inversion is overprinted by general uplift but had probably already occurred in the late Campanian to Maastrichtian. Both the start and end of inversion occurred with low rates of uplift and subsidence.
Arne Jacob, Markus Peltz, Sina Hale, Frieder Enzmann, Olga Moravcova, Laurence N. Warr, Georg Grathoff, Philipp Blum, and Michael Kersten
Solid Earth, 12, 1–14, https://doi.org/10.5194/se-12-1-2021, https://doi.org/10.5194/se-12-1-2021, 2021
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In this work, we combined different imaging and experimental measuring methods for analysis of cross-scale effects which reduce permeability of tight reservoir rocks. Simulated permeability of digital images of rocks is often overestimated, which is caused by non-resolvable clay content within the pores of a rock. By combining FIB-SEM with micro-XCT imaging, we were able to simulate the true clay mineral abundance to match experimentally measured permeability with simulated permeability.
Lydia R. Bailey, Filippo L. Schenker, Maria Giuditta Fellin, Miriam Cobianchi, Thierry Adatte, and Vincenzo Picotti
Solid Earth, 11, 2463–2485, https://doi.org/10.5194/se-11-2463-2020, https://doi.org/10.5194/se-11-2463-2020, 2020
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The Kallipetra Basin, formed in the Late Cretaceous on the reworked Pelagonian–Axios–Vardar contact in the Hellenides, is described for the first time. We document how and when the basin evolved in response to tectonic forcings and basin inversion. Cenomanian extension and basin widening was followed by Turonian compression and basin inversion. Thrusting occurred earlier than previously reported in the literature, with a vergence to the NE, at odds with the regional SW vergence of the margin.
Adrian Linsel, Sebastian Wiesler, Jens Hornung, and Matthias Hinderer
Solid Earth, 11, 1511–1526, https://doi.org/10.5194/se-11-1511-2020, https://doi.org/10.5194/se-11-1511-2020, 2020
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We present a high-resolution 3D analysis of the physicochemical characteristics of two sandstone cubes at the submeter scale. Our study provides insight into the spatial distribution and the controlling factors of small-scale heterogeneity in sandstone media. A comprehensive physicochemical data set is provided, which may help to evaluate the degree of uncertainty that should be considered in field-scale property models.
Georg Schwamborn, Kai Hartmann, Bernd Wünnemann, Wolfgang Rösler, Annette Wefer-Roehl, Jörg Pross, Marlen Schlöffel, Franziska Kobe, Pavel E. Tarasov, Melissa A. Berke, and Bernhard Diekmann
Solid Earth, 11, 1375–1398, https://doi.org/10.5194/se-11-1375-2020, https://doi.org/10.5194/se-11-1375-2020, 2020
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We use a sediment core from the Gobi Desert (Ejina Basin, NW China) to illustrate the landscape history of the area. During 2.5 million years a sediment package of 223 m thickness has been accumulated. Various sediment types document that the area turned from a playa environment (shallow water environment with multiple flooding events) to an alluvial–fluvial environment after the arrival of the Heihe in the area. The river has been diverted due to tectonics.
Philippos Garefalakis and Fritz Schlunegger
Solid Earth, 10, 2045–2072, https://doi.org/10.5194/se-10-2045-2019, https://doi.org/10.5194/se-10-2045-2019, 2019
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The controls on the 20 Myr old Burdigalian transgression in the Swiss Molasse basin have been related to a reduction in sediment flux, a rise in global sea level, or tectonic processes in the adjacent Alps. Here, we readdress this problem and extract stratigraphic signals from the Upper Marine Molasse deposits in Switzerland. In conclusion, we consider rollback tectonics to be the main driving force controlling the transgression, which is related to a deepening and widening of the basin.
Laura Stutenbecker, Peter M. E. Tollan, Andrea Madella, and Pierre Lanari
Solid Earth, 10, 1581–1595, https://doi.org/10.5194/se-10-1581-2019, https://doi.org/10.5194/se-10-1581-2019, 2019
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The Aar and Mont Blanc regions in the Alps are large granitoid massifs characterized by high topography. We analyse when these granitoids were first exhumed to the surface. We test this by tracking specific garnet grains, which are exclusively found in the granitoid massifs, in the sediments contained in the alpine foreland basin. This research ties in with ongoing debates on the timing and mechanisms of mountain building.
Christian Stranne, Matt O'Regan, Martin Jakobsson, Volker Brüchert, and Marcelo Ketzer
Solid Earth, 10, 1541–1554, https://doi.org/10.5194/se-10-1541-2019, https://doi.org/10.5194/se-10-1541-2019, 2019
Mahtab Mozafari, Rudy Swennen, Fabrizio Balsamo, Hamdy El Desouky, Fabrizio Storti, and Conxita Taberner
Solid Earth, 10, 1355–1383, https://doi.org/10.5194/se-10-1355-2019, https://doi.org/10.5194/se-10-1355-2019, 2019
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The dolomitized intervals of the Lower Jurassic deposits exposed in the Montagna dei Fiori Anticline (Central Apennines, Italy) have been investigated. Accordingly, two fault-related dolomitization events were recognised and interpreted as having occurred before and during the Apenninic orogeny. The analyses suggest significant involvement of evaporitic fluids in both events, most likely derived from the underlying Upper Triassic Burano Formation in the detachment level.
Maximilian Rieder, Wencke Wegner, Monika Horschinegg, Stefanie Klackl, Nereo Preto, Anna Breda, Susanne Gier, Urs Klötzli, Stefano M. Bernasconi, Gernot Arp, and Patrick Meister
Solid Earth, 10, 1243–1267, https://doi.org/10.5194/se-10-1243-2019, https://doi.org/10.5194/se-10-1243-2019, 2019
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The formation of dolomite (CaMg(CO3)2), an abundant mineral in Earth's geological record, is still incompletely understood. We studied dolomites embedded in a 100 m thick succession of coastal alluvial clays of Triassic age in the southern Alps. Observation by light microscopy and Sr isotopes suggests that dolomites may spontaneously from concentrated evaporating seawater, in coastal ephemeral lakes or tidal flats along the western margin of the Triassic Tethys sea.
Salomé Mignard, Thierry Mulder, Philippe Martinez, and Thierry Garlan
Solid Earth, 10, 851–869, https://doi.org/10.5194/se-10-851-2019, https://doi.org/10.5194/se-10-851-2019, 2019
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A large quantity a continental material is transported to the oceans by the world rivers. Once in the ocean, these particles can be transported down the continental shelf thanks to underwater avalanches. The repetition of such massive events can form very important sedimentary deposits at the continent–ocean transition. Data obtained during an oceanic cruise in 2010 allowed us to study such a system located offshore of Gabon and to evaluate the importance sediment transport in this area.
Sutieng Ho, Martin Hovland, Jean-Philippe Blouet, Andreas Wetzel, Patrice Imbert, and Daniel Carruthers
Solid Earth, 9, 1437–1468, https://doi.org/10.5194/se-9-1437-2018, https://doi.org/10.5194/se-9-1437-2018, 2018
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A newly discovered type of hydrocarbon leakage structure is investigated following the preliminary works of Ho (2013; et al. 2012, 2013, 2016): blade-shaped gas chimneys instead of classical cylindrical ones. These so-called
Linear Chimneysare hydraulic fractures caused by overpressured hydrocarbon fluids breaching cover sediments along preferential directions. These directions are dictated by anisotropic stresses induced by faulting in sediments and pre-existing salt-diapiric structures.
Leandra M. Weydt, Claus-Dieter J. Heldmann, Hans G. Machel, and Ingo Sass
Solid Earth, 9, 953–983, https://doi.org/10.5194/se-9-953-2018, https://doi.org/10.5194/se-9-953-2018, 2018
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This study focuses on the assessment of the geothermal potential of two extensive upper Devonian aquifer systems within the Alberta Basin (Canada). Our work provides a first database on geothermal rock properties combined with detailed facies analysis (outcrop and core samples), enabling the identification of preferred zones in the reservoir and thus allowing for a more reliable reservoir prediction. This approach forms the basis for upcoming reservoir studies with a focus on 3-D modelling.
Ernest Chi Fru, Stephanos Kilias, Magnus Ivarsson, Jayne E. Rattray, Katerina Gkika, Iain McDonald, Qian He, and Curt Broman
Solid Earth, 9, 573–598, https://doi.org/10.5194/se-9-573-2018, https://doi.org/10.5194/se-9-573-2018, 2018
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Banded iron formations (BIFs) are chemical sediments last seen in the marine sedimentary record ca. 600 million years ago. Here, we report on the formation mechanisms of a modern BIF analog in the Cape Vani sedimentary basin (CVSB) on Milos Island, Greece, demonstrating that rare environmental redox conditions, coupled to submarine hydrothermal activity and microbial processes, are required for these types of rocks to form in the modern marine biosphere.
Annette Kaufhold, Matthias Halisch, Gerhard Zacher, and Stephan Kaufhold
Solid Earth, 7, 1171–1183, https://doi.org/10.5194/se-7-1171-2016, https://doi.org/10.5194/se-7-1171-2016, 2016
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The OPA material has been intensively studied by a variety of multiple scale and non-destructive 3-D X-ray CT investigations, following a consequent top-down approach to identify specific regions of interest. According to the mechanical experiment, it has been observed that the shear failure is located in a clay-rich area. Within the intersecting area of the two main fractures, a so called mylonitic zone with a particle reduction was observed on the open shear failure using CT and SEM techniques.
Georg H. Grathoff, Markus Peltz, Frieder Enzmann, and Stephan Kaufhold
Solid Earth, 7, 1145–1156, https://doi.org/10.5194/se-7-1145-2016, https://doi.org/10.5194/se-7-1145-2016, 2016
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This study improves our understanding of the evolution of pores in shales for modelling transport properties. 3-D microscopy on early and postmature Posidonia Shales showed similar porosities and pore size distributions. Large isolated pore clusters are within carbonates and clay minerals. Pores form during maturation in the postmature-matrix-filling organic matter. Modelled permeabilities are lowest perpendicular to bedding. They decrease with increasing maturity and are comparable to experimental data.
Katherine J. Dobson, Sophia B. Coban, Samuel A. McDonald, Joanna N. Walsh, Robert C. Atwood, and Philip J. Withers
Solid Earth, 7, 1059–1073, https://doi.org/10.5194/se-7-1059-2016, https://doi.org/10.5194/se-7-1059-2016, 2016
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State-of-the-art synchrotron x-ray imaging was used to observe micron scale transport processes in real time. The 20 Hz 3-D image acquisition rates give experimental data free from motion artefacts, and suitable for detailed quantitative analysis of the dynamic fluid distribution, flow pathways and processes. The method marks a major breakthrough in our ability to capture both sub-second and lower frequency non-equilibrium process in many geological or engineering systems.
Steven Henkel, Dieter Pudlo, Frieder Enzmann, Viktor Reitenbach, Daniel Albrecht, Leonhard Ganzer, and Reinhard Gaupp
Solid Earth, 7, 917–927, https://doi.org/10.5194/se-7-917-2016, https://doi.org/10.5194/se-7-917-2016, 2016
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This study investigates the experimentally induced effects of CO2 storage on underground reservoir sandstones by applying high-resolution computer tomography and standard petrophysical methods. The results of digital rock physic calculations derived from the µ-CT scans are compared with measurements achieved by the standard methods. Both approaches lead to similar results for coarse- and medium-grained sandstones but differ for fine-grained sediments.
G. A. Douillet, B. Taisne, È Tsang-Hin-Sun, S. K. Müller, U. Kueppers, and D. B. Dingwell
Solid Earth, 6, 553–572, https://doi.org/10.5194/se-6-553-2015, https://doi.org/10.5194/se-6-553-2015, 2015
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Sedimentary beds can exhibit signs of local deformation in pyroclastic strata. Patterns are reviewed and trigger mechanisms interpreted.
During an eruption, basal granular flows can have a fluidized behavior, inducing over- or underpressure at the bed interface. Basal shear can overturn strata. Large blocks ejected ballistically deform the ground when landing. Explosions at the vent produce shock waves that can destabilize a bed. These syn-eruptive triggers are specific to explosive volcanism.
M. Hermoso, D. Delsate, F. Baudin, L. Le Callonnec, F. Minoletti, M. Renard, and A. Faber
Solid Earth, 5, 793–804, https://doi.org/10.5194/se-5-793-2014, https://doi.org/10.5194/se-5-793-2014, 2014
J. Trabucho-Alexandre, W. W. Hay, and P. L. de Boer
Solid Earth, 3, 29–42, https://doi.org/10.5194/se-3-29-2012, https://doi.org/10.5194/se-3-29-2012, 2012
F. Storti and F. Balsamo
Solid Earth, 1, 25–48, https://doi.org/10.5194/se-1-25-2010, https://doi.org/10.5194/se-1-25-2010, 2010
Cited articles
Argnani, A.: Possible record of a Triassic ocean in the Southern Apennines, Boll. Soc. Geol. It., 124, 109–121, 2005.
Arnaud-Vanneau, A. and Arnaud, H.: Hauterivian to Lower Aptian carbonate shelf sedimentation and sequence stratigraphy in the Jura and northern Subalpine chains (southeastern France and Swiss Jura), in: Carbonate Platforms. Facies, Sequences and Evolution, edited by: Tucker, M. E., Wilson, J. L., Crevello, P. D., Sarg, J. R., and Read, J. F., Int. Assoc. Sedimentol., Spec. Publ., 9, 203–233, 1990.
Bachmann, M. and Hirsch. F.: Lower Cretaceous carbonate platform of the eastern Levant (Galilee and the Golan Heights): stratigraphy and second-order sea-level change, Cret. Res., 27, 487–512, 2006.
Barattolo, F. and De Castro, P.: Early Cretaceous of Mount Tobenna, in: 5th International Symposium on Fossil Algae, Field-trip guide-book, edited by: Barattolo, F., De Castro, P., and Parente, M., pp. 72–78, 1991.
Barron, E. J. and Peterson, W. H.: Model simulation of the Cretaceous ocean circulation, Science, 244, 684–686, 1989.
Bartiromo, A., Barale, G., Barone Lumaga, M. R., Bravi, S., and Barattolo, F.: The Early Cretaceous flora from Profeti, Caserta, Southern Italy, Rev. Paleob. Palynol., 158, 101–116, 2009.
Bartiromo, A., Barale, G., Barone Lumaga, M. R., Bravi, S., and Barattolo, F.: An Early Cretaceous flora from Cusano Mutri, Benevento, southern Italy, Cret. Res., 33, 116–134, 2012.
Birkeland, C.: Nutrient availability as a major determinant of differences among coastal hard-substratum communities in different regions of the tropics, in: Comparisons between Atlantic and Pacific tropical coastal marine ecosystems: community structure, ecological processes, and productivity, edited by: Birkeland, C., UNESCO Rep. Mar. Sci., 46, 45–97, 1987.
Bonardi, G., D'Argenio, B., and Perrone, V.: Carta geologica dell'Appennino meridionale, Mem. Soc. Geol. It., 41, 1341, 1992.
Bralower, T. J., Arthur, M. A., Leckie, R. M., Sliter, W. V., Allard, D., and Schlanger, S. O.: Timing and paleoceanography of oceanic dysoxia/anoxia in the Late Barremian to Early Aptian (Early Cretaceous), Palaios, 9, 335–369, 1994.
Bralower, T. J., Fullagar, P. D., Paull, C. K., Dwyer, G. S., and Leckie, R. M.: Mid-Cretaceous strontium-isotope stratigraphy of deep-sea section, Geol. Soc. Am. Bull., 109, 1421–1442, 1997.
Bralower, T. J., Cobabe, E., Clement, B., Sliter, W. V., Osburn, C., and Longoria, J.: The record of global change in mid-Cretaceous (Barremian-Albian) sections from the Sierra Madre, northeastern Mexico, J. Foraminifer. Res., 29, 418–437, 1999.
Brandt, U. and Veizer, J.: Chemical diagenesis of a multicomponent carbonate systems – 2: stable isotopes, J. Sed. Petr., 51, 987–997, 1981.
Bravi, S. and De Castro, P.: The Cretaceous fossil fishes level of Capo d'Orlando, near Castellammare di Stabia (NA): biostratigraphy and depositional environment, Mem. Sci. Geol., 47, 45–72, 1995.
Brescia, M., D'Argenio, B., Ferreri, V., Pelosi, N., Rampone, S., and Tagliaferri, R.: Neural net aided detection of astronomical periodicities in geologic records, Earth Plan. Sci. Lett., 139, 33–45, 1996.
Brock, T. D., Madigan, M. T., Martinko, J. M., and Parker, J.: Biology of Microorganisms, 7th edn. Prentice Hall, New Jersey, 1994.
Buonocunto, F. P., D'Argenio, B., Ferreri, V., and Raspini, A.: Microstratigraphy of highly organized carbonate platform deposits of Cretaceous age. The case of Serra Sbregavitelli, Matese (Central Apennines), G. Geol., 56, 179–192, 1994.
Burla, S., Heimhofer, U., Hochuli, P. A., Weissert, H., and Skelton, P.: Changes in sedimentary patterns of coastal and deep-sea successions from the North Atlantic (Portugal) linked to Early Cretaceous environmental change, Palaeogeogr. Palaeoclimatol. Palaeoecol., 257, 38–57, 2008.
Carannante, G., Pugliese, A., Ruberti, D., Simone, L., Vigliotti, M., and Vigorito, M.: Evoluzione cretacica di un settore della piattaforma apula da dati di sottosuolo e di affioramento (Appennino campano-molisano), It. J. Geosci. (Boll. Soc. Geol. It.), 128, 3–31, 2009.
Carras, N., Conrad, M. A., and Radoičič, R.: Salpingoporella, a common genus of Mesozoic Dasycladales (calcareous green algae), Rev. Paléobiol., 25, 457–517, 2006.
Casero, P., Roure, F., Endignoux, L., Moretti, I., Mueller, C., Sage, L., and Vially, R.: Neogene geodynamic evolution of the Southern Apennines, Mem. Soc. Geol. It., 41, 109–120, 1988.
Castro, J. M., de Gea, G.A., Ruiz-Ortiz, P. A., and Nieto, L. M.: Development of carbonate platforms on an extensional (rifted) margin: the Valanginian-Albian record of the Prebetic of Alicante (SE Spain), Cret. Res., 29, 848–860, 2008.
Cherchi, A. and Schroeder, R.: Calcimicrobial oncoid coatings from the Pliensbachian Massone Member (Calcari Grigi Formation, Trento Platform, Italy), in: Giornata di Studi Paleontologici "Prof. C. Loriga Broglio", Ferrara, 18 June 2004, edited by: Fugagnoli, A. and Bassi, D., Annali dell'Università di Ferrara, Sez. Museologia Scientifica e Naturalistica, Spec. Vol., 45–49, 2005.
Cherchi, A. and Schroeder, R.: The Praeorbitolina/Palorbitolinoides Association: an Aptian biostratigraphic key-interval at the southern margin of the Neo-Tethys, Cret. Res. (2012), https://doi.org/10.1016/j.cretres.2012.02.018, 2012.
Cherchi, A., De Castro, P., and Schroeder, R.: Sull'età dei livelli a Orbitolinidi della Campania e delle Murge Baresi (Italia meridionale), Boll. Soc. Nat. Napoli, 87, 363–385, 1978.
Chihaoui, A., Jaillard, E., Latil, J.-L., Zghal, I., Susperregui, A.-S., Touir, J., and Ouali, J.: Stratigraphy of the Hameima and lower Fahdene Formations in the Tadjerouine area (Northern Tunisia), J. Afr. Earth Sci., 58, 387–399, 2010.
Chiocchini, M., Farinacci, A., Mancinelli, A., Molinari, V., and Potetti, M.: Biostratigrafia a foraminiferi, dasicladali e calpionelle delle successioni carbonatiche mesozoiche dell'Appennino centrale (Italia), in: Biostratigrafia dell'Italia Centrale, edited by: Mancinelli, A., Studi Geol. Camerti, Spec. Vol. A, 9–129, 1994.
Clarke, L. J. and Jenkyns, H. C.: New oxygen isotope evidence for long-term Cretaceous climatic change in the Southern Hemisphere, Geology, 27, 699–702, 1999.
Coffin, M. F., Pringle, M. S., Duncan, R. A., Gladczenko, T. P., Storey, M., Muller, R. D., and Gahan, L. A.: Kerguelen hotspot magma output since 130 Ma, J. Petrol., 43, 1121–1139, 2002.
Coffin, M. F., Duncan, R. A., Eldholm, O., Fitton, J. G., Frey, F. A., Larse, H. C., Mahoney, J. J., Saunders, A. D., Schlich, R., and Wallace, P. J.: Large igneous provinces and scientific ocean drilling. Status quo and a look ahead, Oceanography, 19, 150–160, 2006.
Costa, O. G.: Studi sopra i terreni ad ittioliti delle provincie meridionali d'Italia. Parte III. Castellammare, Atti Rend. Acc. Sc. Fis. Mat. Napoli, ser. 173, 1–30, 1866.
Danelian, T., Tsikos, H., Gardin, S., Baudin, F., Bellier, J.-P., and Emmanuel, L.: Global and regional palaeoceanographic changes as recorded in the mid-Cretaceous (Aptian–Albian) sequence of the Ionian zone (NW Greece), J. Geol. Soc., Lond., 161, 703–709, 2004.
D'Argenio, B., Amodio, S., Ferreri, F., and Pelosi, N.: Hierarchy of high frequency orbital cycles in Cretaceous carbonate platform strata, Sediment. Geol., 113, 169–193, 1997.
D'Argenio, B., Ferreri, V., Raspini, A., Amodio, S., and Buonocunto, F.\textsc{P.:} Cyclostratigraphy of a carbonate platform as a tool for high precision correlation, Tectonophysics, 315, 357–384, 1999.
D'Argenio, B., Ferreri, V., Weissert, H., Amodio, S., Buonocunto, F. P., and Wissler, L.: A multidisciplinary approach to global correlation and geochronology. the Cretaceous shallow-water carbonates of Southern Apennines, Italy, in: Cyclostratigraphy; approaches and cases histories, edited by: D'Argenio, B., Fischer, A. G., Premoli Silva, I., Weissert, H., and Ferreri, V., SEPM Spec. Publ., 81, 103–122, 2004.
Dean, W. E. and Fouch, T. D.: Lacustrine environment, in: Carbonate depositional environments edited by: Scholle, P. A., Bebout, D. G., and Moore, C. H., Am. Assoc. Pet. Geol., Mem., 33, 97–130, 1983.
De Castro, P.: Nuove osservazioni sul livello ad Orbitoline in Campania, Boll. Soc. Nat. Napoli, 71, 103–135, 1963.
De Castro, P.: Mesozoic, in: 5th International Symposium on Fossil Algae, Field-trip guide-book, edited by: Barattolo, F., De Castro, P., and Parente, M., 21–38, 1991.
Delgado, O. and Lapointe, B. E.: Nutrient-limited productivity of calcareous versus fleshy macroalgae in a eutrophic, carbonate-rich tropical marine environment, Coral Reefs, 15, 151–159, 1994.
Di Lucia, M.: Il record dei cambiamenti globali nelle piattaforme carbonati che del Cretacico medio dell'Appennino meridionale, Doctorate Thesis, University of Naples, available at: http://www.fedoa.unina.it/3342/1/Matteo_Di_Lucia_-_PhD_thesis.pdf. 125 p., 2009.
Di Lucia, M. and Parente, M.: Carbon-isotope stratigraphy of upper Barremian-lower Albian shallow-water carbonates of southern Apennines (Italy): high-resolution correlation with deep-water reference sections, Soc. Geol. It., Rendiconti Online, 2, 65–70, 2008.
Di Lucia, M., Mutti, M., and Parente, M.: Bio-chemostratigraphy of the Barremian-Aptian shallow-water carbonates of the southern Apennines (Italy): pinpointing the OAE1a in a Tethyan carbonate platform, Solid Earth Discuss., 3, 789–838, https://doi.org/10.5194/sed-3-789-2011, 2011.
Doglioni, C.: Foredeeps versus subduction zones, Geology, 22, 271–274, 1994.
Donnadieu, Y., Dromart, G., Goddéris, Y., Pucéat, E., Brigaud, B., Dera, G., Dumas, C., and Olivier, N.: A mechanism for brief glacial episodes in the Mesozoic greenhouse, Paleoceanography, 26, PA3212, https://doi.org/10.1029/2010PA002100, 2011.
Embry, J. C., Vennin, E., van Buchem, F. S. P., Schroeder, R., Pierre, C., and Aurell, M.: Sequence stratigraphy and carbon isotope stratigraphy of an Aptian mixed carbonate-siliciclastic platform to basin transition (Galve sub-basin, NE Spain), in: Mesozoic and Cenozoic Carbonate Systems of the Mediterranean and the Middle East: Stratigraphic and Diagenetic Reference Models, edited by: van Buchem, F. S. P., Gerdes, K. D., and Esteban, M., Geol. Soc., London, Engineering Geology Spec. Publ., 329, 113–143, 2010.
Emeis, K.-C. and Weissert, H.: Tethyan-Mediterranean organic carbon-rich sediments from Mesozoic black shales to sapropels, Sedimentology, 56, 247–266, 2009.
Erba, E., Channell, J. E. T., Claps, M., Jones, C., Larson, R., Opdyke, B., Premoli Silva, I., Riva, A., Salvini, G., and Torricelli, S.: Integrated stratigraphy of the Cismon Apticore (Southern Alps, Italy): a "reference section" for the Barremian-Aptian interval at low latitudes, J. Foraminifer. Res., 29, 371–391, 1999.
Erba, E., Bottini, C., Weissert, H., and Keller, C. E.: Calcareous nannoplankton response to surface-water acidification around Oceanic Anoxic Event 1a, Science, 329, 428–432, 2010.
Erbacher, J., Thurow, J., and Littke, R.: Evolution patterns of radiolaria and organic matter variations: A new approach to identify sea-level changes in mid-Cretaceous pelagic environments, Geology, 24, 499–502, 1996.
Fassel, M. L. and Bralower, T. J.: Warm, equable mid-Cretaceous: Stable isotope evidence, Geol Soc. Am. Spec. Pap., 332, 121–142, 1999.
Ferreri, V., Weissert, H., D'Argenio, B., and Buonocunto, F. P.: Carbon isotope stratigraphy: a tool for basin to carbonate platform correlation, Terra Nova, 9, 57–61, 1997.
Föllmi, K. B.: Early Cretaceous life, climate and anoxia, Cret. Res., 35, 230–257, 2012.
Föllmi, K. B., Weissert, H., Bisping, M., and Funk, H.: Phosphogenesis, carbon isotope stratigraphy, and carbonate-platform evolution along the Lower Cretaceous northern Tethyan margin, Geol. Soc. Am. Bull., 106, 729–746, 1994.
Friedrich, O., Reichelt, K., Herrle, J. O., Lehmann, J., Pross, J., and Hemleben, C.: Formation of the Late Aptian Niveau Fallot black shales in the Vocontian Basin (SE France): evidence from foraminifera, palynomorphs, and stable isotopes, Mar. Micropal., 49, 65–85, 2003.
Gattacceca, J. and Speranza, F.: Paleomagnetism of Jurassic to Miocene sediments from the Apenninic carbonate platform (southern Apennines, Italy): evidence for a 60° counterclockwise Miocene rotation, Earth Plan. Sci. Lett., 201, 19–34, 2002.
Goldhammer, R. K., Dunn, P. A., and Hardie, L. A.: Depositional cycles, composite sea-level changes, cycle stacking pattern and the hierarchy of stratigraphic forcing. Examples from Alpine Triassic platform carbonates, Geol. Soc. Am. Bull., 102, 535–562, 1990.
Golubic, S., Radoicic, R., and Seong-Joo, L.: Decastronema kotori gen. nov., comb. Nov.: a mat-forming cyanobacterium on Cretaceous carbonate platforms and its modern counterparts, Carnets de Géologie/Notebooks on Geology – Article 2006/02 (CG2006{_}A02), 2006.
Graziano, R.: The Early Cretaceous drowning unconformities of the Apulia carbonate platform (Gargano Promontory, southern Italy): local fingerprints of global palaeoceanographic events, Terra Nova, 11, 245–250, 1999.
Graziano, R.: 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, Cret. Res., 21, 106–127, 2000.
Graziano, R.: The Early Cretaceous drownings of Tethyan carbonate platforms: controlling mechanisms and paleoceanography. Insights from the Apulia record, in: Temperate-type (Foramol facies) carbonate platforms versus tropical-type (Chlorozoan facies) carbonate platforms: tridimensional arrangement of lithofacies, benthic associations and evolution of the related depositional systems, edited by: Simone, L., Ruberti, D., and Graziano, R., COFIN 2000 Workshop, Pozzuoli (Naples), 25–27 February 2003, 55–62, 2003.
Guiscardi, G.: Sull'età degli scisti calcarei di Castellammare, Rend. R. Acc. Sc. Fis. Mat. Napoli, ser.1, 5, 122–123, 1866.
Hallock, P.: The role of nutrient availability in bioerosion: consequences to carbonate buildups, Palaeogeogr. Palaeoclimatol. Palaeoecol., 63, 275–291, 1988.
Hallock, P.: Global change and modern coral reefs: New opportunities to understand shallow-water carbonate depositional processes, Sediment. Geol., 175, 19–33, 2005.
Hallock, P. and Schlager, W.: Nutrient excess and the demise of coral reefs and carbonate platforms, Palaios, 1, 389–398, 1986.
Hansen, K. W. and Wallmann, K.: Cretaceous and Cenozoic evolution of seawater composition, atmospheric O2 and CO2: a model perspective, Am. J. Sci., 303, 94–148, 2003.
Haq, B. U., Hardenbol, J., and Vail, P. R.: Chronology of fluctuating sea level since Triassic (250 million years ago to present), Science, 235, 1156–1167, 1987.
Haq, B. U., Hardenbol, J., and Vail, P. R.: Mesozoic and Cenozoic chronostratigraphy and cycles of sea-level change, in: Sea-level changes – An integrated approach, edited by: Wilgus, C. K., Hastings, B. S., Kendall, C. G. St. C., Posamentier, H. W., Ross, C. A., and van Wagoner, J. C., SEPM Spec. Publ., 42, 71–108, 1988.
Haworth, M., Hesselbo, S. P., McElwain, J. C., Robinson, S. A., and Brunt, J. W.: Mid-Cretaceous pCO2 based on stomata of the extinct conifer Pseusofreneloplis (Cheirolepidiaceae), Geology, 33, 749–752, 2005.
Hay, W. W.: Evolving ideas about the Cretaceous climate and ocean circulation, Cret. Res, 29, 725–753, 2008.
Heldt, M., Lehmann, J., Bachmann, M., Negra, H., and Kuss, J.: Increased terrigenous influx but no drowning: palaeoenvironmental evolution of the Tunisian carbonate platform margin during the Late Aptian, Sedimentology, 57, 695–719, 2010.
Herrero, A. and Flores, E.: The cyanobacteria: molecular biology, genomics and evolution, Caister Adademic Press, Norfolk, UK, 484 pp., 2008.
Herrle, J. O. and Mutterlose, J.: Calcareous nannofossils from the Aptian-Lower Albian of southeast France: palaeoecological and biostratigraphic implications, Cret. Res., 24, 1–22, 2003.
Herrle, J. O., Pross, J., Friedrich, O., and Hemleben, C.: Short-term environmental changes in the Cretaceous Tethyan Ocean: micropalaeontological evidence from the Early Albian Oceanic Anoxic Event 1b, Terra Nova, 15, 14–19, 2003.
Hong, S. K., and Lee, Y. I.: Evaluation of atmospheric carbon dioxide concentrations during the Cretaceous,Earth Plan. Sci. Lett., 327, 23–28, 2012.
Hottinger, L.: Larger foraminifera, giant cells with a historical background, Naturwissenschaften, 69, 361–371, 1982.
Hottinger, L.: Shallow benthic foraminiferal assemblages as signal for depth of their deposition and their limitations, Bull. Soc. Fr., 168, 491–505, 1997.
Hu, X., Jansa, L., and Sarti, M.: Mid-Cretaceous oceanic red beds in the Umbria–Marche Basin, central Italy: Constraints on paleoceanography and paleoclimate, Palaeogeog. Palaeoclimat. Palaeoecol., 233, 163–186, 2005.
Hu, X., Zhao, K., Yilmaz, I. O., and Li, Y.: Stratigraphic transition and palaeoenvironmental changes from the Aptian oceanic anoxic event 1a (OAE1a) to the oceanic red bed 1 (ORB1) in the Yenicesihlar section, central Turkey, Cret. Res. (2012), https://doi.org/10.1016/j.cretres.2012.01.007, 2012.
Huang, C., Hinnov, L., Fischer, A. G., Grippo, A., and Herbert, T.: Astronomical tuning of the Aptian Stage from Italian reference sections, Geology, 38, 899–902, 2010.
Huang, Y., Yang, G., Wang, C., and Wu, H.: The stabilisation of the long-term Cretaceous greenhouse climate: Contribution from the semi-periodical burial of phosphorus in the ocean, Cret. Res. (2012), https://doi.org/10.1016/j.cretres.2012.04.005, 2012.
Huck, S., Rameil, N., Korbar, T., Heimhofer, U., Wieczorek, T. D., and Immenhauser, A.: Latitudinally different responses of Tethyan shoal-water carbonate systems to the Early Aptian oceanic anoxic event (OAE 1a), Sedimentology, 57, 1585–1614, 2010.
Huck, S., Heimhofer, U., Rameil, N., Bodin, S., and Immenhauser, A.: Strontium and carbon-isotope chronostratigraphy of Barremian–Aptian shoal-water carbonates: Northern Tethyan platform drowning predates OAE 1a, Earth Plan. Sci. Lett., 304, 547–558, 2011.
Husinec, A. and Read, J. F.: Microbial laminite versus rooted and burrowed caps on peritidal cycles: salinity control on parasequence development, Early Cretaceous isolated carbonate platform, Croatia. Geol. Soc. Am. Bull., 123, 1896–1907, 2011.
Husinec, A., Velić, I., Fucek, L., Vlahović, I., Maticec, D., Ostrić, N., and Korbar, T.: Mid Cretaceous orbitolinid (Foraminiferida) record from the islands of Cres and Losinj (Croatia) and its regional stratigraphic correlation, Cret. Res., 21, 155–171, 2000.
Husinec, A., Velić, I., and Sokač, B.: Diversity patterns in Mid-Cretaceous benthic foraminifers and dasycladalean algae of the southern part of the Mesozoic Adriatic Platform, Croatia, in: Geologic Problem Solving with Microfossils: A Volume in Honor of Garry D. Jones, edited by: Demchuk, T. D. and Gary, A. C., SEPM, Spec. Publ., 93, 153–170, 2009.
Immenhauser, A., Hillgärtner, H., and van Bentum, E.: Microbial-foraminiferal episodes in the Early Aptian of the southern Tethyan margin: ecological significance and possible relation to oceanic anoxic event 1a, Sedimentology, 52, 77–99, 2005.
Jahren, A. H.: The biogeochemical consequences of the mid-Cretaceous superplume, J. Geodyn., 34, 177–191, 2002.
Jenkyns, H. C.: Cretaceous anoxic events: from continents to oceans, J. Geol. Soc., Lond., 137, 171–188, 1980.
Jenkyns, H. C.: Geochemistry of oceanic anoxic events, Geochem. Geophys. Geosys., 11, Q03004, https://doi.org/10.1029/2009GC002788, 2010.
Jenkyns, H. C. and Wilson, P. A.: Stratigraphy, paleoceanography and evolution of Cretaceous Pacific guyots: relics from a greenhouse earth, Am. J. Sci., 299, 341–392, 1999.
Jenkyns, H. C., Gale, A. S., and Corfield, R. M.: Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its paleoclimatic significance, Geol. Mag., 131, 1–34, 1994.
Johnson, C. C., Barron, E. J., Kaufmann, E. G., Arthur, M. A., Fawcett, P. J., and Yasuda, M. K.: Middle Cretaceous reef collapse linked to ocean heat transport, Geology, 24, 376–380, 1996.
Jones, C. E. and Jenkyns, H. C.: Seawater strontium isotopes, oceanic anoxic events, and seafloor hydrothermal activity in the Jurassic and Cretaceous, Am. J. Sci., 301, 112–149, 2001.
Kaźmierczak, J. and Iryu, Y.: Cyanobacterial origin of microcrystalline cements from Pleistocene rhodoliths and coralline algal crusts of Okierabu-jima, Japan, Acta Palaeontol. Polonica, 44, 117–130, 1999.
Kaźmierczak, J., Coleman, M. L., Gruszczynski, M., and Kempe, S.: Cyanobacterial key to the genesis of micrite and peloidal limestones in ancient seas, Acta Palaeontol. Polonica, 41, 319–338, 1996.
Kerans, C.: Use of one- and two-dimensional cycle analysis in establishing high-frequency sequence frameworks, in: Milankovitch sea level changes, cycles and reservoirs on carbonate platforms in Greenhouse and Ice-house worlds, edited by: Read, J. F., Kerans, C., and Weber, L. J., SEPM Short Course, 35, part 2, 1–20, 1995.
Kidwell, S. M.: Palaeobiological and sedimentological implications of fossil concentrations, Nature, 318, 457–460, 1985.
Kidwell, S. M.: Models for fossil concentrations: paleobiologic implications, Paleobiology, 12, 6–24, 1986.
Korbar, T.: Orogenic evolution of the External Dinarides in the NE Adriatic region: a model constrained by tectonostratigraphy of Upper Cretaceous to Paleogene carbonates, Earth Sci. Rev., 9, 296–312, 2009.
Kump, L. R., Brantley, L., and Arthur, M. A.: Chemical weathering, atmospheric CO2, and climate, Annu. Rev. Earth Plan. Sci., 28, 611–667, 2000.
Kuroda, J., Tanimizu, M., Hori, R. S., Suzuki, K., Ogawa, N. O., Tejada, M. L. G., Coffin, M. F., Coccioni, R., Erba, E., and Ohkouchi, N.: Lead isotopic record of Barremian–Aptian marine sediments: Implications for large igneous provinces and the Aptian climatic crisis, Earth Plan. Sci. Lett., 307, 126–134, 2011.
Larson, R. L. and Erba, E.: Onset of the mid-Cretaceous greenhouse in the Barremian-Aptian: igneous events and the biological, sedimentary, and geochemical responses, Paleoceanography, 14, 663–678, 1999.
Li, Y.-X., Bralower, T. J., Montañez, I. P., Osleger, D. A., Arthur, M. A., Bice, D. M., Herbert, T. D., Erba, E., and Premoli Silva, I.: Toward an orbital chronology for the early Aptian Oceanic Anoxic Event (OAE1a, $\sim $120 Ma), Earth Plan. Sci. Lett., 271, 88–100, 2008.
Longo, G., D'Argenio, B., Ferreri, V., and Iorio, M.: Fourier evidence for high frequency astronomical cycles recorded in Early Cretaceous carbonate platform strata, Monte Maggiore southern Apennines, Italy, in: Orbital Forcing and Cyclic Sequences, edited by: De Boer, P. L. and Smith, D. G., Int. Assoc. Sedimentol., Spec. Publ., 19, 77–85, 1994.
Lowenstam, H. A. and Weiner, S.: On Biomimeralization, New York, Oxford University Press, 324 pp., 1989.
Masse, J.-P. and Fenerci-Masse, M.: Drowning discontinuities and stratigraphic correlation in platform carbonates. The late Barremian-early Aptian record of southeast France, Cret. Res., 32, 659–684, 2011.
Masse, J.-P., Fenerci-Masse, M., Korbar, T., and Velić, I.: Lower Aptian Rudist Faunas (Bivalvia, Hippuritoidea) from Croatia, Geol. Croat., 57, 117–137, 2004.
Matthews, R. K. and Al-Husseini, M. I.: Orbital forcing glacio-eustasy: A sequence-stratigraphic time scale, GeoArabia, 15, 155–167, 2010.
Mazzoli, S., Barkham, S., Cello, G., Gambini, R., Mattioni, L., Shiner, P., and Tondi, E.: Recontruction of continental margin architecture deformed by the contraction of the Lagonegro Basin, southern Apennines, Italy, J. Geol. Soc. Lond., 158, 309–319, 2001.
Méhay, S., Keller, C. E., Bernasconi, S. M., Weissert, H., Erba, E., Bottini, C., and Hochuli, P. A.: A volcanic CO2 pulse triggered the Cretaceous Oceanic Anoxic Event 1a and a biocalcification crisis, Geology, 37, 819–822, 2009.
Menegatti, A., Weissert, H., Brown, R. S., Tyson, R. V., Farrimond, P., Strasser, A., and Caron, M.: High-resolution δ13C stratigraphy through the early Aptian "Livello Selli" of the Alpine Tethys, Paleoceanography, 13, 530–545, 1998.
Miller, A. G., Espie, G. S., and Canvin, D. T.: Physiological aspects of CO_{2 }$and HCO$^{-}3 transport by cyanobacteria: a review, Can. J. Bot., 68, 1291–1302, 1989.
Mondillo, N., Balassone, G., Boni, M., and Rollinson, G.: Karst bauxites in the Campania Apennines (southern Italy): a new approach, Period. Mineral., 80, 407–432, 2011.
Montañez, I. P. and Osleger, D. A.: Parasequence stacking patterns, third-order accommodation events, and sequence stratigraphy of Middle to Upper Cambrian platform carbonates, Bonanza King Formation, southern Great Basin, in: Carbonate Sequence Stratigraphy, edited by: Loucks, R. G. and Sarg, J. F., Am. Assoc. Pet. Geol., Mem., 57, 305–326, 1993.
Mostardini, F. and Merlini, S.: Appennino centro-meridionale. Sezioni geologiche e proposta di modello strutturale, Mem. Soc. Geol. It., 35, 177–202, 1986.
Mutterlose, J., Bornemann, A., and Herrle, J.: The Aptian-Albian cold snap: evidence for "mid" Cretaceous icehouse interludes, N. Jb. Geol. Paläont. Abh., 252, 217–225, 2009.
Mutti, M. and Hallock, P.: Carbonate systems along nutrient and temperature gradients: some sedimentological and geochemical constraints, Int. J. Earth Sci. (Geol Rundsch), 92, 465–475, 2003.
Najarro, M., Rosales, I., Moreno-Bedmar, J. A., de Gea, G. A., Barrón, E., Company, M., and Delanoy, G.: High-resolution chemo- and biostratigraphic records of the Early Aptian Oceanic Anoxic Event in Cantabria (N Spain): Palaeoceanographic and palaeoclimatic implications, Palaeogeog. Palaeoclimat. Palaeoecol., 299, 137–158, 2011.
Ogg, J. G., Agterberg, F. P., and Gradstein, F. M.: The Cretaceous period, in: A geologic time scale 2004, edited by: Gradstein, F., Ogg, J., and Smith, A., Cambridge University Press, 344–383, 2004.
Oglesby, R. and Park, J.: The effect of precessional insolation changes on the Cretaceous climate and cyclic sedimentation, J. Geophys. Res., 94, 14793–14816, 1989.
Patacca, E. and Scandone, P.: Geology of the Southern Apennines, in: Crop-04, edited by: Mazzotti, A., Patacca, E., and Scandone P., Boll. Soc. Geol. It., Spec. Issue 7, 75–119, 2007.
Pelosi, N. and Raspini, A.: Analisi spettrale della ciclicità di alta frequenza in successioni carbonatiche neritiche di limitato spessore. Il caso del Cretacico dei Monti di Sarno (Campania), G. Geol., 55, 37–49, 1993.
Philip, J.: Peri-Tethyan neritic carbonate areas: distribution through time and driving factors, Palaeogeogr. Palaeoclimatol. Palaeoecol., 196, 19–37, 2003.
Pittet, B., van Buchem, F. S. P., Hillgärtner, H., Razin, P., Grötsch, J., and Droste, H.: Ecological succession, palaeoenvironmental change, and depositional sequences of Barremian-Aptian shallow-water carbonates in northern Oman, Sedimentology, 49, 555–581, 2002.
Price, G. D., Sellwood, B. W., and Valdes, P. J.: Sedimentological evaluation of general circulation model simulations for the "greenhouse" Earth: Cretaceous and Jurassic case studies, Sediment. Geol., 100, 159–180, 1995.
Price, G. D., Valdes, P. J., and Sellwood, B. W.: A comparison of GCM simulated Cretaceous "greenhouse" and "icehouse" climates: implications for the sedimentary record, Palaeogeog. Palaeoclimat. Palaeoecol., 142, 123–138, 1998.
Rameil, N., Immenhauser, A., Warrlich, G., Hillgärtner, H., and Droste, H.: Morphological patterns of Aptian Lithocodium–Bacinella geobodies: relation to environment and scale, Sedimentology, 57, 883–911, 2010.
Raspini, A.: Sedimentologia e ciclostratigrafia del Cretacico inferiore in facies di piattaforma carbonatica dell'Appennino centro-meridionale, Doctorate Dissertation, Univ. Bologna, 1996.
Raspini, A.: Microfacies analysis of shallow water carbonates and evidence of hierarchically organized cycles. Aptian of Monte Tobenna, Southern Apennines, Italy, Cret. Res., 19, 197–223, 1998.
Raspini, A.: Stacking pattern of cyclic carbonate platform strata. Lower Cretaceous of southern Apennines, Italy, J. Geol. Soc. Lond., 158, 353–366, 2001.
Read, J. F., Kerans, C., and Weber, L. J.: Milankovitch sea level changes, cycles and reservoirs on carbonate platforms in Greenhouse and Ice-house worlds, SEPM Short Course, 35, 81 pp., 1995.
Ridgwell, A. and Zeebe, R. E.: The role of the global carbonate cycle in the regulation and evolution of the Earth system, Earth Plan. Sci. Lett., 234, 299–315, 2005.
Riding, R.: Microbial carbonates: the geological record of calcified bacterial-algal mats and biofilms, Sedimentology, 47 (Suppl. 1), 179–214, 2000.
Riding, R. and Wright, V. P.: Paleosols and tidal flat/lagoon sequences on a Carboniferous carbonate shelf: sedimentary associations of triple disconformities, J. Sed. Petr., 51, 1323–1339, 1981.
Robson, J.: Depositional models for some Cretaceous carbonates from the Sorrento Peninsula, Mem. Soc. Geol. Ital., 40, 251–257, 1987.
Royer, D. L., Berner, R. A., Montañez, I. P., Tabor, N. J., and Beerling, D. J.: CO2 as a primary driver of Phanerozoic climate, GSA Today, 14, 4–10, 2004.
Ruiz-Ortiz, P. A. and Castro, J. M.: Carbonate depositional sequences in shallow to hemipelagic platform deposits; Aptian, Prebetic of Alicante (SE Spain), Bull. Soc. Géol. Fr., 169, 21–33, 1998.
Sandulli, R. and Raspini, A.: Regional to global correlation of Lower Cretaceous (Hauterivian-Barremian) carbonate platforms of the southern Apennines and Dinarides, Sediment. Geol., 165, 117–153, 2004.
Scheepers, P. J. J. and Langereis, C. G.: Paleomagnetic evidence for counter-clockwise rotations in the southern Apennines fold-and-thrust belt buring the Late Pliocene and Middle Pleistocene, Tectonophysics, 239, 43–59, 1994.
Schlager, W.: Benthic carbonate factories of the Phanerozoic, Int. J. Earth Sci., 92, 1–26, 2003.
Schlager, W., Philip, J., and Bosellini, A.: Cretaceous carbonate platforms, in: Cretaceous Resources Events and Rhythms, edited by: Beaudoin, B. and Ginsburg, R., Nato Adv Res Workshop, 87–112, 1988.
Schlanger, S. O. and Jenkyns, H .C.: Oceanic anoxic events: causes and consequences, Geol Mijnb, 55, 179–211, 1976.
Scholle, P. A. and Arthur, M. A.: Carbon-isotope fluctuations in Cretaceous pelagic limestones: potential stratigraphic and petroleum exploration tool, Am. Assoc. Pet. Geol. Bull., 64, 67–87, 1980.
Schroeder, R., van Buchem, F. S. P., Cherchi, A., Baghbani, D., Vincent, B., Immenhauser, A., and Granier, B.: Revised orbitolinid biostratigraphic zonation for the Barremian-Aptian of the eastern Arabian Plate and implications for regional stratigraphic correlations, GeoArabia, Spec. Publ., 4, 49–96, 2010.
Seilacher, A.: Trace Fossil Analysis. Springer-Verlag Berlin Heidelberg, 2007.
Simmons, M. D., Emery, D., and Pickard, N. A. H.: Hensonella dinarica (Radoičič), an originally calcitic Early Cretaceous Dasycladacean alga, Palaeontology, 34, 955–961, 1991.
Simmons, M. D., Whittaker, J. E., and Jones, R. W.: Orbitolinids from Cretaceous sediments of the Middle East – a revision of the F. R. S. Henson and Associates Collection, in: Proceedings of the Fifth International Workshop on Agglutinated Foraminifera, edited by: Hart, M. B., Kaminski, M. A. and Smart, C. W., Grzybowski Foundation Spec. Publ., 7, 411–437, 2000.
Skelton, P. W. and Gili, E.: Rudists and carbonate platforms in the Aptian: a case study on biotic interactions with ocean chemistry and climate, Sedimentology, 59, 81–117, 2012.
Smith, A. G., Smith, D. G., and Funnell, B. M.: Atlas of Mesozoic and Cenozoic Coastlines, Cambridge University Press, London, 1994.
Stanley, S. M.: Influence of seawater chemistry on biomineralization throughout phanerozoic time: Paleontological and experimental evidence, Palaeogeog. Palaeoclimat. Palaeoecol., 232, 214–236, 2006.
Stanley, S. M. and Hardie, L. A.: Secular oscillations in the carbonate mineralogy of reef-building and sediment-producing organisms driven by tectonically forced shifts in seawater chemistry, Palaeogeog., Palaeoclimatol., Palaeoecol., 144, 3–19, 1998.
Stanley, S. M., Ries, J. B., and Hardie, L. A.: Low-magnesium calcite produced by coralline algae in seawater of Late Cretaceous composition, PNAS, 99, 15323–15326, 2002.
Steuber, T.: Plate tectonic control on the evolution of Cretaceous platform-carbonate production, Geology, 30, 259–262, 2002.
Stricklin Jr., F. L., Smith, C. I., and Lozo, F. E.: Stratigraphy of Lower Cretaceous Trinity deposits of central Texas, Bur. Econ. Geol., Rep. Investigations, Austin, 71, 63 pp., 1971.
Takashima, R., Sano, S.-I., Iba, Y., and Nishi, H.: The first Pacific record of the Late Aptian warming event, J. Geol. Soc., London, 164, 333–339, 2007.
Tasli, K., Ozer, E., and Koc, H.: Benthic foraminiferal assemblages of the Cretaceous platform carbonate succession in the Yavca area (Bolkar Mountains, S Turkey): biostratigraphy and paleoenvironments, Geobios, 39, 521–633, 2006.
Tomašov\'{y}ch, A., Fürsich, F. T., and Olszewski, T. D.: Modeling shelliness and alteration in shell beds: variation in hardpart input and burial rates leads to opposing predictions, Paleobiology, 32, 278–298, 2006.
van Buchem, F. S. P., Pittet, B., Hillgärtner, H., Grötsch, J., Al Mansouri, A. I., Billing, I. M., Droste, H. H. J., Oterdoom, W. H., and van Steenwinkel, M.: High-resolution sequence stratigraphic architecture of Barremian/Aptian carbonate systems in northern Oman and the United Arab Emirates (Kharaib and Shu'aiba Formations), GeoArabia, 7, 461–501, 2002.
Varol, B., Altiner, D., and Okan, Y.: Dasycladacean algae from the Mesozoic carbonate facies of the Sariz-Tufanbeyli autochthon (Kayseri, SE Turkey), Mineral Res. Expl. Bull., 108, 49–56, 1988.
Velić, I.: Stratigraphy and palaeobiogeography of Mesozoic benthic foraminifera of the Karst Dinarides (SE Europa), Geol. Croat., 60, 1–113, 2007.
Vezzani, L., Festa, A., and Ghisetti, F. C.: Geology and tectonic evolution of the Central-Southern Apennines, Italy, Geol. Soc. Am., Spec. Pap., 469, 1–58, 2010.
Vilas, L., Masse, J. P., and Arias, C.: Orbitolina episodes in carbonate platform evolution: the early Aptian model from SE Spain, Palaeogeogr. Palaeoclimatol. Palaeoecol., 119, 35–45, 1995.
Vincent, B., van Buchem, F. S. P., Bulot, L. G., Immenhauser, A., Caron, M., Baghbani, D., and Huc, A. Y.: Carbon-isotope stratigraphy, biostratigraphy and organic matter distribution in the Aptian–Lower Albian successions of southwest Iran (Dariyan and Kazhdumi formations), GeoArabia, Spec. Pub., 4, 139–197, 2010.
Vlahović, I., Tišljar, J., Velić, I., Matičec, D., Skelton, P. W., Korbar, T., and Fuček, L.: Main events recorded in the sedimentary succession of the Adriatic Carbonate Platform from the Oxfordian to the Upper Santonian in Istria (Croatia), in: Evolution of Depositional Environments from the Palaeozoic to the Quaternary in the Karst Dinarides and the Pannonian Basin, Field Trip Guidebook, edited by: Vlahović, I. and Tišljar, J., 22nd Int. Assoc. Sedimentol., 19–56, 2003.
Wang, P. X.: Global monsoon in a geological perspective, Chin. Sci. Bull., 54, 1113–1136, 2009.
Weissert, H. and Erba, E.: Volcanism, CO2 and palaeoclimate: a Late Jurassic–Early Cretaceous carbon and oxygen isotope record, J. Geol. Soc. Lond., 161, 695–702, 2004.
Weissert, H. and Lini, A.: Ice age interludes during the time of Cretaceous Greenhouse Climate?, in: Controversies in Modern Geology, edited by: Muller, D. W., McKenzie, J. A., and Weissert, H., Academic Press, 173–191, 1991.
Weissert, H., Lini, A., Föllmi, K. B., and Kuhn, O.: Correlation of Early Cretaceous carbon isotope stratigraphy and platform drowning events: a possible link?, Palaeogeogr., Palaeoclimatol., Palaeoecol., 137, 189–203, 1998.
Whalen, M. T., Day, J., Eberli, G. P., and Homewood, P. W.: Microbial carbonates as indicators of environmental change and biotic crises in carbonate systems: examples from the Late Devonian, Alberta basin, Canada, Palaeogeogr. Palaeoclimatol. Palaeoecol., 181, 127–151, 2002.
Wilson, J. L. and Jordan, C.: Middle Shelf Environment, in: Carbonate Depositional Environments, edited by: Scholle, P. A., Bebout, D. G., and Moore, C. H., Am. Assoc. Pet. Geol., Mem., 33, 297–344, 1983.
Wissler, L., Weissert, H., Buonocunto, F. P., Ferreri, V., and D'Argenio, B.: Calibration of the Early Cretaceous Time Scale: a combined chemostratigraphic and cyclostratigraphic approach to the Barremian–Aptian interval, Campania Apennines and Southern Alps (Italy), in: Cyclostratigraphy; approaches and cases histories, edited by: D'Argenio, B., Fischer, A. G., Premoli Silva, I., Weissert, H., and Ferreri, V., SEPM Spec. Publ., 81, 123–133, 2004.
Wortmann, U. G., Hesse, R., and Zacher, W.: Major-element analysis of cyclic black shales: Paleoceanographic implications for the Early Cretaceous deep western Tethys, Paleoceanography, 14, 525–541, 1999.
Wortmann, U. G., Herrle, J. O., and Weissert, H.: Altered carbon cycling and coupled changes in Early Cretaceous weathering patterns: Evidence from integrated carbon isotope and sandstone records of the western Tethys, Earth Plan. Sci. Lett., 220, 69–82, 2004.
Zappaterra, E.: Source-rock distribution model of the Periadriatic Region, AAPG Bull., 78, 333–354, 1994.