D. Violanti

Evolution of the Messinian Mediterranean environments: the Tripoli Formation at Capodarso (Sicily, Italy)

Abstract New field data have been collected from the Capodarso section (Caltanissetta basin, Sicily); 48 samples from the Tripoli Formation were analysed for foraminifera, dinocysts, palynofacies, CaCO 3 , pollen grains and clay minerals. The uppermost clays of the Terravecchia Formation are clearly the result of deeper deposition than those corresponding to the lowermost analysed samples within the overlying Tripoli Formation. So, the general evolution of the basin was from normal marine conditions to confinement, during which the sedimentation of diatomite vs. clay was mainly controlled by relative sea-level changes. Three successive types of processes are considered to have generated the diatomites: 1. (1) in the lower part of the section, the sea level was relatively high and deposition of diatomites was aided by sea-level rises of unequal importance and variations of continental precipitations and run-off; 2. (2) then, relatively minor sea-level oscillations prevailed; however, the second part of the sequence is characterized by a generally strong shallowing trend leading to basin confinement; 3. (3) the explanation for diatomites during the last member does not rely as much on the occurrence of substantial sea-level rises in an increasingly desiccated basin; on the other hand, an increased number of rivers reached the central area of the basin, which helped to produce the youngest diatomites. The warm (subtropical to tropical) and xeric climate predisposed to such an evolution, inducing continuous high salt-concentration of marine waters; so, the smallest influx of less saline (oceanic) waters and/or continental freshwater (run-off) could produce water-mass stratification and diatomite deposition. However, not all lithologic breaks are likely to correspond to recorded environmental transitions. Bio- and magnetostratigraphy of the section allow consistent relationships between the sea-level curve at Capodarso and the δ 18 O curve at Site 588 (southwest Pacific), attesting global eustatic control on the sedimentation of the Caltanissetta basin up to the beginning of the Messinian salinity crisis.

Morphogroup analysis of agglutinated foraminifers off Terra Nova Bay, Antarctica, Expedition 1987/1988.

Statistical analyses of benthic agglutinated foraminifers from surface sediments off Terra Nova Bay (Ross Sea, Antarctica), collected during the 1987–1988 expedition (PNRA), are presented here. Percentage variations of epifaunal and infaunal morphogroups and a Q-mode analysis indicate that almost all the foraminiferal assemblages are dominated by epifaunal to interstitial small Portatrochammina antartica. Infaunal milioline-shaped Miliammina earlandi is dominant only in a nearshore area. Redepositional processes seem only in part reflected by the distribution of agglutinated tests. Only the extremely high percentages of small trochamminids, probably resuspended in the water column, and of the stout miliamminids may be related to winnowed sediments. Infaunal cylindrical (Nodulina, Reophax) and milioline-shaped (Miliammina) morphotypes are frequent on the inner shelf and slopes of the banks and are inferred to be mobile forms, well adapted to unstable bottoms. The flattened tapered Pseudobolivina antarctica seems positively correlated with increasing depth, and suggests oxygen-depleted muds and a sluggish circulation in the deep Drygalski Basin. All the dominant morphotypes (trochamminids, hormosinids, Miliammina earlandi and Pseudobolivina antarctica) are inferred to be opportunists, able to inhabit different micro-habitats and exploit various feeding resources.

Stress tolerant microfossils of a Messinian succession from the northern Mediterranean basin (Pollenzo section, Piedmont, Northwestern Italy)

High resolution quantitative data on calcareous nannofossil and foraminifer assemblages of the upper part of the Pollenzo section (Alba, Piedmont, northwestern Italy) are discussed in order to investigate the palaeoenvironmental evolution within the time interval immediately preceding the Messinian Salinity Crisis (MSC) and coeval to its onset. The studied succession, measuring approximately 24 m in thickness, consists of the seven uppermost cycles (Pm1-Pm7) of the Sant’Agata Fossili Marls. The latter are characterized by euxinic shale/ marl couplets that include a distinct carbonate-rich bed. Cyclical, orbitally controlled, fluctuations of warm/oligotrophic and temperate/ mesotrophic conditions are documented in the lower cycles Pm1-Pm4 on the basis of opposite abundances of planktonic microfossils. An increasingly stressed palaeoenvironment is recorded from cycle Pm5 upward by the higher abundance of stress tolerant taxa among the calcareous nannofossils (Reticulofenestra spp., Sphenolithus abies, Helicosphaera carteri, Umbilicosphaera rotula, and Rhabdosphaera procera), planktonic (Turborotalita quinqueloba) and benthic foraminifers (Bolivina spp., Bulimina echinata, and Cassidulina crassa). These data support the onset of the MSC within the time interval of the deposition of cycle Pm5. Small size planktonic foraminifers survived up to the lower part of cycle Pm7 while the more resistant calcareous nannofossils survive up to the upper part of cycle Pm7, positioned a few metres below the first gypsum bed (cycle Pg1). Micropalaeontological events (last peaks of Turborotalita multiloba and Orbulina universa, peak of S. abies) allow correlation of the lower Pm1-Pm4 cycles of the Pollenzo section with the upper cycles of the pre-evaporitic Mediterranean succession. RIASSUNTO [Microfossili tolleranti condizioni di stress ambientale del Messiniano pre-evaporitico di Pollenzo (Piemonte, Italia nordoccidentale] In questo studio vengono analizzati nuovi dati quantitativi sulle associazioni messiniane a foraminiferi e nannofossili calcarei della parte superiore delle Marne di Santa Agata Fossili nella sezione di Pollenzo (Alba, Piemonte, Italia nord-occidentale), costituita da alternanze cicliche di peliti laminate e di marne omogenee. Nell’intervallo studiato sono presenti anche livelli carbonatici cementati, e le associazioni diventano progressivamente impoverite, fino a scomparire a circa 1.5 m al di sotto del primo livello di gessi primari. Lo studio quantitativo ad alta risoluzione dei foraminiferi è stato condotto sui residui >125 μm e tra 63-125 μm. Nelle alternanze di peliti laminate e marne è stata evidenziata una iniziale ciclicità nelle variazioni percentuali dei microfossili calcarei. Le associazioni diventano poi dominate da taxa tolleranti condizioni di stress ambientale. Tra i nannofossili calcarei, taxa indicativi di condizioni fortemente eutrofiche e/o a salinità variabile sono rappresentati da Reticulofenestra spp., Helicosphaera carteri, Umbilicosphaera rotula e Rhabdosphaera procera, tra i foraminiferi da Turborotalita quinqueloba, Bulimina echinata, Cassidulina crassa e Bolivina spp. Drastici cambiamenti nelle associazioni a foraminiferi caratterizzano i cicli Pm4 e Pm5: scomparsa di esemplari e taxa >250 μm e >125 μm, impoverimento generale delle associazioni, aumento percentuale di C. crassa, Eponides cf. tumidulus, tipici di fondali ricchi di fitodetrito. Condizioni ambientali estremamente instabili e/o di stress sono inoltre suggerite dalle alte percentuali dei nannofossili calcarei Sphenolithus abies e di piccole Reticulofenestra spp. Foraminiferi planctonici (T. quinqueloba) di piccole dimensioni (<125 μm) sono presenti fino alla parte inferiore del ciclo Pm7, pochi metri al di sotto del primo banco di gessi (ciclo Pg1). I nannofossili calcarei risultano un poco più resistenti, sopravvivendo fino alla parte sommitale del ciclo Pm7. Gli ultimi picchi di abbondanza di Turborotalita multiloba e Orbulina universa nei cicli Pm1-Pm4 ed il picco d’abbondanza di S. abies alla base del ciclo Pm5 permettono la correlazione con i cicli sommitali della successione pre-evaporitica messiniana dell’area Mediterranea. Bollettino della Società Paleontologica Italiana, 52 (1), 2013 46 at basin margins, by primary sulphate evaporites of the Primary Lower Gypsum unit, representing here the Vena del Gesso Formation (Dela Pierre et al., 2011). In situ primary evaporites are not documented in the depocentral zones, but seismic data show that their time equivalent sediments are represented by shales (Irace et al., 2010). The transition between the shallow marginal area and the buried depocentre is exposed on the southern sector of the Piedmont Basin (Alba region) and was reconstructed in detail along a SW-NE transect. On the southern basin margins six Primary Lower Gypsum (PLG) cycles were recognised, composed of bottom grown-selenite layers; the sixth bed represents a distinct marker bed referred to as the Sturani Key-Bed (SKB) (Dela Pierre et al., 2011) and correlatable to the 6th PLG cycle (dated to about 5.84 Ma) (Lugli et al., 2010). Moving towards the NE (i.e., towards the depocentral zone), and in the Pollenzo section, only two gypsum beds are present below the SKB. They overlie a cyclical succession of euxinic shales, marls and carbonate-rich beds belonging to the Sant’Agata Fossili Marls. Because of their position with respect to the SKB, the uppermost three shales and marls cycles must be considered as the deeper water equivalent of the lower cycles of the PLG unit deposited in marginal setting (Dela Pierre et al., 2011). In the Pollenzo section, a thick slumped interval divides the Sant’Agata Fossili Marls into two portions. In the lower one, seven cycles were recognised; in the upper portion, above the slump, seven cycles (Pm1-Pm7) were recorded, each one including a distinct carbonate-rich bed. According to physical-stratigraphic position (with respect to the North of the Gello, Fanantello, Monte del Casino and Trave sections from central Italy (Negri et al., 1999; Manzi et al., 2007; Iaccarino et al., 2008; Roveri et al., 2008; Di Stefano et al., 2010), at latitude around 43° N. Recent studies in the area focused on the succession cropping out along the Tanaro River, near Alba (Lozar et al., 2010; Dela Pierre et al., 2011, 2012). This comprises the pre-MSC sediments, and overlying deposits, which testify the three stages of the MSC (Roveri et al., 2008), and evidence the lateral facies transition between marginal and distal settings. In the Pollenzo section the marine deposits, pertaining to the Sant’Agata Fossili Marls, are well exposed, separated in a lower and an upper interval by a thick slumped portion. Previously cited studies evidenced a precession-driven cyclicity, more evident in the interval overlying the slump, on the basis of lithological, petrographic, geochemical and micropalaeontological analyses. The upper part of the Sant’Agata Fossili Marls is overlain by the first local gypsum-bearing cycle, correlated to the 4th cycle of the Primary Lower Gypsum unit deposited in the marginal sector of the Messinian basin (Dela Pierre et al., 2011). Preliminary semiquantitative micropalaeontological analyses recorded very impoverished assemblages in the upper Sant’Agata Fossili Marls, dated to the calcareous nannofossil Zone MNN11b/c (Raffi et al., 2003) on the basis of Amaurolithus delicatus occurrence and to the foraminifer Non Distinctive Zone (Iaccarino, 1985) or to the Zone MMi13c (Lourens et al., 2004) on the basis of the occurrence of T. multiloba, of dominantly dextral coiling N. acostaensis and of Bulimina echinata (Lozar et al., 2010). A more detailed study of the sediments above the slump is here presented, in order to better understand the basin evolution in the time interval immediately preceding the MSC and coeval to its onset. A high resolution sampling and quantitative micropalaeontological analyses were performed on calcareous nannofossil and >125μm and 63-125μm foraminiferal assemblages. This procedure evidenced a cyclicity in the lowermost assemblages and a wider than expected foraminifer occurrence before the onset of the gypsum deposition as well as the importance of small planktonic and benthic taxa for the reconstruction of palaeoenvironmental changes. GEOLOGIC AND STRATIGRAPHIC SETTING During the Messinian, the TPB corresponded to a wide wedge top basin, developed above Alpine, Ligurian and Adria basement units (Rossi et al., 2009). The shallow marginal zones of the Messinian basin are presently exposed in the northern (Torino Hill and Monferrato) and southern (Langhe) sectors of the TPB, whereas the depocentral zones are buried below Pliocene and Quaternary sediments (Savigliano and Alessandria basins) (Fig. 1). The succession begins with deep water marine muddy sediments referred to as the Sant’Agata Fossili Marls (Tortonian-Lower Messinian) that record progressively more restricted conditions heralding the onset of the MSC (Sturani, 1978). This unit displays a precession-related cyclic stacking pattern, given by the repetition of euxinic shale/marl couplets and is followed, Fig. 1 Structural sketch of NW Italy (modified from Bigi et al., 1990). The arrow shows the location of the Pollenzo section. AM: Alto Monferrato; BG: Borbera-Grue; IL: Insubric Line; MO: Monferrato; TPB: Tertiary Piedmont Basin; TH: Torino Hill; SVZ: Sestri-Voltaggio zone. 47 D. Violanti et alii Stress-tolerant Messinian microfossils in NW Italy sample and by the Fisher’s diversity index (α) which takes into account the number of taxa as well as the number of specimens for each sample, using PAST ver. 1.77 (Hammer et al., 2008). Qualitative analyses were also carried out on the 45-63 μm fraction. The studied material is housed at the Museo di Geologia e Paleontologia dell’Università di Torino under repository numbers MGPT-PU134019 to MGPTPU134084.

Virtual Tours Through Earth’s History and Palaeoclimate: Examples from the Piemonte (Northwestern Italy) Geoheritage (PROGEO-Piemonte Project)

A project developing virtual tours on the geoheritage of Piemonte aims to disseminate geological knowledge to the general public. Two of the most crucial geological themes, geological time and climatic and environmental change, are addressed. People will increase their awareness of Earth’s geodiversity and of the potential of Earth Sciences to improve our everyday lives. The tours will be developed with special attention to educational purposes and in lay language, and will also contribute to preserving vulnerable geoheritage.

The northernmost record of the Messinian salinity crisis (Piedmont basin, Italy)

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Multimedia and Virtual Reality for Imaging the Climate and Environment Changes Through Earth History: Examples from the Piemonte (NW Italy) Geoheritage (PROGEO-Piemonte Project)

The dissemination of the knowledge of critical geological issues, such as past environmental and climate change and their correct placement in the geological time scale, is essential to rise the awareness of the huge potential impact of the Earth Sciences on the current and future generations. We selected two examples (the Marguareis and the Langhe and Monferrato areas) to disseminate these topics to a broad audience. Virtual tours, hosted on the PROGEO-Piemonte project website (www.progeopiemonte.it), have been developed with special care to educational purposes and made suitable for mobile devices. These allow us to overcome theoretical problems related to the complexity of geological items (spatial and evolutionary complexity, deep time dimension), with plain language explanations, detailed pictures and dynamic 3D models. The virtual visit overcomes practical difficulties, such as restricted access to high mountain or dangerous areas, and improves the access to detailed geological information at different scales, not readily available in the outcropping rocks. Dynamic or static information, stored on the website, are available on Google Earth or Google Maps in the field (mobile navigation) or at home (PC-based navigation). The virtual tours thus become an alternative to the visit on site, or a tool for deepening knowledge before or after the visit. This is especially helpful for schools, because virtual tours could be used in classroom with many different goals. The virtual tours, once accessed on-line by many visitors, will in turn push public administrators to realize geotouristic facilities on site and fund educational projects on these important issues.