<^G9-A? 2: A* ISSN 0366-2047 BOLLETTINO DELLA SOCIETÀ DEI NATURALISTI IN NAPOLI VOLUME CI - 1992/1993 GIANNINI EDITORE NAPOLI 1994 ISSN 0366-2047 BOLLETTINO DELLA SOCIETÀ DEI NATURALISTI IN NAPOLI VOLUME CI - 1992/1993 GIANNINI EDITORE NAPOLI 1994 SOCIETÀ DEI NATURALISTI IN NAPOLI VIA MEZZOCANNONE, 8 CONSIGLIO DIRETTIVO BIENNIO 1992-93 Prof. Aldo Napoletano Prof. Oreste Schettino Prof. Teresa De Cunzo Dott. Maria Carmela Del Re Prof. Eugenio Piscopo Prof. Amalia Tavernier Prof. Vincenzo Cutillo Prof. Pietro Battaglini Prof. Giuseppe Caputo Prof. Gennaro Corrado Prof. Enrico Franco - Presidente - Vice-Presidente - Segretario - Vice-Segretario - Tesoriere - Bibliotecario - Redattore delle Pubblicazioni - Consigliere - Consigliere - Consigliere - Consigliere BOLLETTINO DELLA SOCIETÀ DEI NATURALISTI IN NAPOLI Comitato editoriale Claudio Agnisola Filippo Barattolo Pietro Battaglini Giuseppe Caputo Graziano Fiorito Enrico Franco Vincenzo Cutillo - Redattore delle pubblicazioni INDICE Fiume M. Giovanna - Gravimetrie study of Phlegrean Fields Caldera: Mount of Cuma - Archiaverno area . . pag. 5 Buonomo P„ Mirabella P„ de Filippo G., Milone M. - First report on thè fauna of Tammaro valley . . . . » 15 Soppelsa O., Battaglini F., Battaglini P. - Recent faunistic and ecotoxi- cological arrangement of thè terminal tract of thè Sarno river (Campania, Italy) . . » 29 Fimiani P., Digilio M.C., Bionomics of Myopites stylata F. (Diptera, Tephritidae) and its naturai enemies in Vivara island (Gulf of Naples) . . . » 53 Avallone B., Balsamo G., Marmo F. - Immunocytochemistry of carbonic anhydrase in thè chick embryo membranous labyrinth during development ............................................... » 63 Esposito V., De Girolamo P., Sammarco M., Gargiulo G. - Ocurrence of (Tendorphin- and enkephalin-like immunoreactivity in thè hy- pothalamus of thè domestic fowls, Gallus domesticus . » 73 Battaglini P., Soppelsa O., Improta C., Ferrara L. - Action of thè cad- mium on thè Carassius auratus living in lentie waters containing catabolic ammonia . . » 89 Andreozzi G , Antonucci R., Affatato C, De Girolamo P., Gargiulo G., Ferrara L„ Sammarco M., Battaglini P. - Catabolic NH3 influence on cadmium toxicity to thè gut of Carassius auratus L. . . » 105 CONTRIBUTI IN ITALIANO Barbera C, Leuci G., Rapuano M., Virgili A. - Mammiferi olocenici provenienti da uno scavo effettuato nell'isola di Capri (Italia meridionale) ................................................ » 123 A. Vallario - Il Dissesto Idrogeologico . » 141 Boll Soc . Natur . Napoli - Voi. 101 (1992-1993): hi Gravimetrie study of Phlegrean Fields Caldera: Mount of Cuma - Archiaverno area M. Giovanna Fiume Dipartimento di Geofìsica e Vulcanologia, Università degli Studi «Federico II», L.go S. Marcellino 10, Napoli, Italy Key words: Gravity, Phlegrean Fields, Caldera. Abstract. Purpose of this paper is thè geophysical characterization of thè under¬ ground structure of a particular area of thè volcanic Phlegrean district: Mount of Cuma and thè adjacent area of Archiaverno. New microgravimetric data, measured along a profile Crossing W to E thè Phlegrean area and passing nearby thè Cuma and thè Archiaverno lake, were obtained and interpreted. Additionallv, in order to get more information, thè latest aeromagnetic data of these areas were digitized. All thè information arising from this kind of study allowed thè structural knowledge of a very complex area to be increased. In fact, thè hypotheses about thè dimension and thè event leading to thè formation of thè calderic structure connected to thè Phlegrean Fields volcanic district, are stili various and debated. Riassunto. Studio Gravimetrico della Caldera dei Campi Flegrei: area del monte Cuma-Archiaverno. Nell’area dei Campi Flegrei sono stati acquisiti nuovi dati microgravimetrici di dettaglio lungo un profilo che parte dall’area di M. di Cuma ed arriva fino a Pozzuoli. Dopo la fase di correzione ed elaborazione dei dati rilevati, sono state analizzate ed interpretate, da un punto di vista strutturale, le aree M. di Cuma e dell’Archiaverno caratterizzate dalla presenza di due anomalie gravimetriche positive. Il modello scaturito da tale interpretazione ipotizza la presenza di un doppio ribassamento strutturale al di sotto delle aree in questione. Introduction The Phlegrean area is located inside thè Piana Campana graben, west of Naples and is roughly 70 square kilometers wide (Fig. 1). This depressed structure formed on thè western edge of thè Appenninic chain since thè Upper Pliocene, probably in association with thè opening of thè Tyrrhenian sea. The Phlegrean Fields volcanic complex, together with Ischia and Received 14.5.92, accepted 8.2.93 Precida, represents a complicated voi carne System formed by a mainly pyroclastic monogenie group of small volcanoes lined up in an east-west direction. They fed an activity characterized by potassio chemism (Di Girolamo et al., 1984). Figure 1 - Location of Campi Flegrei The majority of thè present produets are pyroclastic in nature; lava fio ws and domes are very scanty. The distribution of thè ejected volumes in relation to thè age, indicates that thè activity has migrated towards thè inner part of thè caldera, characterized by decreasing parossistic phases. The explosive Phlegrean activity is characterized by water-rnagma intera/: tion. Events without hydromagmatic components are extremely rare. The most common produets are alcaline trachytes which represent thè final produci of thè low content potassium series. They are thè produets of recrystallization processes which happened in a relatively small-depth environment ’ M. Giovanna Fiume Description of Cuma-Archiaverno area In thè Mount of Cuma area a small isolateci hill is present, which emerges from thè plain between thè sea and thè Occidental hills of thè Archiaverno-Averno System (Fig. 2). The hill is made of a partially outcrop- ping trachytic lavic dome (>0.01 m.y.) covered either by old products or by more recent products. Such a dome is intensely fractured, even if particularly important faults or fractures could not be pointed out This kind of stratigraphic sequence is also found in other areas located at thè edges of thè volcanic Phlegrean district. AB GRAVIMETRI PROFILE Figure 2 - Location of stratigraphic section 8 Boll. Soc . Natur. Napoli - Voi 101 (1992-1993) Fig. 2 shows thè stratigraphic section of Mount of Curo a and of another fringe area which more or less have thè same stratigraphyc and structural characteristic (Marmolite). East of this structure there is a younger feature (Archiaverno) (0.01 m. y.) made of vellow tuff. It is made up of an almost concentric rise at thè Averno. This rise was interpreted by De Lorenzo ( 1 904) as thè evidence of a crater bigger than thè Averno crater. The rest of these apparatus is represented by thè mount of Ginestra and thè northern portion of thè Averno lake. The remaining portion was probably reduced by tettonic collapses and was morphologically mo difi ed on thè south-west and south-east sides by thè Baia, Fondi di Baia and Mount Nuovo volca- noes. The Phlegrean Fields Caldera The presence of a collapsed structure connected to thè Phlegrean Fields is known either by geological and volcanological observation at thè surface and by thè analysis of geophysical data. Many and sometimes contrasting theories exist about thè limits of this collapse and thè genera- ting event. About thè first hypothesis we recali Rittmann (1950) which hypothesizes thè formation of thè Phlegrean caldera as due to thè parossi- stic eruption of thè Campanian grey tuff which would have caused thè collapse of thè presumed stratovulcano called Archiflegreo. Later, Di Girolamo (1970); Barberi et al. (1978) supposed that thè formation of thè Campanian Ignimbrite (Campanian grey tuff) was due to a series of eruptions happening along thè fractures located north of thè Phlegrean Fields. These eruptions caused thè collapse of a vast area of thè Phlegrean Fields and a portion of thè bay of Naples. Rosi et al. (1983); Rosi and Sbrana (1987), partially accepting thè Rittman's hypotesis, recognized thè line formed by M. of Precida, Cuma, S. Severino, Marmolite, Camaldoli as thè edge of thè Phlegrean caldera, caused by thè collapse of a magmatic chamber after thè eruption of thè Campanian Ignimbrite. It must be said that clear geological signs which may confirm thè existence of a “step” due to thè caldera edge are not recognizable, at least not morphologically. Finally, based on thè latest studies, Lirer et al. (1987) hypothesized that thè formation of thè Phlegrean caldera was due to another big eruption (Neapolitan Yellow Tuff). According to this study, after thè emplacement of thè yellow tuff, a collapse of thè centrai part of thè Phlegrean Fields arised. The yellow tuff remained only on thè edges because there they were supported by older M. Giovanna Fiume 9 volcanic structures. Such a collapse would be limited by faults having Appenninic and Antiappenninic direction, which in turn would become thè place for other new activity (Capo Miseri o- Porto Miseno-BacolbPunta Epitaffio-Archiaverno) . This hypothesis was recently revaluated by Scando- ne et al. (1991), Fedi et al. (1991). They, interpreted thè caldera collapse as less extended than thè previous hypothesis (Rittmann, 1950; Rosi & Sbrana, 1987) and considered M. of Procida, Cuma, S. Severino, Marmoli- te, Camaldoli areas, not as thè caldera edge, but as completely outside thè caldera. Geographical data As previously mentioned, thè presence of a large gravity low (Fig. 3), thè interpretation of thè other geophysical data and thè drilling data (Cassano & La Torre, 1987; Fedi et al., 1991) make probable a collapse in thè Pozzuoli bay. Figure 3 - Campi Flegrei gravity anomaly (Agip, 1987). Contour intervals 1 mGal 10 Boll Soc . Natur. Napoli - Voi 101 ( 1992-1993 ) The analysis of thè samples taken from this drilìings, points out intense phenomena of compactation and hydrothermal reactions which, due to thè increasing of thè tuff and tufites density, makes thè gravimetrie interpreta- tion difficult. As a matter of fact, these phenomena strongly decreased thè density contrast among thè various lithotypes. All this points out a very complicated situation and thè difficulty to draw a density model, either because of thè several, rapid succession of events and because of thè high temperature. Furthermore, thè effeets related to thè high temperature on thè volcanic rocks are particularly supported by thè analysis of magnetic data (Nunziata & Rapolla 1 98 1 ; Agip, 1987). This because of phenomena of demagnetization due to recent or past circulation of hot waters. Such a phenomenon, pointed out in thè M. of Cuma-Archiaverno areas too, causes a very scant correlation between magnetic and gravimetrie anomalies (Fig. 4). Gravimetri study of thè Phlegrean Caldera Gravimetrie data acquisitori New detailed microgravimetric data along profiles were collected in thè studied area (Fiume, 1991) in order to study thè medium to shallow 26 MGAL . PinOCLASTIC DEPOSITS (<8000B.P. ) 2.5 Km PRODUCTS OF AVERNO ERUPTION GAVRO YELLOW TUFF PRE-CALDERA ACTIVITY Figure 4 - Gravimetrie profile (new data) and magnetometric profile (Agip, 1970) M. Giovanna Fiume 11 depth structures. A D-type La Coste microgravimeter was utilized during thè fìeld study phase. Distances between stations were 50 m. on overage. Gravity values were referred to thè Capodimonte main gravity vaine (Cannizzo et al, 1978). In particular, in order to calculate thè Bouguer anomaly, a density vaine of 1.4 g/cmc was utilized according to thè data of thè shallow wells existing in thè area (Ducei & Rippa, 1988). The analized profile, shown on Fig. 4a, begins from Mount of Cuma-Archiaverno area and ends at Pozzuoli area, Crossing thè caldera in an cast to west direction; along this profile it is possible to recognize a negative gravity trend of thè intermediate frequency band which starts from thè Averno area and reaches thè minimum values to wards thè Pozzuoli bay. Various filterings were performed, in order to separate thè deep contributes from thè more shallow ones. A cut-off wavelength of 5 km was chosen to separate thè caldera contributes from thè shallover ones (Fig. 5). Figure 5 - Gravimetrie filtered profile (M. Cuma-Fuorigrotta) 12 Boll ' %c. Ator, Napoli - F# 101 f!992:Ì995j Interpretation of thè data A quantitative analysis was performed on thè above mentioned resi- dual profilo in thè Mount of Cu m a- Are hiavern o area. As can be seen on Fig. 4 a these two areas, which are chronologically and volcanologically different, are characterized by thè presence of two gravimetrie highs having slightly different amplitudes. Given thè presence of an outerop (frorn 5rn up to 40 rn. to sea-level) of thè trachytic structure, was hypotesi- zed a simple two layer density model constrained on thè surface by thè outeropping points of thè trachytic structure (Mount of Cuma). The utìlized density for thè trachytic sequence is 2.5 g/cmc. The density attributed to thè upper pyroclastics was 1.8 g/cmc. The suggested quantita¬ tive model, obtained by a 2D inversion program is repori. ed on Fig. 6. The Àgip aeromagnetic data of thè Mount of Cuma area were digitized toc, along a n or t -south profile (Agip, 1987), in order to attempt a correlation between thè two sets of geophysical data, as reported on Fig. 4b. Results As already stated above, mount of Cuma area, together with S. Severi¬ no, Marmolite, Camaldoli, M. of Procida represent in some Authors' opinion a border area of thè Phlegrean caldera (Rittmann, 1950; Rosi & Sbrana, 1987; hypothesis A). More recent studies on thè contrary, (Di Girolamo et ah 1984; Lirer et ah 1987; Scandone et ah 1991) hypothesize thè above mentioned areas to be completely uninvolved zones in thè collapse (hypothesis B). The quantitative model shown on Fig. 6, points out thè presence of a high density shallow structure, lowering toward thè Averne lake area. A kind of doublé depression results in this area between M. of Cuma and thè Archiaverno and between this structure and Averno lake. Regarding thè densities utilized in thè stmctural model, thè 2.5 g/cmc value of thè dense layer could be everywhere representative of one kind of lava. As said, this is contrained only dose to M. of Cuma where, it is possible to recognize thè trachytic mass in thè outerop. Regarding thè rest of thè model, thè utilized density could be associated even with compacted and alterated pyroclastic materials due to old or recent circulation of underground waters. M. Giovanna Fiume 13 From a structural point of view, thè limit of thè first depression coincides at thè surface with thè inner edge of Mount of Cuma. In this kind of structure it is possibile to recognize thè hypothesis A. The hypothesis B instead associates thè formation of thè caldera with thè Neapolitan Yellow Tuff eruption. In this case thè limits of thè collapse in question would be more internai, and in particular recognizable with thè Capo Miseno-Baco- li-Punta Epitaffio-Archiaverno volcanic line. The model proposed in thè study would even explain thè second depression dose to thè Archiaverno- Averno lake, as shown on Fig. 6. Briefly, this structural model (Fig. 6) could be justified by thè succession of thè two above stated eruptions. These eruptions in tura caused thè emptyng of thè magmatic chamber which would be thè cause of thè formation of thè two calderic collapses. Boll Soc . Natur. Napoli - Voi 101 ( 1992-1993 ) REFERENCES Agip, 1987. Campi Flegrei- Permesso Lago Patria: aggiornamento del modello geofìsico. In Rapp. Int. MESG/IMPO . Barberi, F., F. Innocenti, L. Lirer, R. Munno, T.S. Pescatore, & R. Santacroce, 1978. The Campanian Ignimbrite: a major prehistoric eruption in thè Neapoli- tan area (Italy). Bull Volcanol. , 41: 1-22. Cannizzo, L., G. Cerutti, I. Marson, 1987. Absolute gravity measurements in Eurip. Il nuovo Cimento , le, n° 1. Cassano, E. & P. Torre, 1987. Geophysics. In: Rosi M. and Sbrana A. (Editors), Phlegrean Fields. CNR. Quad. Rie; Sci., 114: 103-133. De Lorenzo, G., 1904. L’attività vulcanica dei Campi Flegrei. Rend. Acc. Sci . Fis. Mat. Napoli, 10: 203-221. Di Girolamo, P., 1970. Differenziazione gravitativa e curve isochimiche nell’Ignim- brite Campana. Rend. Soc. Ital Minerai Petrog. , 26: 547-588. Di Girolamo, P., M.R. Ghiara, L. Lirer, R. Munno, G. Rolandi & D. Stanzione, 1984. Vulcanologia e petrologia dei Campi Flegrei. Boll Soc. Geol. lt., 103: 349-413. Fedi, M., C. Nunziata, A. Ra polla, 1991. The Campanian Campi flegrei area: a contribution to discern thè best structural model from gravity interpretation. J. Volc. Geotherm. Res., 48:51-59. Ducei, D. & F. Rippa, 1988. Banca dati sul sottosuolo di Pozzuoli. In Atti Conv. “Bradisismo e Fenomeni Connessi" . Napoli, 1988. Fiume, M.G., 1990. Modellizzazione geofìsica delle strutture superficiali e profonde del distretto vulcanico Flegreo. Tesi Dottorato di ricerca, Dipartimento di Geofìsica e Vulcanologia, Università «Federico II», Napoli. Lirer, L., G. Luongo, & R. Scandone, 1987. On thè volcanological evolution of Campi Flegrei. EOS, Trans. Am. Geophis. Union, 68: 226-234. Nunziata, C. & A. Rapolla, 1981. Interpretation of gravity and magnetic data in thè Phegrean Fields Geothermal Area, Naples, Italy. J. Volcanol Geotherms. Res., 10: 209-226. Rittmann, A., 1950. Sintesi geologica dei Campi Flegrei. Boll. Soc. Geol. Ital, 69: 117-128. Scandone, R., 1991. The structure of thè Campanian Plain and thè activity of thè Neapolitan volcanoes. J. Volcanol. Geotherm. Res., 48: 1-31. Rosi, M. & A. Sbrana (Editors), 1987. Phlegrean Fields. CNR. Quad. Rie; Sci., 114: 175. Rosi M., A. Sbrana & C. Principe, 1983. The Phlegrean Fields structural evolution, volcanic history and eruptive mechanisms. J. Volcanol Geotherm. Res., 17: 273-288. Boll Soc. Natur. Napoli - Voi 101 (1992-1993): 15-27 First report on thè fauna of Tammaro valley Buon omo P.1, Mirabella P.2, de Filippo G.\ Milone M.2 ' Studi di Ecologia Applicata, via Caravaggio 143Y, 80126, Napoli, Italv 2 Dipartimento di Zoologia, Università degli Studi «Federico II» di Napoli, via Mezzocannone 8, 80126 Napoli, Italv Key words: Mammals, birds, macrobenthos, butterflies, Tammaro river. Summary. Faunistic researches have been carried out along Tammaro river from 1984 to 1991, in relation to a wider programme for thè environmental monitoring. Mammals, Birds, fresh water Macrobenthofauna and Lepidoptera Rhopalocera have been studied and thè first results are here reported. We have found 12 species of Mammals and 66 of Birds (18 are resident and breeding, 39 only breeding, 47 migrant, 32 wintering, 3 non breeding summer visitors). As regards thè Macrobenthofauna we have found 5 genera of Plecoptera, 6 families of Trichoptera, 1 1 genera of Ephemeroptera, 5 families of Coleoptera, 6 genera of Odonata, 5 families of Diptera, 2 genera of Heteroptera, 1 family and 1 order of Crustacea, 2 genera of Gasteropoda, 3 families of Oligochaeta, 1 taxon of Acarina. Among Lepidoptera we have identified 13 species of Rhopalocera during thè autumn. At a first analvsis of data a good species diversitv results in thè study area, but naturai habitats are continuously decreasing. Riassunto. Primo contributo alla conoscenza della valle del Tammaro. Le ricerche faunistiche nella valle del Tammaro (Sannio), svolte nel periodo 1 984- 1991, sono inquadrate nell’analisi della fauna appenninica in aree a rischio a causa di rilevanti attività antropiche come la costruzione di invasi. In questo resoconto vengono presentate le prime liste faunistiche delle specie di Mammiferi, Uccelli, Lepidotteri Ropaloceri e dei taxa riscontrabili operando un’analisi del macrobenthos. Sono state riscontrate 12 specie di Mammiferi, 66 specie di Uccelli, di cui 18 residenti, 39 solo nidificanti, 47 migranti, 32 svernanti, 3 estivanti. Tra il macrobenthos ritroviamo i seguenti taxa: cinque generi di Plecotteri, sei famiglie di Tricotteri, 1 1 generi di Efemerotteri, cinque famiglie di Coleotteri, sei generi di Odonati, cinque famiglie di Ditteri, due generi di Eterotteri, una famiglia e un genere di Crostacei, due generi di Gasteropodi, tre famiglie di Oligocheti, un gruppo di Acari. Infine sono state identificate 13 specie di Lepidotteri Ropaloceri relative al solo periodo autunnale. In particolare tra l’avifauna e la bentofauna si osserva una buona diversità di specie con alcune emergenze faunistiche. Per cui, anche se, con la notevole mosaicizzazione del territorio, si osserva una probabile diminuzione degli habitat naturali, l’area del Tammaro mostra un discreto interes¬ se faunistico e probabilmente una buona qualità ambientale. Received 27.1 1.92, accepted 14.6.93 16 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) Introduction The Tammaro river rises in thè Sannio’s Appennines through a series of springs in thè Sepino commune (CB). It flows into thè Calore river near thè railway station of Paduli (BN). Its drainage-basin (673 sq.km) develops from NW to SE between thè Matese massif and thè Sannio mountains downstream thè Sella of Vinchiaturo (Carta della Montagna, 1976; Plensio, 1978). The river crosses through a series of hills characterized by miocene soils and more recent pliocene sediments. A suffìcient stability occurs along thè slopes where prevalent arenaceous and/or carbonate soils outcrop; whereas in thè land characterized by clayey soils it is possible to observe a considerable geomorphologic trouble, independently by thè slope. The territory was inhabited since thè prehistory, but it owes his development to thè seasonal activity linked to thè moving of thè herds since thè Roman Age. The basin develops along thè cattle-track Pescassero- li-Candela (AAVV, 1990). The man-made landscape is typical of thè Appen¬ nines and it is also defined by thè stock-raising, by thè farming, by thè little towns developed along thè historical lines of communication. On thè landscape fragmentariness, expanded until now, are superimposed recent phenomena of little industrialization, intensive tobacco growing and river sand mines. Since thè half of thè 80’s a dam is under construction near Ponte Ligustino, in order to utilize thè Tammaro-water to irrigate thè fìelds. Fauna is practically unknown along thè valley if we consider thè few and fragmentary informations got from little locai issues, without a scienti- fic purpose, (Plensio, 1978) and those ones, however incomplete, got from thè "Carta Faunistica della Campania” (Grassi & Milone, 1985) and from thè Campania Breeding Birds Atlas (Fraissinet & Kalby, 1987). In this picture thè Department of Zoology has started a research programme over all thè areas of Campania where there are dams under construction or about to be planned with three principal aims: 1. to investigate thè Fauna of thè Appennines in thè unknown areas, 2. to preserve thè faunistic emergencies and 3. to evaluate and monitor thè impact of a dam on thè biological communities. This report is thè fìrst contribution to thè fauna analysis of thè Tammaro valley's. Buonomo R., Mirabella P., de Filippo G., Mìlone M. 17 ■ Study area The considered area (fig. 1) is located between thè "Varco di Vinchia- turo” (CB) (A) and thè place name "Monteleone” (B) near Pescosannita (BN); its altitude varies from 590 m (from sea-level), "Fontana della Tenda ” (C), to 284 m, "Monteleone” (B). The Tammaro is a torrent-like river, but it often shows wide bends. The river-bed is prevalently in its naturai state except where thè roads or thè railways cross it, in these cases thè embankments are reinforced with building materials. The banks are covered with thè vegetation that, so- mewhere, in some spots, takes up very small space (only 1 meter). The riparian bush is constituted by willow-, elm-, ash-, alder- tree, tamarisk, hornbeam. In thè meandering-areas we can see Carex and Typha. Near "Ponte Pescosardo ” (D) and near "Ponte Ligustino” (E), since 1987 , owing to thè construction of thè dam, thè area is characterized by marshes because of thè excavations and of thè continuai stream deviation. Methods Data relating to this work have been collected from 1984 to 1991: Mammals, Birds, Macrobenthofauna and Butterflies were studied. The researches into thè Mammals are connected to thè Project "Mam¬ mals of Italy Atlas”, started in 1990. They were carried out through direct observations and by examining thè tracks found along thè banks and thè river-bed. The direct observations refer to Mammals occasionally detected during thè other surveys or to animals found died. The indirect observa¬ tions regard tracks or spraints. Through thè analysis of carnivorous’ faeces (Prigioni, 1991) it is possible to show thè presence of Insectivora and Rodentia. The determination of thè species is possible through thè analysis of bones (Toschi & Lanza, 1959; Toschi, 1965) and coats (Debroit et al., 1982). Birds have been censused by thè Emlen transect method (1971). The transects, 1 kilometre long, were carried out early in thè morning, 1 hour after thè sunrise, in particular during thè breeding (April-July) and thè wintering (December-February) periods. The census was taken year after year in thè 1985-91 period in thè following localities: "Fontana della Tenda (C), Ponte Principe (F), Ponte Stretto (G), Ponte Pescosardo (D), Ponte Ligustino (E), Monteleone (B)” . *00*, 18 Figure 1 - Location of Tammaro valley. Localities - A: Varco di Vinchiaturo; B: Monteleone; C: Fontana della Tenda; D: Ponte Pescosardo; E: Ponte Ligustino; F: Ponte Principe; G: Ponte Stretto; Mairi towns: 1 : S. Giuliano del Sannio; 2: Sepino; 3: S. Croce del Sannio; 4: Sassinoro; 5: Morcone; 6: Campolattaro; 7: Reino; 8: Pesco Sannita. Buonomo R., Mirabella P., de Filippo G., Milone M . 19 The Macrobenthofauna was collected in thè same localities, during thè 1990-91 years, according to Ghetti (1986). The samples were collected in spring and autumn by utilizing thè “surber” according to thè tipology of thè river’ stretch; thè samples were determined in thè laboratory until a taxa’s level useful and necessary to obtain thè values of thè environment’s quality (E.B.I.: Ghetti, modified, 1986; I.B.G.: by Verneaux, 1983). The Lepidoptera (Rhopalocera) were collected covering linear tran- sects, along thè river. Until now only thè autumnal period (1991) it has been investigated. The species’ determination was carried out according to Higgins & Riley (1983). Results In table I thè 12 species of Mammals identified along thè banks and thè river-bed are indicated. Table I - The Mammals of thè Tammaro banks Species Erinaceus europeus Talpa europea Lepus capensis Myotis glis Arvicola terrestri Rattus norvegicus Mus musculus Vulpes vulpes Mustela nivalis Martes foina M. martes Sus scrofa The Avifauna identified during thè transect counts is shown in table II; it is also described thè phenology of thè species. 66 species have been identified: 18 are considered as sedentary-, 39 as breeding- (in addition to thè sedentary species), 47 as migratory-, 32 as wintering-, 3 as non breeding summer visitor-species. 20 Boll Soc. Natur. Napoli - Voi 101 ( 1992-1993 ) Table II - Chek-list of thè birds of thè Tammaro banks with their phenological status. B=breeding; S=sedentary; M=migratorv; W=wintering; E=non breeding summer visitor. Species Phenologv Ardea cinerea M,W,E Buteo buteo M,W,E Milvus milvus B,M,W,E M. migrans M,W Falco tinnnnculus S Gallinula chloropus s Charadrius dubius B,M,W Scolopax rusticola B,M,W Vanellus vanellus M,W Tringa ochropus M,W Columba livia S C. palumbiis B,M,W Streptopelia tnrtur B,M Apus apus B,M Alcedo atthis B,M,W Cuculus canorus S Jynx torquilla B,M,W Lulliila arborea B,M Galerida cristata B,M Alauda arvensis B,M,W Hirundo rustica B,M Delichon urbica B,M Anthus campestris B,M A. pratensis M,W Motacilla cinerea B,M M. alba B,M,W Troglodytes troglodytes S Prunella modularis M,W Erithacùs rubecula B,M,W L u se i n i a m ega rhvn chos B,M Phoenicurus ochrurus M,W Saxicola torquata B,M,W Buonomo R Mirabella P., de Filippo G., Milane M . 21 cont. Table II Species Phenology Oenanthe oenanthe B,M Turdus merula S T. philomelos M,W Acrocephalus schoenobaenus B,M,W A. scirpaceus B,M A. arundinaceus B,M Cettia cettii B,M,W Cisticola juncidis S Sylvia melanocephala S S. communis B,M S. atricapilla B,M,W Phylloscopus collybita B,M,W Muscicapa striata B,M Aegithalos caudatus B,M,W Parus caeruleus S P. major s Remiz pendolinus s Sitta europea s Lanius collurio B,M Garrulus glandarius s Pica pica s Corvus corone cornix s Passer italiae s P. montanus s Fringilla coelebs B,M,W Serinus serinus B,M,W Carduelis chloris B,M,W C. carduelis B,M,W C. spinus B,M,W C. cannabina B,M,W Emberiza citrinella B,M E. eia B,W E. cirlus B,M,W Miliaria calandra S 22 Boll Soc . Natur . Àfopo/i - Po/. 101 (1992-1993) The taxa of thè Macrobenthofauna are listed according to thè systema- tic level required to determinate thè water's quality. The specimens identified belong to 5 genera of Plecoptera, 6 families of Trichoptera, 1 1 genera of Ephemeroptera, 5 families of Coleoptera, 6 genera of Odonata, 5 families of Diptera, 2 genera of Heteroptera, 1 family and 1 order of Crustacea, 2 genera of Gasteropoda, 3 families of Oligochaeta, 1 taxon of Acarina (table III). 13 Butterflies species until now are identified (table IV). Table III - Macrobenthofaunistic taxa of Tammaro river. Order or class - | - - - — - - - Family Genus Plecoptera Capniidae Capnia Nemauridae Protonemnra Perlodidae Isoperla P e riode s Taenioptervgidae Brachyptera Trichoptera Limnephilidae Psvchomyidae Rhyacophilidae Polvcentropodidae Hvdropsvchidae Philopotamidae Ephemeroptera Baetidae Baetis Pseudocentroptilum Ephemerellidae Ephemerella Leptophlebiidae Paraleptophlebia Habrophlebia Eleptageniidae Ecdyonurus Rhithrogena Epeorus Eie etra gena Caenidae Caenis Oligoneuridae Oligoneuriella Coleoptera Elminthidae Hvdrophilidae Haliplidae Hvdraenidae Dvtiscidae Buonomo R., Mirabella P., de Filippo G., Milone M. 23 cont. Table III Order or class Family Genus Odonata Zyg. Platycnemididae Plactynemis Coenagrionidae Pyrrhosoma Calopterydidae Calopterix Anis. Gomphidae Onychogomphus Libellulidae Orthetrum Cracothermis Diptera Simuliidae Chironomidae Limoniidae Ceratopogonidae Tipulidae Heteroptera Corixidae Micronecta Pleidae Plea Amphipoda Gammmaridae Cladocera Basommatophora Planorbidae Gyraulus Physidae Physa Tubificida Tubificidae Enchytraeidae Haplotaxida Hydracarina Lumbricidae Discussici In thè area of thè Tammaro river, thè development of thè naturalistic research has made possible only a comparison between our data on thè Mammals and thè Birds and those ones of thè “Carta Faunistica della Campania” (Grassi & Milone, 1985) and of thè Breeding Birds of Campania Atlas (Fraissinet & Kalby, 1987). This comparison is limited because of thè different methods of investigation: thè data frorn thè “Carta Faunistica” were reported according with thè Commune boundaries and those ones from Atlas were referred to squares 1:25.000 according with I.G.M. maps. 13 Mammals species are reported for thè Tammaro area in thè “Carta Faunistica”. Here we report 12 species: among them lack Elyomis guerci 24 Boll Soc , Natur. Napoli - Voi 101 (1992-1993) Table IV - Lepidoptera of thè Tammaro banks Species Family Papiliu machao'n Papilionidae Arto gei a rapa e Pieridae Arto gei a inannii Artogeia napi Colias crocea Lycaena p. phleas Lvcaenidae Heodes tityrus Everes alcetas Po lyommatu s i c a rus Melitaea didyina Nvmphalidae Maniola jurtina Satvridae Coenonympha pamphilus Ochlodes venatus Hesperiidae 1 nus, Muscardinus avellanarins, Canis lupus, Mustela putorius, Meles meles, Felis silvestris, which are reported in thè “Carta Faunistica”. This differen- ce in thè number of species is due to thè fact that in thè “Carta Faunistica” onlv thè species of agricultural and hunting interest are documented. The only faeces found in thè studv area are those of Vulpes vulpes, but we haven’t found bones or coats of micromammals there. As regards thè other species we think that it is possible thè presence of Canis lupus (checked for thè Matese massif and thè Sannio's mountains), but it would be a very occasionai occurrence which is related to thè wide mobility of thè species along thè Appennines (Boitani L., pers. comm.). Not scientific literature report thè presence of Meles meles, Mustela putorius and Sciurus vulgaris (Plensio, 1978); we have no evidence for thè first two species, and we are sure that Sciurus vulgaris is mistaken for Myotis glis. Differing from thè “Carta Faunistica” and thè Breeding Birds Atlas, our data don't include thè night-birds of prey: this is due to thè transect method. Other species (as thè migratorv Charadriiformes, some Ardeidae or Anatidae) are not reported in our check-list may be because of their accidental presence in thè studv area due to thè variability of thè climate and of thè habitats’ tvpology. A better analysis on thè breeding birds is possible by comparing thè data from thè Atlas with our list (see table II). In thè Tammaro basin 60 breeding birds are reported in thè Atlas while 57 species are censused in this paper. Species like Falco suhbuteo, Coturnix Buonomo R ., Mirabella P., de Filippo G., Milone M . co tur nix, Phasianus colchicus , Saxicola rnbetra, Phylloscopus sibilatrix, Parus palustris, Corvus monedula, Corvus corax, Petronia petronia, select for habitats different frorn those ones found along thè Tammaro river. For this reason they are reported in thè Tammaro region by thè Atlas, but are not reported in our list. Other species like Picus viridis, Picoides major, Acrocephalus melanopogon, Hippolais poliglotta, Sylvia cantillans , Certhia brachydactyla, Oriolus oriolus could be extremely localized on thè territory (so that it would be unlikely to take a census of them with thè transects). An other hypothesis could be thè reduction of suitable breeding habitats in thè last years. On thè other hand thè transect method has proved thè breeding of Milvus milvus, Anthus campestris , Acrocephalus schoenobaenus , A. arundinaceus , Cisticola juncidis, Sitta europea, Remiz pendolinus , Cardite¬ la spinus which are not inserted in thè Atlas. Other species, regarded as “probable breeding” in thè Atlas, as Alcedo atthis, A. scirpaceus, Muscicapa striata , and Corvus corone cornix, were proved to be surely breeding. It is important thè breeding of Anthus campestris , which is indicated as a rare breeding species in Campania (de Filippo et al., 1990). Moreover it is very important thè breeding of Acrocephalus schoenobaenus and Carduelis spinus (Conti P., pers. comm.), since these nidifications are thè fìrst ones in thè Campania District. The ornithological informations described in thè work of Plensio (1978) are difficult to interpreti there are species easy to identify like Perdix perdix or Oriolus oriolus, some hard to identify like Hippolais poly gioita or Regulus regulus, some typical of other biogeo- grhaphic areas like Parus cristatus, or some considered thè same species such as Anthus campestris and Melanocorypha calandra. In this first approach to thè benthofaunistic taxa our list of familia and genera can lead to same generai considerations. The identification of many genera of Plecoptera shows thè presence of fresh-waters rich in oxygen and a stony river-bed, even if thè genus Isoperla is able enough to endure a light defilement. In thè order of Trichoptera we can note thè presence of Hydropsychidae where thè river is rich in organic substances and thè current is moderate; other families like Philopotamidae and Rhyacophili- dae are typical of torrent-like rivers. In thè order of Ephemeroptera it is important thè identification of one species of genus Caenis recently observed in thè South of Italy (Belfiore C., pers. comm.). Other genera like Baetis and Ephemerella endure pollution very well, others like Oligoneu- riella are characteristic of torrents or streams with speedy waters. The Coleoptera Elmididae prefer stony and pebbly stream-beds; other families like Hydrophilidae and Hydraenidae can live in stagnant-waters too. Coleoptera generally prefer bank- microhabitats with shallow water, lots of 26 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) vegetation and organic remains. The families of Ceratopogonidae, Chiro- nomidae and Tipulidae (Diptera) are all of sandy- or oozy-bottom rich in organic material. The genus Physa (Gasteropoda) suggests thè presence of limpid and oxygenated fresh-water. On thè other hand thè Oligochaeta prefers rivers with sandy- or oozv-bottoms, aquatic vegetation and organic remains. These observations show a high environmental variability and a considerable lack of information on thè Appennines Macrobenthofauna. The Lepidoptera here identified are generally species with wide range in Italv; their occurrence denotes a great fiorai diversity caused by a considerable mosaicism in thè landscape. Further considerations are not possible because thè survev concerns only thè late summer and it lacks all thè spring species. Today thè Tammaro valley's is not "... thè verv great forest...very terrible and shadowy for thè several high and branched oaks ..." as a geographer Dominican friar wrote in 1681 neither that one described by thè historiographer Galanti in 1770 (Plensio, 1978). A generai analysis of our data displays a considerable mosaicism of thè area, a good species diversity independentlv by thè decrease of naturai habitats but according to thè high environmental variability. It is impor¬ tane now, to carry on thè naturalistic research in an unknown area to hypothesize a suitable management through a valuation of thè environ¬ mental quality. Acknowledgements Research no.219 from thè Eco-Ethological Group (G.E.E.) of Naples. Grants from M.P.I. 60%. We are grateful to drs. Carlo Belfiore and Paola Conti for their informations. This work has received contributions by thè people of G.E.E. group, in particular by L. Fusco and C. Piazza. REFERENCES AA.VV., 1990. Trekking della transumanza, Comunità Montana ALto Tammaro Fortore Ufita, Morcone (BN), Edigrafica morconese. Carta della Montagna, 1976. Campania, voi. II, monografie regionali, Ministero deH'Agricoltura e Foreste, Geotecneco, Urbino, Arti Grafiche Editoriali. Debroit, S., G. Fivaz, C. Mermod & J.M. Weber, 1982. Atlas des poils des Mammife- res d’ Europe , Institute de Zoologie de l'Université de Neuchatel. Buonomo R., Mirabella P., de Filippo G., Milane M. de Filippo, G., L. Fusco & M. Milone, 1990. L’indice di rarità percentuale (I.R.P.): un indice quantitativo basato sugli atlanti faunistici. Boll. Soc. Natur. Napoli, 98-99: 83-90. Emlen, J.T., Population densities of birds derived from transect counts. The Auk, 88: 323-342. Fraissinet, M., & M. Kalby, 1987. Atlante degli uccelli nidificanti in Campania (1983-1987) , Regione Campania - A.S.O.I.M., Salerno, Tipolitografia Incisivo. Ghetti, P.F., 1986. I macroinvertebrati nell’analisi di qualità dei corsi d’acqua, Provincia Autonoma di Trento - Stazione Sperimentale Agraria Forestale - Servizio Protezione Ambiente, Trento, Tip. Bertelli. Grassi, G. & M. Milone, 1985. Carta Regionale Faunistica, Ass. Agr. Foreste, Reg. Campania, Napoli. Higgins, L.G. & N.D. Riley, 1983. Faiialle d’Italia e d’Europa, Milano, Rizzoli. Plensio G., 1978. " Super Tamari Fluvium” Al di sopra del fiume Tammaro (dall’itinerario di Antonino), Campobasso, La grafica moderna. Prigioni, C., 1991. Aspetti della biologia della Volpe ( Vulpes vulpes ) in Italia settentrionale. Hystrix, 3: 41-50. Toschi, A., 1965. Fauna d’Italia, Mammalia, voi. 7, Bologna, Calderini. Toschi, A., & B. Lanza, 1959. Fauna d’Italia, Mammalia , voi. 4, Bologna, Calderini. Verneaux, J., 1983. Une nouvelle methode pratique d’evaluation de la qualité des eauxcourantes. Ann. Se. Univ. Besancon. zool., 3: 11-21. . Soli Soc \aiur. \apoli - VSl 101 f 1992-19^3). 29-92 29 Recent faunistic and ecotoxicological arrangement of thè terminal tract of thè Sarno river (Campania, Italy) Soppelsa O., Battagllni F. e Battaglili! P. Dipartimento di Zoologia, Università degli Studi «Federico II», Napoli, Italy Key words: River pollution, benthic fauna, ecotoxicology. Abstract. This report describes thè present faunistic, ecologica!, and ecotoxi- •cological environment of thè centrai and terminal part of thè Samo river in Campania. Previous studies considered it as a paradigmatic example of river pollution. Six stations located from thè centrai part of thè river to its mouth were selected for this study. Animai taxa include few species which are typical of a polysaprobic environ¬ ment. This is due to thè inflow of thè Cavaiola stream, thè most important tributary of thè Sarno river and main cause of its pollution. The station located before thè Cavaiola stream stili maintains acceptable ecological and faunistic conditions, while after thè point of confluence with this stream there is a zonation with river population, highly toxic influenced by thè waters of this tributary. Our research showed that thè causes of this pollution are thè high number of Industries operating along thè river, thè home waste of thè highly and densely urbanised neighbouring area and a poor utilisation of substances used in agricuì- ture. The comparison between current data and thè relevant literature shows a generai worsening of thè ecological and faunistic condition of thè river, making its possible recovery even more difficult. Riassunto. Recente assetto ecologico e faunistico della bassa valle e foce del fiume Sarno (Campania, Italia). Il Sarno è situato essenzialmente nella fertile pianura dell'agro nocerino-sar- nese. L’affluente più grande è il torrente Cavaiola, altre immissioni sono il Canale Fosso Imperatore e il Canale di S. Antonio Abate. Sfocia dopo circa ventiquattro chilometri nel Golfo di Napoli al confine dei Comuni di Torre Annunziata e Castellammare di Stabia. In rapporto alla lunghezza del suo corso e per la notevole urbanizzazione e industrializzazione del suo bacino, il Sarno è sottoposto ad un massiccio sfrutta¬ mento, che rende la portata più esigua esponendo il fiume agli attacchi inquinanti. La presente ricerca ha lo scopo di analizzare Fattuale stato ecologico ed ecotossicologico del tratto medio-terminale del Fiume Sarno che è considerato Receìved 27.1 1.92, accepted 6.6.93 30 Boll Soc. Natur. Napoli - Voi 101 (1992-1993) come un esempio paradigmatico di inquinamento fluviale. L’analisi ha interessato sei stazioni di campionamento, da prima del Cavaiola fino alla foce, in un periodo di tempo di circa un anno (ott. 90 - giu. 9 1 ) per un totale di cinque serie di prelievi. In ogni stazione sono state effettuate analisi, chimico-fìsiche dell’acqua e contemporaneamente è stata raccolta la bentofauna. La presenza contemporanea di ione ammonio e azoto nitroso indica che parte dell’inquinamento del Sarno è di origine organica. L’acqua è risultata basica per la presenza di NH3. Tuttavia l’azione basica dell’NLL è tamponata da acidi, come l’H2S, provenienti anch’essi dalla decomposi¬ zione di materiali organici o scaricati dalle industrie conserviere; si ottiene così una stabilizzazione del pH su valori leggermente basici. I solfuri presenti provengo¬ no anche dagli scarichi di alcuni processi della lavorazione conciaria ove viene usato Na2S. Nel periodo estivo le condizioni divengono più gravi per la diminuita portata del fiume e per l’elevata temperatura che rende l’ossigeno, già in condizio¬ ni normali prossimo agli 0 mg/L, meno solubile in acqua. Dai risultati ottenuti si deduce che le acque del Sarno sono “molto dure”. Si sono registrati, nel corso dei prelievi, anomali sbalzi della concentrazione dello ione CL a valle del Cavaiola; probabilmente il forte aumento dei cloruri è dovuto alla dissalazione delle pelli. Dai valori degli indici di dominanza e di diversità si evince che il tratto di fiume compreso tra l’immissione del Cavaiola e la foce risulta il più danneggiato, sebbene si noti un leggero recupero nel tratto terminale. La stazione 5 a monte della confluenza, dove sono presenti tutti e 6 i phvla, conta il maggior numero di specie, sono infatti presenti oltre ad un 33.5% di Nematodi, un 18.6% di Rotiferi e un 16.3% di larve di Ditteri (essenzialmente del genere Chironomus), anche un 12% di Copepodi, un 5% di Gasteropodi tra cui i generi Planorbis e Physa e un 2.4% di Emitteri. Nella stazione 4 si può notare la differente composizione faunistica tra le due sponde a causa della confluenza del Torrente Cavaiola. Nelle stazioni 3 e 2 sono presenti solo Turbeilari ( Stenostomum sp., Mesostoma sp.), Rotiferi (Rotaria neptunia), Nematodi, Oligocheti ( Tnbifex tubifex ) e Ditteri (anche qui larve di Chironomus). Nella stazione 1 sono stati raccolti anche alcuni Copepodi. Complessivamente sono stati raccolti 2226 animali appartenenti a 6 phyla (Platelminti, Rotiferi, Nematodi, Molluschi, Anellidi, Artropodi) e raggruppabili in 13 taxa. In definitiva si è notata la presenza di tre zone differenziate tra loro per la qualità e quantità di individui raccolti. La prima zona, identificabile nella stazione 5 è la più ricca di phyla ed ha una struttura faunistica tale da poter essere compresa tra le classi alfa e beta mesosaprobie del sistema saprobio. La seconda zona, la più devastata dall’inquinamento, comprende il tratto subito a valle dell’immissione del Cavaiola ed è definibile come metasaprobia. La terza ed ultima zona è identificabi¬ le nelle stazioni 3, 2, e 1 ed ha accentuate caratteristiche polisaprobie. I dati faunistici, in perfetto accordo con i parametri fisico-chimici, hanno permesso di ricondurre a due tipi fondamentali le cause dell’inquinamento: il primo alla grossa presenza delle industrie, il secondo agli scarichi domestici; causa minore ma non per questo trascurabile è l'inquinamento di origine agricola. La stazione a monte del Cavaiola conserva ancora condizioni accettabili. Dalla confluenza del Cavaiola in poi si ha una “zonazione”, infatti le acque di questo affluente costituiscono una vera e propria barriera ecologica alla diffusione degli Soppelsa O., Battaglini F. e Battaglini P. animali; gli indici di dominanza diventano altissimi e quelli di diversità bassi rendendo evidente la condizione di forte stress. Il confronto dei presenti dati con quelli in letteratura mostra un peggioramen¬ to generale delle condizioni del fiume; gli apporti inquinanti non riescono ad essere smaltiti e ciò comporta un allontanamento dalle condizioni di normalità. Altro ostacolo alla formazione di biocenosi ben definite sono le forti oscillazioni stagionali dei reflui. Introduction The Sarno river flows in a fertile plain surrounded on thè North side by thè Vesuvius and on thè other sides by thè Lattari Mountains. It flows through eight cities. It is originated by three sources: S. Maria della Foce (2.5 m3/s), used for a water System and a hydroelectric power plant; Acqua di Palazzo (3 m3/s), located at thè town of Sarno; and Acqua di S. Marino (2 m3/s). The three sources flow together originating a single river: thè Sarno river. The largest tributary is thè Favaiola stream, which increases its flow rate due to thè inflow of thè Solofrana stream. The Favaiola stream takes origin at about 1 ,300 m above sea level frorn thè Garofalo Mountain near Solofra and runs for almost 35 km before flowing into thè main stream of thè Sarno river at San Marzano. Other tributaries flowing into thè Sarno river are thè Fosso Imperatore canal and thè S. Antonio Abate canal. The Sarno river gives rise to thè Bottaro canal at Scafati. This canal was built for thè purpose of irrigating thè lands of thè Pompeii area. After twenty-four kilometres thè Sarno river flows into thè Gulf of Naples at thè border between thè towns of Torre Annunziata and Castel¬ lammare di Stabia. In proportion to its length thè Sarno river suffers a heavy agricultural exploitation and thè pollution by industriai and domestic wastes, both reducing its flow rate and exposing thè river to continuous pollution attacks. As a matter of fact, thè highly urbanized area crossed by thè river is characterized by a widespread and potentially polluting vegetable and fruit intensive cultivation and by several preserved food, tanning, paper, and pharmaceutical industries (d'Elia et al., 1974). In view of thè above, it appears clear that thè Sarno river is a paradigmatic example of highly altered watercourse. After thè faunistic, ecological and generai studies (Battaglini, 1979) on thè hygienic, sanitary 32 Boli Soc . Natur. Napoli - Voi 101 ( 1992-1993 ) and pollution aspects (d'Elia, 1988), thè ecological data, sensu lato, are no longer present in literature. Due to thè ecological, rural and social-econo¬ mie importance of this river in Campania, it was necessary to examine thè current conditions of thè centrai and terminal part of thè Sarno river, which is thè area most affected by alternative phenomena of anthropic origin. The location of research stations is very important to verify thè sanitary conditions of a river (Battaglini, 1979). In this specific case thè location of thè stations was easier, as it was based on previous researches (Battaglini et al., 1967 - 1968; d’Elia et al., 1974). However, a survey with relevant sampling-site takings was carried out to detect any changes in thè conditions of thè river. Procedures and methods Five monitoring sites were located along thè Sarno river and one along thè tributary Cavaiola (see Fig. 1); these are numbered in Arabie numerals from thè mouth to thè middle of thè river. Station 1 represents thè mouth of thè river and is situated at about 200 m from thè sea. Station 2 was located beyond thè inflow point of thè S. Antonio Abate canal and thè drain of a paper mill (2.7 km from thè sea). Station 3 is not very far from station 2. It is situated between thè towns of Scafati and Pompeii and was selected to obtain a relative control (reference specimen) of thè chemical tests for thè subsequent stations (1 and 2), as it is located upriver from an important tributary: thè canal of S. Antonio Abate (3.825 km from thè sea). Station 4 is located downstream from thè inflow point of thè Cavaiola stream (10.025 km from thè sea), which was analysed by thè CAV special station due to its polluting power. Station 5 is thè closest to thè source and is located upriver from thè confluence with thè Cavaiola stream; this station will be considered as a control to all intents and purposes of thè research. The listed stations are located in an area of study that ranges from approximately one kilometre upriver from thè inflow of thè Cavaiola to its terminal part (see Fig.l), covering a total of 10.350 km. Samplings were carried out at each station both on thè right (R) and on thè left bank (L) on thè following days 01/10/90, 12/12/90, 26/02/91, 08/05/91 and 26/06/91, proceeding upstream from station 1 to station 5 as Soppelsa O., Battaglini F. e Battaglini P. suggested by standard sampling methods for fluvial fauna (Standard Methods, 1989). One-litre (1 L) water samples were taken and stored in Teflon bottles at each station for thè chemical-physical study of thè waters. Furthermore, samples of exactly 60 mi were taken for thè analysis of oxygen dissolved in thè water. Figure 1 - Simplified representation of thè Sarno river and of its tributaries; thè various sampling stations are reported (•). The chemical-physical researches concerned thè survey of NO2, NH4+, Cl“, Fe, Fe2+, Fe3+, Ca2+, Mg2+,02, H2S, total hardness, alkalinity, temperatu¬ re (air, water), pH. Air temperature was measured with a +10 to +40° C scale thermome- ter, while water temperature was determined by means of a 0 to 50 scale pit thermometer with a 0.5° C accuracy. Spectrophotometry methods were used to analyze thè concentration of pollutants. 34 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) The concentration of ion magnesium was obtained theoretically su- btracting thè calcium from total hardness. The collecting of mesobenthofauna was carried out with a small 30 cm wide and 38 cm deep landing net (approx. 25 L capacity, 0.5 cm mesh diameter). The six samplings were carried out at each station within a time span of 12 h and repeated at intervals of about two months from each other to examine thè entire yearly cycle of thè river. The Dominance index of Simpson (Pielou, 1966b), thè Difference index of Shannon (Pielou, 1966c), and thè similarity index (Pielou, 1966a) were assessed along with thè taxonomic determination and thè ecological- statistical analysis in order to obtain a more accurate picture of thè distribution and thè population characteristics. Results Chemical-Physical Results The chemical-physical characteristics of thè water taken from both banks of thè six stations during thè research are reported in detail in Tables 15. The chemical-physical data give an even better idea of thè big damage that thè Cavaiola stream causes to thè Sarno river. As a matter of fact, upriver from this inflow (Station 5) thè average 02 and NH3 values of thè river are 1.25 and 0.33 mg/L, respectively, while at thè immediately subsequent station 4L its course is conditioned by thè values of thè tributary: thè average 02 and NH3 values are 0.2 and 4.7, respectively. Thus, it is likely that thè Cavaiola stream is responsible both for thè increase of organic waste and decrease of thè concentration of oxygen dissolved in water. Even if it is obvious that this is due to aerobic-type catabolic processes, it should be noted that catabolic processes are mainly anaerobio due to thè very low rate of 02 and thè presence of H2S. These phenomena are mainly ascribable to thè massive number of tanneries operating along thè Solofrana stream (a tributary of thè Cavaiola stream) and draining waters containing hair and flesh tissues. The great number of unlawful drains flowing into both streams should also be considered. In addìtion to thè increase of organic substances, thè Cavaiola stream is also responsible for thè presence of toxic substances such as hexavalent chrome (found through qualitative tests) and for thè significant variation of Cl“, basically due to thè hide desalting process (see Tables I-V). Soppelsa O., Battaglini F. e Battaglini P . Table I - Chemical-physical properties of water samples taken at thè various stations on thè 1/10/90; L=left bank - R=right bank 1/10/90 Station 1 Station 2 Station 3 Station 4 Station 5 CAV. S D S D S D S D S D T °C (air) 22 22 27 27 29 29 24 24 24 24 24 T °C (water) 15 14 16 16 16 16 16 16 16 16 16 pH 7.13 7.18 6.95 6.87 7.02 7.00 6.92 7.05 7.06 7.14 7.08 02 (mg/L) - - - - - - - - - - - NO; (mg/L) 0.6 0.1 0 0 0.1 0.1 0 2 0.3 2 trace NH; (mg/L) 1.1 1.1 1.3 0.7 1.9 0.4 3.5 0.6 0.25 0.5 4.3 CL (mg/L) 75 75 75 75 75 75 300 40 50 50 300 Hardness* 484 488 463 454 445 449 393 430 441 445 392 Ca++ (mg/L) 125 126 124 124 122 122 100 122 119 119 95 Mg++ (mg/L) 41.2 41.4 36.7 34.5 33.6 34.4 34.4 29.7 34.5 35.4 37 Alcalinity 400 400 465 470 455 455 460 420 432 437 550 CO, (mg/L) 30.4 26.8 44.4 54.6 37.0 38.7 47.5 32.0 31.7 27.3 39.2 Fe (total) (mg/L) 0 0 trace trace trace trace 0.6 0 0 0 0.7 Fe++ (mg/L) 0 0 0 0 0 0 0 0.1 0 0 0.1 Fe+++ (mg/L) 0 0 0 0 0 0 0 0.5 0 0 0.6 * = mg/L CaCQ, Table II - Chemical-physical properties of water samples taken at thè various stations on thè 12/12/90; L=left bank - R=right bank 12/2/90 Station 1 Station 2 Station 3 Station 4 Station 5 CAV. S D S D S D S D S D T °C (air) 5.0 4.5 8.0 8.0 14.5 14.5 14.0 9.0 9.0 9.0 12.0 T °C (water) 12.5 12.0 13.0 13.0 13.0 13.0 12.0 12.5 12.5 12.5 12.0 pH 7.17 7.15 7.18 7.18 7.25 7.20 7.55 7.33 7.41 7.36 7.39 02 (mg/L) 0.4 0.2 0.4 0.2 0.4 0.4 trace 1.6 1.6 1.6 trace NO; (mg/L) >2.0 >2.0 >2.0 >2.0 >2.0 2.0 0.1 0.4 0.6 0.6 0.1 NH; (mg/L) 0.8 1.3 0.8 0.8 1.5 0.6 2.5 0.2 0.3 0.2 3.6 Cl" (mg/L) 100 100 150 150 150 150 >300 50 45 50 >300 .Hardness* 502 484 502 488 472 488 459 454 466 445 516 Ca++ (mg/L) 138 135 136 137 132 130 130 129 130 129 138 Mg++ (mg/L) 37.7 35.2 38.9 34.8 34.0 39.0 32.2 31.5 33.9 29.4 41.1 Alcalinity 450 470 475 470 450 470 545 425 425 425 >550 C02 (mg/L) 25.0 29.0 26.8 26.4 22.0 25.5 12.8 16.7 14.0 15.8 19.0 Fe (total) (mg/L) 0.3 0.2 0.4 0.4 trace 0.3 0.5 0 0 0 0.5 Fe++ (mg/L) 0 0 0 0 0 0 0.5 0 0 0 0.5 Fe+++ (mg/L) 0.3 0.2 0.4 0.4 trace 0.3 0 0 0 0 0 * = mg/L CaCO, 36 Boll. Soc. Natur. Napoli - Voi. 101 ( 1992-1993 } Table III - Chemical-physical properties of water samples taken at thè various stations on thè 26/02/91; L=left bank - R=right bank 26/2/91 Station 1 Station 2 Station 3 Station 4 Station 5 CAV. S D S D S D S D S D T °C (air) 7 7 8 8 10 10 11 14 10 14 11 T °C (water) 12.0 12.0 11.5 11.5 12.0 12.0 12.0 12.0 12.0 12.0 12.0 PH 7.19 7.19 7.14 7.19 7.29 7.22 7.74 7.41 7.46 7.42 7.77 0, (mg/L) 0.4 0.4 0.6 0.4 0.6 0.6 0.2 0.7 0.8 1.5 0.2 NO; (mg/L) >2.0 >2.0 1.3 1.3 1.3 1.3 1.3 0.4 0.4 0.4 >2.0 NHJ (mg/L) 1.0 1.0 1.2 1.0 1.2 0.8 2.8 0.4 0.4 0.4 4.5 CL (mg/L) 75 75 75 75 75 75 130 50 50 50 130 Hardness* 509 509 509 509 488 498 310 466 466 473 306 Ca++ (mg/L) 140 139 140 140 136 140 95 138 132 136 93 Mg++ (mg/L) 38.2 38.8 38.2 38.2 35.4 35.6 17.3 29.1 32.7 32.0 17.7 Alcalinity 425 430 425 430 425 425 425 320 430 420 340 C02 (mg/L) 23.3 23.8 26.4 23.8 18.5 22.0 10.6 14.1 12.3 13.6 5.3 Fe (total) (mg/L) 0.4 0.3 0.4 0.4 0.1 0.2 0.5 0 0 0 0.5 Fe++ (mg/L) 0 0 0 0 0 0 0.4 0 0 0 0.5 Fe+++ (mg/L ) 0.4 0.3 0.4 0.4 0.1 0.2 0.1 0 0 0 0 * = mg/L CaCO, Table IV - Chemic.al-physical properties of water samples taken at thè various stations on thè 08/05/91; L=left bank - R=right bank 8/5/91 Station 1 Station 2 Station 3 Station 4 Station 5 CAV. S D S D S D S D S D T °C (air) 1 1 1 1 15 1? 17 17 20 18 20 18 20 T °C (water) 14 14 14 14 14 14 16 14 14 14 16 pH 7.13 7.17 7.25 7.18 7.28 7.20 7.68 7.34 7.35 7.42 7.82 0: (mg/L) 0.3 0.4 0.6 0.6 0.6 0.6 0.4 1.0 1.0 1.0 0.4 NO; (mg/L) >2.0 >2.0 >2.0 >2.0 >2.0 >2.0 0 0.8 0.6 0.6 0 NII: (mg/L) 1.3 2.0 0.65 1.3 0.75 1.5 6.0 0.5 0.2 0.4 3.0 CL (mg/L) 150 150 120 120 75 75 300 50 50 50 >300 Hardness* 502 477 472 488 456 473 425 441 438 445 409 Ca++ (mg/L) 136 127 134 134 132 130 127 124 124 124 127 Mg++ (mg/L) 38.9 38.3 32.8 36.6 30.2 35.6 25.9 31.5 30.7 32.4 22.0 Alcalinity 475 475 460 465 445 445 450 420 415 420 625 C02 (mg/L) 30.4 27.3 22.4 26.4 19.4 24.2 8.0 16.3 15.8 13.2 7.0 Fe (total) (mg/L) 0.5 0.4 0.4 0.3 0.2 0.1 0.3 0.1 trace trace 0.4 Fe++ (mg/L) 0.3 0.3 0.1 trace trace trace 0.2 trace 0.1 0.1 0.2 Fe+++ (mg/L) 0.2 0.1 0.3 0.2 0.1 trace 0.1 trace 0 0 0.2 * = mg/L CaCO, Soppelsa O., Battaglinì F, e Battaglini P. 37 Table V - Chemical-physical properties of water samples taken at thè various stations on thè 26/06/91; L=left bank - R=right bank 26/6/91 Station 1 Station 2 Station 3 Station 4 Station 5 CAV. S D S D S D S D S D T °C (air) 21 21 24 24 27 27 29 29 29 29 29 T °C (water) 17 17 17 17 17 17 17 15 15 15 17 pH 7.37 7.21 7.38 7.38 7.54 7.42 7.54 7.54 7.50 7.53 7.52 0, (mg/L) - NO; (mg/L) >2.0 >2.0 >2.0 >2.0 >2.0 >2.0 0.1 0.5 0.5 0.5 0.1 NHI (mg/L) 2.0 2.0 2.0 2.0 1.3 1.5 >8.0 0.4 0.3 0.4 >8.0 CL (mg/L) 150 150 150 150 150 150 >300 75 75 75 >300 Hardness* 502 463 474 473 456 463 445 429 437 436 434 Ca++ (mg/L) 133 128 124 124 127 127 124 123 123 123 126 Mg++ (mg/L) 40.7 34.3 39.2 39.2 33.2 34.9 32.4 29.2 30.9 30.9 28.6 Alcalinity 490 480 460 460 440 450 500 420 420 420 500 CO, (mg/L) 18.0 25.0 16.3 16.3 11.0 14.5 12.3 10.1 11.4 11.4 12.7 Fe (total) (mg/L) 0.3 0.4 0.2 0.2 0.1 0.2 0.6 0 0 0 0.6 Fe++ (mg/L) 0 0 0 0 0 0 0.5 0 0 0 0.5 Fe+++ (mg/L) 0.3 0.4 0.2 0.2 0.1 0.2 0.1 0 0 0 0.1 * = mg/L CaC03 The values of NH3, of H2S and N02 increased from winter to summer due to thè seasonal work of many preserved food industries operating in that area and due to thè decrease of 02 concentrations caused by thè temperature increase. Faunistic -E oologie al Results A total of 2,226 animals belonging to 6 phyla (Platyhelminthes, Rotife- ra, Nematoda, Mollusca, Annelida, Arthropoda) and which could be grou- ped in 13 taxa were collected (Tab. VI). Station 5 (Tab. VII) is located upriver from thè confluence, where all of thè 6 phyla are observed, and has thè highest number of species. Besides a 33.5% of Nematoda -with thè species Dorylaimus sp. and Rhabdolaimus sp.- a 18.6% of Rotifera - Rotaria rotatoria, Branchionus angularis and Philodina sp.- and a 16.3% of Dipterans (larva) - with thè species Chaobo- rus plumicornis and Chironomus sp.- there is also a 12% of Copepods (■ Ciclops strenuus), a 5% of Gastropods among which we find thè species Physa sp., Planorbis sp. and Physa fontinalis - and a 2.4% of Hemipterans (Velia rivorum). The difference in thè faunistic composition of thè two Table VI - Global structure of thè fauna during thè various samplings 38 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) r- ri ri r- d" oo o oo m r rn _ o d- r~ co O d" ON o d" q m ri q co o ò ON LO ri ri d q d q NO d q oo o d" co ON o in in d" ON d" nO rn NO NO rn m i— < d- in n ri H d" n On ri ri d- o 5— i >— ri to ri ni oo d- ni On m n (N r O o r- n O d" r- ON NO n rn rn oo nO o (N q o

rn r- rn o rn LO ON ri ri d o d d in d o oo d" ’ 1 ri o r- rn d" d- m » n in r- ON ON CM On * — < — m . — < m m *— nO o 00 O o o o o o o O o o o o o o o (N 00 q oo q q n NO 00 n q q o ri d" OO q ri q ri d d ON d q in ri m o O d- r- d" m O m On r- oo o ON nO ri On T— C . — d" n o fN i < — i m o o od q .2 o X < H o cd E ; banks caused by thè confluence of thè Cavaiola stream can be noted at station 4 (Tab. Vili); as a matter of fact, we can say that among all thè samples taken on thè I e 11 bank ,, thè Nematoda were thè only ani mais found in mud samples. At station 3 (Tab. IX) and 2 (Tab. X) there are only Turbellarians - with thè species Mìcrostomum lineare, Microstomum sp., Stenostomum sp., Mesostoma lingua, Mesostoma sp., Rotifera - with thè species Rotaria neptunia, Branchionus sp., Nematoda, with Rhabditis limnicola, Oligochaetes - with thè species Tubifex tuhifex, Limnodrilus sp., Stylaria sp. and Dipterans - once again with larva of Chironomus sp., Chironomus thumnii, Eristalis sp.-. At station 1 , besides thè same taxa found at stations 2 and 3 there were also occasionai findings of some Copepods (Tab. XI). Discussion The contemporary presence of ammonium ion and nitrous nitrogen shows that thè pollution of thè Sarno river is partially of organic origin (sewers, preserved food industry drains, urban waste, farm rejects, etc.) even though toxic inorganic substances due to minor tanning products are also present. Despite thè above, thè pH value is slightly basic at all thè stations. It is our opinion that many anthropogenic aspects concur to this, such as H2S-buffered NH3, both originated by thè decomposition of organic matter or by preserved food industry drains, and anion HS , which in favourable condition is balanced with hydrogen sulphide and may thus dissociate itself a second time giving rise to S2“, both originated by thè decomposition of sulphide and thè drains of some tannery processes using Na2S. Anomalous increases of thè Cl~ ion concentration (probably due to thè hide desalting process) were reported during thè sampling both in thè Cavaiola stream and on thè left bank of station 4. The concentration of ammonia also contributes to thè definition of thè pH; in water it reacts as follows: NH3 + H20 ^ NH| + OH- water will be more basic if ammonia increases; this reaction is completely moved to thè left. An increase of thè ammonia ion in time has been observed. Its utmost level was reached in thè sampling carried out on thè 26th of lune, 1991; Table Vili - Composition of thè fauna at station 4 at thè various times of sampling Soppelsa O., Battaglini F. e Battaglini P . 'sf- oo NO oo T— ( NO o NO V“H ON o nO °N O- oo NO NO et ON o nO d d 04 d d d d ’-1 d d d od d d ON 04 LO <— co LD CO 1— 1 i-H O co LO ON ON in oo NO co uo o co On ON o o in NO ON LO co NO CO d d NO d- NO fN d d d fN 04 d 04 CO - nO 04 - ON On 04 O o o o o O o o o O o o O o ON ^r co o o O in On On ON , o m co NO oo nO NO nO NO 00 CO co fN d 1 d Nf” o- _ 04 fN 04 ON ! CO CO o o O o o o o O o O o o o o — co N" 'd- fN ON d- in (N in o o o o- o o NO od d NO of 00 d; 04 co co co co in ih d fN fN co CO •'Cf fN o O o O O o o o o o o o o o _ o co CO NO CO o NO o o o co o o | d in in co in in d in d co fN o fN co fN o o O o o o o o o o o o o o m co i> NO o o o o o o o o o ON cO d 00 LO CO 1 ih _ ON m in fN o O o o o o o o o o o o o o ON CO cd d .2 cd cd d 5 tu cd cd cd cd o D, cd 2 CU o -d o cd 0) S-I -d d o (U "o Ih 0 o cd E cu a o u to cd d o o .5P s 53 2 cd s 'C cd o cu cu o "d jd o cu cd o cf> o a cu a 0 52 cu c 2 a £ cu cd u <0 a H 2 a O X < U O U CQ X Q o o nO m o o CO Of" o o n- o o oo O o fO O o LO LO o o o o ON co o o LO o o nO oo o o ON co < H o H TOTAL (%) 8.55 28.86 4.39 8.55 2.41 12.06 9.43 25.88 1.54 9.43 100 Table IX- Composition of thè fauna at station 3 at thè various times of sampling 42 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) in nT ON o n o o o o o o o in o o sO i— ' nj- Ni- o in o o o o o o co o o n}- o oo d i— H d d d d d d in ,~ o (N m LO in NO o in o o o o o o o n oo NT nO oo i — i >— i ▼— ! CO o vO nO ON o o o o o o o o o n o n Q no in ni (N ni vO n cd o NO n6 ; T— 1 in co ni NO ni co co in vO o vO* oo O m o o o o o o o o o NO o m (N co o q in no n ni o co in co co co n O nO Nf o n o o o o o o o _ o _ Q m oo ni n- in oo ni o q co in (O NO in ni co LO o oo o ni co 00 o o o o o o o o o n- o Nf co nO d d ni o q *— < ni in *— i +2 •*— < co ON __ n ni co oo n- o o o o o o o o o oo o oo Q On OS Nf- co o n- rn ni Nf NO Nf ON CO On n}- co n ni Nf (N rn of nO o o o o o o o o o _ o sO d s C cd a cu o d jd a cd co a 3 B 0,800-1,000 □ 0.600-0,800 M 0,400-0,600 H 0,200-0,400 B 0,000-0,200 left bank Figure 3 - Graphic representation of thè Dominance index 12/12/90 08/05/91 St. 1 St. 2 St. 3 St. 4 Stations 26/06/91 St. 5 w fi) 3 ■o a 2,000-2,500 □ 1,500-2,000 B 1,000-1,500 H 0,500-1,000 B 0,000-0,500 righi bank Figure 4 - Graphic representation of thè Diversity index of Shannon 48 Boll Soc . Natur. Napoli - Voi. 101 ( 1992-1993 ) 26/06/91 St. 1 St. 2 St. 3 St. 4 St. 5 Stations Figure 5 - Graphic representation of thè Diversity 12/12/90 c n a> 26/02/91 ■§ CD w m 2,000-2 ,500 □ 1 ,500-2 ,000 ■ 1,000-1 ,500 a 0,500-1 ,000 m o o o p ò ,500 left bank index of Shannon Equality 01/10/90 12/12/90 26/02/91 08/05/91 St. 2 St. 3 St. 4 Stations 26/06/91 St. 5 m 0,800-1 ,000 □ 0,600-0 ,800 ■ 0,400-0 ,600 m 0,200-0 ,400 a o o o p ó ,200 righi bank Figure 6 - Graphic representation of thè Equality index 49 Soppelsa O., Battaglini F. e Battaglini P. Equality 12/12/90 26/02/91 08/05/91 St. 2 St. 3 St. 4 Stations 26/06/91 St. 5 co fi) 3 H 0,800-1,000 □ 0,600-0,800 B 0,400-0,600 H 0,200-0,400 Il 0,000-0,200 left bank Figure 7 - Graphic representation of thè Equality index River pollution due to preserved food industries must therefore be added to thè more serious and steady contribution of tanning industries. The different Dominance, Equality and Diversity index values suggest that thè part of river between thè inflow of thè Cavaiola stream and thè mouth of thè river is thè most damaged, even if a light recovery is observed in its terminal part. In fact, according to Odum (1973), thè Diversity index is low in physically controlled ecosystems, i.e. subject to highly restrictive chemical-physical factors, while it is high in biologicallv controlled ecosy¬ stems. Thus, a higher Diversity means more complex feeding networks, more cases of symbiosis and more possibilities of a negative feedback control, which reduces variations and increases stabilitv. The Diversity index of Shannon clearly shows this zonation of popula- tions too. In view of thè above, it can thus be stated that along thè examined part of thè Sarno river it is possible to identify three areas with different species and different quantities of animals collected for each species. The first area can be identified by stations 5 and 4L. It is thè richest in phyla and its faunistic structure can be included among thè mesosaprobic alpha and beta classes of V. Sladecek’s System (1965). The second area is 50 Boll. Soc. Natur. Napoli - Voi 101 (1992-1993) thè most damaged by thè pollution. It includes thè part downstream from thè inflow of thè Cavaiola river and can be defined as metasaprobic. The third and last area can be identifìed by stations 3, 2 & 1. This area has strong polisaprobic features. Having used research methods adopted in some previous studies (Battaglini et al., 1968, 1971, 1979), thè conditions of thè Sarno river in 1979 could be compared with its current conditions. Compared data show a generai worsening in thè conditions of thè river. Polluting elements cannotbe eliminated, thus causingthe accumula- tion of toxic mud on thè bottoni and thè subsequent moving away from normal conditions, i.e. conditions preventing thè growth up of a typical river environment benthofauna. Significant seasonal variations of waste are another obstacle to thè formation of well defined biocoenose (d'Elia, 1988). The pH is almost unchanged, but NH| and nitrous nitrogen concen- trations have increased, confirming a higher inflow rate of organic origin. Even more worrying is thè fall of thè dissolved oxygen concentration from mean values of approximately 3.3 mg/L in 1979 to approximately 0.6 mg/L. This is likely to be thè cause of thè decreased specific Diversity. As regards total hardness, thè concentration doubled at all stations and in all sam- plings. The worsening and thè increase in thè concentration of polluting substances is also caused by thè increased exploitation of thè springs, so that most of thè spring waters are conveyed to be used as drinking water. Considering animai communities as a whole, thè first things to be noticed are thè strong decrease in thè number of taxa and thè lower number of single animals. The disappearance of some taxa, such as Gastropods, is clearly due to thè worsening of all environmental condi¬ tions. Only Dipterans larva were collected among thè Arthropoda. Some particularly resistant species as Turbeilari (Steno stormirvi sp., Mesostoma sp., Microstomnm sp.), Rotifera (Rotaria neptunia) and Nematoda can stili be found in thè river. The species variety is heavily reduced among thè taxa too. Only species typical of metasaprobic or, at thè most, polysaprobic environments can survive (Liebmann, 1951). As a matter of fact, thè only species of Oligochaeta found is thè Tubifex tubifex. The zoocoenose of thè downstream part and up to thè mouth of thè Sarno river consists of few species - all adapted to typical polysaprobic environment conditions - whose distribution is determined by thè inflow of thè Cavaiola stream. The faunistic data are perfectly consistent with thè 51 Soppelsa O., Battaglini F. e Battaglini P. chemical-physical parameters and lead to thè sarne two basic types of polluting reasons: thè massive number of industries and urban waste. Station 5 stili maintains acceptable conditions confirmedby a not very high Dominance vaine and an almost suffìcient Diversity. From thè con- fluence of thè Cavaiola stream onwards there is a “zonation” even in thè case of thè little Sarno river. In fact, thè waters of this tributary are a reai ecological barrier against thè diffusion of animals. Dominance indexes rise substantially while Diversity indexes decrease, thus revealing thè highly stressing condition. The comparison between thè current data and those previously collec- ted by one of thè Authors (Battaglini et al., 1968) shows a generai worsening of thè conditions of thè river, Anthropogenic polluting elements cannot be eliminated, thus causing thè accumulation of toxic mud on thè bottom and thè subsequent moving away from normal conditions. All this prevents thè growth of a typical river environment benthofauna, also because of thè strong seasonal variations in thè type and quantity of waste. Acknowledgements The present study was supported by a contribution of Italian MURST (40 & 60%) REFERENCES AA.VV. (1989) Standard methods for thè examination of water and wastewater. American Public Healt Association. New York. Battaglini, P. (1979) Aspetto ecologico delle comunità animali del Fiume Sarno (Campania). Rend. Ass Se. Fis Mat. Soc. Naz- Se. Leti. Art., Sez. IV, 46: 1-34. Battaglini, P., Percuoco, G. (1967) Osservazioni ecologiche della fauna limnologi¬ ca del lago craterico di Astroni (Campi Flegrei). Boll. Soc. Nat. in Napoli, 76: 695-771. Battaglini, P., Pierantoni, A., Percuoco, G. (1967) Ricerche sulla fauna del Sarno. I) Descrizioni del corso d’acqua e dati popolazionistici sugli invertebrati della sorgente ed alto corso. Boll. Soc . Nat. in Napoli, 76: 695-771. Battaglini, P., Pierantoni, A., Percuoco, G. (1968) Ricerche sulla fauna del Sarno. II) Studio ecologico di una zona del corso inferiore. Boll. Soc. Nat. in Napoli, 77:481-497. Bianucci, G., Bianucci, E. R. (1982) Il trattamento delle acque inquinate. Hoepli, Milano. Bianucci, G., Bianucci, E. R. (1980) L’analisi chimica delle acque naturali ed inquinate. Hoepli, Milano. 52 Boll. Soc . Natur . iVapo/i - Vo/. 101 (1992-1993) cTElia, E. (1988) L’inquinamento delle acque del bacino del Fiume Sarno. Stato di fatto e interventi di risanamento. Università degli Studi di Napoli, Napoli. d’ELiA, E., Mendia, L., Troncone, M.R. (1974) Condizioni di inquinamento del comprensorio del Fiume Sarno. Istituto di Ricerca sulle Acque, Napoli. Liebmann, H. (1951) Handbuch der Frishwasser und Abwasser Biologie. Verlag R. Oldenbourg, Miinchen. Odum, E.P. (1973) Principi di ecologia. Piccin, Bologna. Pielou, E. C. (1966a) Species-diversity and pattern-diversyity in thè study of ecological successions. J. Theoret. Biol., 10: 370-383. Pielou, E. C. (1966b) The measurement of diversity in different types of biological collections. /. Theoret. Biol., 13: 131-144. Pielou, E. C. (1966c) Shannon's formula as a measure of specific diversity: its use and disuse. Amer Nat. , 100: 463-465. Sladecek, V. (1965) The future of saprobity System. Hydrobiologia, 25: 518-537. Boll Soc . Natun Napoli - Voi 101 (1992-1993): 53-63 53 Bionomics of Myopites stylata F. (Diptera, Tephritidae) and its naturai eri em ics in Vivara island (Gulf of Naples) Fimiani P., Digilio M.C.1 Dipartimento di Biologia, Difesa e Biotecnologie agro-forestali, Università degli Studi della Basilicata, Via Nazario Sauro 85, 85100 Potenza, Italy Dipartimento di Entomologiae Zoologiaagraria, Università degli Studi di Napoli «Federico II» Via Università 100, 80055 Portici (Na), Italy Key words: Inula, host alternation, Bactrocera (Dacus) oleae. Abstract. Myopites stylata F. (Diptera, Tephritidae), is a gall-forming fly living on thè composite Inula viscosa Aiton. The bionomy and parasitoid complex of this insect species were studied in Vivara, a small island in thè Gulf of Naples. M. stylata adults always emerged from thè second half of September to thè end of October. The parasitoid species obtained were different Chalcidoids (Hymenoptera): two undetermined species of Habrocytus Thomson, belonging to albiformis Walker group (Pteromalidae), Eupelmus urozonus Dalman (Eupelmidae), Torymus cyani- mus Boheman and Dimeromicrus kiesenwetteri Mayr (Torymidae), Eurytoma tibia- lis Boheman (Eurytomidae). The role and effectiveness of E. urozonus as a possible naturai control agent of thè Olive Fly, Bactrocera (Dacus) oleae (Gmelin) is at present not well defined. However, in this study M. stylata, compared with other Mediterranean areas, resulted an important alternative host for E. urozonus. Riassunto. Bionomia di Myopites stylata F. (Diptera, Tephritidae) e dei suoi nemici naturali nell'isola di Vivara (Golfo di Napoli). Il presente lavoro riporta alcuni dati bionomici su Myopites stylata F. (Diptera, Tephritidae) e sul complesso dei suoi nemici naturali nell'isola di Vivara (Golfo di Napoli). Lo studio è stato effettuato mediante raccolta dei capolini fiorali della Composita Inula viscosa Aiton, trasformati in galle dall’azione del Dittero. Dalle galle sono sfarfallati il Tefritide ed i parassitoidi relativi, tutti appartenenti alla superfamiglia Chalcidoidea (Hymenoptera). Le specie ottenute sono: Torymus cy animus Boheman e Dimeromicrus kiesenwetteri Mayr (Torymidae), Eurytoma tibialis Boheman (Eurytomidae), due specie non determinate del genere Ha¬ brocytus Thomson, appartenenti al gruppo albiformis Walker (Pteromalidae), e Eupelmus urozonus Dalman (Eupelmidae). I parassitoidi sono sfarfallati lungo un arco di tempo piuttosto lungo, mentre gli adulti del Dittero nel periodo settembre- ottobre, coincidente con la fioritura dell’inula a Vivara. Il parassitoide quantitati¬ vamente più importante è risultato Habrocytus spp. Anche E. urozonus si ritrova in quantità notevole, contrariamente ad altre aree mediterranee dove alcuni Autori hanno ottenuto pochi o nessun esemplare di questo parassitoide dalle galle di I. viscosa. A Vivara, quindi, M. stylata costituisce un importante ospite alternativo di E. urozonus, che potrebbe quindi risultare utile, nonostante le complesse intera- Received 24.4.92, accepted 8.2.93 Boll . Soc. Natur. Napoli - Voi. 101 ( 1992-1993 ) zioni con gli altri parassitoidi, nel controllo naturale della Mosca dell'olivo, Bactrocera (Dacns) oleae (Gmelin). Introduction The mediterranean maquis in Vivara island (Gulf of Naples) is a naturai environment free of antropic influence, which offers interesting opportunities for ecological studies (Fimiani, 1977; 1981). The features of this island are reported in a special issue edited by Regione Campania (1981). A list of thè insect species living on Vivara island, collected with sweeping nets, is available (D'Antonio & Fimiani, 1988). Myopites stylata F. (Diptera, Tephritidae) lives exclusively on thè composite Inula viscosa Aiton, where it produces galls from flowers (Fig. 1). /. viscosa is common in thè Mediterranean area, where it is often associated with olive groves. Myopites females typically lay their eggs in flower ovaries, by introducing thè ovipositor through thè corollar tube. The hatching larva penetrates into thè flower receptacle, which gradually becomes hypertrophic, and finally is transformed in a wooden-plurilocular gali, with special tubercles in place of thè achenes. The association between inules and olive trees was investigated in Italy by Martelli (1910), Bua (1938) and Silvestri (1940), then in Greece by Isaakidès (1955; 1957), in Corse (Féron et al., 1961) and Continental France (Delanoue & Arambourg, 1965), and more recently in Crete (Neuen- schwander et al., 1983). The importance of ecological studies on thè relationship between spontaneous vegetation and olive tree is also recently emerged in thè last OILB Working Group on Fruit Flies, held in Sassari in November 1990 (unpubk). The present note aims at defining thè naturai enemy complex of M. stylata in Vivara, trying also to assess in this environment thè role of inule as a naturai reservoir of Bactrocera ( Dacus ) oleae (Gmelin) parasitoids in olive orchards. Materials and methods The galls were collected once a year from 1982 to 1985, in October, January, November and May respectively in thè four years of thè study. The samples were kept in thè laboratory for over one year to recover all thè Fimiani P„ Digilio M.C. 55 emerging adult flies and parasitoids. In 1982, galls were cumulatively stored in plastic boxes (cm 20 x 30 x 10) closed with a fine gauze. For all thè Figure 1 - Myopites stylata F. gali on Inula viscosa Aiton. 1, 2. Gali formation. 3. Gali completely formed. 4. M. stylata mature larva. remaining years of thè study thè galls were individually stored in glass vials (cm 10 x 0.6) plugged with cotton wool. Part of thè collected galls were also dissected. Adults emerging from galls stored in thè boxes were periodically collected for species identifìcation, while those isolated in thè vials were weekly collected to assess thè time distribution of adult emergence trends. Results and discussion The total number of both fly and parasitoid specimens obtained in thè different years of study is reported in Table I. The parasitoid complex is 56 Boll. Soc. Natur. Napoli - Voi 101 (1992-1993) illustrateci in Table IL The relative abundance of parasitoids emerging from thè galls is shown in Table III. For M. stylata a sex ratio nearly equal to 0.5 was recorded (Tab. I). The adults of this species mostly emerged Table I - Myopites stylata and parasitoids emerged from collected galls. collecting vears 1982 1983 1984 1985 collected galls 530 159 80 43 active galls 124 59 43 Number per sex d’c? 99 dcf 99 dd 99 0 99 Myopites stylata F. 176 151 99 92 40 30 26 20 total parasitoids 668 484 64 130 56 31 13 21 Habrocytus spp. 618 421 40 82 45 27 4 7 Eupelmus urozonus Dalman 13 28 6 21 - - 9 13 Torymus ?cy animus Boheman 8 10 11 1 1 4 1 - 1 Dimeromicrus kiese.nwetteri Mayr 8 14 5 13 6 2 - - Eurytoma tibialis Boheman 21 11 2 3 1 1 - - ' For this collection it was not possible to know thè number of active galls, i.e. thè galls yielding adults, both flies or parasitoids. during thè second and third week of September (Figs. 2, 3), apart from a few individuate emerging through October. For isolated galls it was possible to assess that in average several flies and parasitoids were in most cases present for each inhabited gali (Tab. IV). However, thè galls which did not yield any insect, not even thè Tephritid who had caused thè gali formation, were 22% in 1983 and 26% in 1984 (Tab. I). In fact, upon dissection of galls collected in November, we observed that in some cases they were absolutely empty. Pteromalids Two species of Habrocytus Thomson were obtained, differing in marginai vein length and slightly in colour. Habrocytus spp. was usually thè most abundant species (Tab. III). Its relative abundance ranged from 32.3% up to 90.2%, and was always thè highest except in May 1985, when Eupelmus urozonus Dalman exceeded p.. M ( ' 40 30 20 10 0 -Q .Q _Q JQ ffl ® 0 © © © © a a u ii ii u S5S5<<<< « « « « >.>.>. >^ E O. CL Q, Q, CO CO co co 3 - - - - - -2222n^ ^ ▼“ CSJ CO ^ C\J C\l e\i □ Eurytoma Wk Dimeromicrus □ Torymus H Eupelmus ■ Habrocytus N O N ^ O ffl ^ OJ CO T- CM W Figure 2 - Emergences of Myopites stylata parasitoids. Collection of January 1983. e\i oa Torymus Eupelmus Habrocytus Figure 3 - Emergences of Myopites stylata parasitoids. Collection of November 1984 (left) and May 1985 (right). The galls of both these collections are produced by Tephritids emerged in September-October 1984. Boll Soc. Natur. Napoli - Voi 101 (1992-1993) Table II - The parasitoid complex. parasitoid family and subfamilv feeding behaviour host Habrocytus spp. albiformis Walker group Pteromalidae Pteromalinae ectophagous polyphagous Eupelmus urozonus Dal man Eupelmidae Eupelminae ectophagous poliphagous Tory mas ?cy animus Boheman Torymidae Toryminae ectophagous Tefritid galls on Composites Dimeromicrus kiesenwetteri Mavr Torymidae Monodontomerinae ectophagous Tefritid galls on Composites Eurytoma tibialis Boheman Eurytomidae Eurytominae endophagous Tefritids galls on Composites Table III - Relative abundance of parasitoids emerged from Myopites stylata galls collecting vears 1982 1983 1984 1985 Habrocytus spp. 90.19 62.89 82.76 32.35 Eupelmus urozonus Dalman 3.56 13.91 - 64.71 Torymus ?cy animus Boheman 1.56 1 1.34 5.74 2.92 Dimeromicrus kiesenwetteri Mavr 1.91 9.28 9.2 - Eurytoma tibialis Boheman 2.78 2.58 2.3 - Table IV - Average number of Myopites stylata andparasitoids emerged from one gali . collecting vears M. stylata x ± sd parasitoids x ± sd N. 1983 1.54 + 1 .62 v 1.57 + 1.17 124 1984 1.19 ± 1.40 1.47 ± 1.18 59 1985 1.07 + 1.08 0.79 + 0.94 43 Fimiani P., Dìgiììo M.C< 59 thè number of Pteromalids present in our samples (Tab. III). The adult emergence was mainly registered from January until May (Fig. II, III) and, in 1983, to a lower extent also in September-October (Fig. 2). Habrocytus trypetae Thomson is reported both as an ectoparasitoid of Tephritid larvae and as a hyperparasitoid on Enrytoma curta Walker (Varley, 1937). The possible occurrence of similar ecological relationships in thè case of thè Habrocytus spp. that we found in Vivara remains to be evaluated. In Central (Terracina, Latina, Lazio) and Southern Italy (Cala¬ bria) Habrocytus was already reported as thè most common parasitoid found on M. stylata (Martelli, 1910). The high relative abundance of Pteromalids has been reported also by Féron et al. (1961) for Corsica. In this case an undetermined species of Pteromalus accounted for 40% of thè total insects collected. In contras!, Habrocytus sp. was only rarelv reared from Myopites galls collected in thè Marche region (Rivosecchi, 1960a). However, this different situation could be partly due to thè fact that thè host species were Myopites biodi Brébisson and M. frauenfeldi Schiner. Eupelmids In this group, thè only represented species is Eupelmus urozonus Dalman. The relative abundance of this species varies depending on thè collection periods, reaching up to 64.7% (May 1985 collection, Tab. III). E. urozonus emerged at thè same time as Habrocytus , with thè last flights recorded in October (Figs. II, III). No E. urozonus is obtained from thè November 1984 collection (Tab. III). While some authors (Isaakidès, 1955, 1957) consider M. stylata as a valid alternative host for E. urozonus , others did not (Fèron et al., 1961; Delanoue & Arambourg, 1965; Neuenschwander et al., 1983). In fact, in Crete Neuenschwander et al. (1983) reported a low presence of this Chalcidoid (Tab. V). Their data are different from our findings (Tab. V). Fèron et al. (1961) reported that M. stylata galls collected in Corse in September did not yield any E. urozonus ; but, because thè absence of spontaneous vegetation resulted in a higher rate of olive fly infestation, they suggested a possible positive role of wild plants, such as inules, in olive groves, as naturai reservoirs of Eurytoma sp. In Vivara too we found that no or few E. urozonus emerged from thè samples collected in autumn (October 1982 and November 1984), then reports of Corse are not really in disagreement with Vivara ones. 60 Boll. Soc . Natur. Napoli - Voi 101 (1992-1993) Table V - Eupelmus urozonus adults emerged from 100 galls. ° from Neuenschwan- der et al. , 1 983. localities ratios dates of collection Crete 2.98 December ° Vivara 7.74 October 1982 Vivara 16.98 January 1983 Vivara 51.16 May 1985 Delanoue & Arambourg (1965) found that E. urozonus presents a different oviposition behaviour on M. stylata and on D. oleae. The existen- ce of biotypes adapted to different hosts would prevent a shift between thè two Tephritids. Torymids Torymids were always present in low numbers in our samples, with a relative abundance ranging between 1.6% and 11.3% (Tab. 3). Adult emergences of Torymids species started in January, about at thè same time as Habrocytus , and thè highest values were registered in February-March (Figs. 2, 3). In Marche region (Rivosecchi, 1960b) Dimeromicrus kie- senwetteri Mayr early in thè season shows a few generations on Myopites blotii Brébisson and M. frauenfeldi Schiner, and afterwards it develops and overwinters on M. stylata galls on I. viscosa, since these galls are persistent during winter. Varley (1941) observed in Torymus cy animus Boheman a tendency to superparasitism : thè female commonly lays many eggs in one host, leading to a high mortality rate, which might account for thè low presence of T. cyanimus adults recorded in Vivara. Superparasitism occurrence has been reported also for D. kiesenwette- ri : adult females of this species were found to lay up to 10 eggs per host; D. kiesenwetteri successfully developed also as an ectophagous hyperparasite on Eurytoma curta larvae (Rivosecchi, 1960a). On thè Adriatic coast (Rivosecchi, 1960b) D . kiesenwetteri is a common parasitoid of Tephritids, particularly of species of thè genus Myopites Brébisson. Fimiani P., Digilio M.C. 61 Eurytomids Eurytoma tibialis Boheman (= E . curia Auct., nec Walker) was obtai- ned only in a few specimens (Tab. Ili), which scatteredly emerged in different periods of thè year (Figs. 2, 3). The similarity of emergence times observed for parasitoids in thè different years of thè study, in spite of laboratory Storage of galls, and, in most cases, thè significant association with thè life cycle of thè host seem to suggest thè possible existence of diapause. However, Neuenschwander et al. (1983) after recording thè onset of E. urozonus emergence in December, concluded that diapause in Crete is less severe than in Conti¬ nental Greece (Louskas, in Neuenschwander et al., 1983). Rivosecchi (1958) compared hibernating larvae of two parasitoids of Tephritis stictica Loew, Eurytoma tristis Mayr and Ormyrus hungaricus Erdos, kept at room temperature, at 25 °C and at 30°C, and noticed that exposure to higher temperatures fastens thè development rate, causing pupation to occur much in advance in respect to parasitoids stored at lower temperatures. For M. stylata thè diapause regulated developmental arrest is much more evident. In fact Myopites pupae collected in Vivara in November, in galls not yet completely formed, did not develop into adults until thè occurren- ce of /. viscosa flowering, only 10 months later. For isolated galls it was possible to assess that in average several flies and parasitoids were in most cases present for each inhabited gali (Tab. 4). In conclusion, thè results show that in Vivara island /. viscosa can be an effective naturai reservoir for E. urozonus, which might be useful in thè naturai control of thè olive fly, B. oleae. Acknowledgments Thanks are due to Prof. G. Viggiani and Prof. P. Mazzone (Dipartimen¬ to di Entomologia e Zoologia agraria, Università degli Studi di Napoli Federico II) and to Prof. L. Rivosecchi (Istituto Superiore di Sanità, Roma) for advice in parasitoid (G. V. and P. M.) and Tephritid (L. R.) identifica- tion. Prof. E. Tremblay (Dipartimento di Entomologia e Zoologia agraria, Università degli Studi di Napoli Federico II) is gratefully acknowledged for his interest to this research. 62 Boll Soc . /tewr. Napoli - Voi 101 (1992-1993) REFERENCES Bua, G., 1938. Contributo alla conoscenza dei parassiti temporanei della Mosca delle olive ( Dacus oleae GmeL). L’Olivicoltore, 9: 3-5. D'Antonio, C. & P. Fimiani, 1988. Approccio ad un inventario entomofaunistico dell’isola di Vivara (Na). Nota preliminare. Animar. Ist. Museo Zool. Univ. Napoli, 26: 155-170. Delanoue, P. & Y. Arambourg, 1965. Contribution à l’étude en laboratoire d ’Eupel- mus urozonus Daini. (Hym. Chalcidoidea Eupelmidae). Ann. Soc. Ent. Fr., (N.S) I: 817-842. Feron, M., Benard, R. & S. Poitout, 1961. La mouche de l’olive, Dacus oleae Gmel. et ses parasites en Corse en 1959 et 1960. Entomophaga, 6: 173-183. Fimiani, P., 1 977. Aspetti entomologici della biocenosi olivicola dell’isola di Vivara. Trifoglio Natura, 7: 22-28. Fimiani, P., 1981. Aspetti fenologici e biologici negli Insetti dell'isola di Vivara.- In Vivara Oasi di Protezione Naturale. Giunta regionale della Campania: 51-68. Isaakides, C.A., 1955. La lutte biologique contre la mouche des olives en Grèce. Pragm. Akad. Athen., 22: 1-19. Isaakides, C.A., 1957. Sur la lutte biologique contre le Dacus oleae Rossi. Entomo¬ phaga, 2: 245-249. Martelli, G., 1910. Materiali per la conoscenza dei parassiti della Mosca delle olive. IL Myopites limbardae Schiner. Boll. Lab. Zool. gen. agr. Portici, 4: 303-306. Neuenschwander, P., Bigler, F., Delucchi, V. & S. Michelakis, 1983. Naturai enemies of preimaginal stages of Dacus oleae Gmel. (Dipt. Tephritidae) in Western Crete. I. Bionomics and phenologies. Boll. Lab. Ent. agr. Filippo Silvestri, 40: 3-32. Regione Campania, 1981. Vivara Oasi di Protezione Naturale. -Giunta regionale della Campania: 182 pgs. Rivosecchi, L., 1958. Note sui parassiti dei Tripetidi. I. Eurytoma tristis Mayr e Eurytoma hungaricus Erdòs (Hymenoptera Chalcididae). Boll. Lab. Zool. agr. e Bachic., I: 187-208. Rivosecchi, L., 1960a. Note sui parassiti dei Tripetidi: Dimeromicrus kiesenwetteri Mayr (Chalcidoidea, Torymidae) ed altri Calcidoidei del litorale marittimo delle Marche. Parassitologia, 2: 287-293. Rivosecchi, L., 1960b. Note sui parassiti dei Tripetidi. IL Dimeromicrus kiesenwet¬ teri Mayr (Chalcidoidea, Torymidae) parassita di larve del gen. Myopites Brèbisson. Boll. Zool. agr. e Bachic., s. II, 3: 179-200. Silvestri, F., 1940. La lotta contro la mosca delle olive. In Atti del Convegno Nazionale di Olivicoltura, Bari, 21-22 settembre 1938, 2: 56-82. Varley, G.C., 1937. Description of thè eggs and larvae of four species of Chalcidoid Hymenoptera parasitic on thè knapweed gall-fly. Proc. R. Ent. Soc. London (B), 6: 122-130. Varley, G.C., 1941. On thè search for hosts and thè egg distribution of some Chalcid parasites of thè knapweed gall-fly. Parasitology , 33: 47-66. Boll Soc. Natur. Napoli - Voi 101 (1992-1993): 63-72 63 Immunocytochemistry of carbonio anhydrase in thè chick embryo membranous labyrinth during development Avallone B., Balsamo G., Marmo F. Cattedra di Istologia ed Embriologia Dipartimento di Genetica, Biologia generale e Molecolare Università degli Studi «Federico II», Via Mezzocannone 8, 80134 Napoli, Italv Key words: Immunocytochemistry, Carbonic-anhidrase, Embryo, Labyrinth. Abstract. An immunocvtochemical studv with polyclonal antibodies was carried out with thè aim to localize carbonic anhydrase (CA) isozymes CA I and CA II in thè various cells of chick membranous labyrinth during development. Our data indicate that CA I and CA II are localized in thè same cells in thè chick embryos. In fact CA I and CA II are diffuselv localized in thè membranous labirinth bud during thè early developmental stages, successivelv thè sensorial epithelium of thè maculae acusticae and crista ampullaris stronglv stained bv thè immunocvto- chemical procedure. Cochlear and vestibular dark cells consistentlv appeared stained for CA I and CA II. The epithelial cells of thè endolymphatic sac and of thè brain choroid plexus were similarlv stained for both isozymes. In one day and one week chicken CA was visualized immunocvtochemically in thè same sites as at advanced embryo n al stages. It is suggested that these findings are related to otolith formation and maintenance, as well as to fluid and ionie flux in thè endolymph. Riassunto. Studi Immunocitochimici sull’anidrasi carbonica del labirinto membranoso deH’embrione di pollo durante lo sviluppo. È stato condotto uno studio con anticorpi policlonali allo scopo di localizzare gli isoenzimi dell’anidrasi carbonica (CA) CA I e CA 11 nel labirinto membranoso del pollo durante lo sviluppo. I dati indicano che negli embrioni, già dai primi stadi di sviluppo i due isoenzimi sono diffusamente presenti nell’epitelio otocistico e succesivamente nell’epitelio sensoriale delle creste ampollari e delle macule acustiche, come a livello delle cellule scure del vestibolo e del tegmentwn vasculosum. Sono, inoltre, positivi alla reazione immunocitochimica per i due isoenzimi anche l’epitelio del sacco endolinfatico e dei plessi corioidei. Nei pulcini di un giorno e di una settimana la localizzazione dell’enzima è sovrapponibile a quella degli embrioni in cui è presente un buon differenziamento del labirinto membranoso. Gli Autori correlano tali reperti con l’azione dell’enzi¬ ma nella morfogenesi e nel riassorbimento degli otoliti e con l’intervento dello stesso nel flusso di ioni e di fluidi delTendolinfa. Received 27.1 1.92, accepted 16.6.93 64 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) Introduction Carbonio anhydrase (CA) catalyses thè reversible reaction between carbon dioxide and water to form carbonio acid which spontaneouslv dissociates into bicarbonate and hvdrogen ions. CA is known to be involved in several cellular functions, such as C02 removai from red blood cells, acidifìcation of secreta in thè parietal cells of thè gastric mucosa, selective release of K+ and resorption of NA+ and water in thè kidney tubules. CA is also responsible for thè production of aqueous humor in thè eye ciliarv bodies, of cerebrospinal fluid in thè choroid plexus, and of endolymph in thè stria vascularis of thè inner ear (Watana- be, 1963; Lim et al., 1983; Hsu & Nomura, 1985). In addition, there is convincing evidence that CA may be involved in thè deposition of calcium carbonate in thè shell of molluscs (Wilbur & Jodrey, 1 955) and chick eggs (Hodges & Lòrcher, 1 967), and, as regards thè membranous labyrinth, in otoconia formation in chicks (de Vincentiis & Marmo, 1968; Fermin and Igarashi, 1986), mice (Purichia & Erway, 1972), and Bufo bufo tadpoles (Campantico, 1968). Cytochemical CA localization in inner ear tissues was studied in thè guinea pig and thè rat bv Watanabe (1963), thè chick embryo bv Marmo (1966), thè chinchilla by Lim et al. (1983), thè guinea pig by Hsu and Nomura (1985) and Takumida et al. (1989a). Biochemical investigations by Erulkar and Maren (1961) in thè cat inner ear demonstrated that thè highest CA concentration is in thè co- chlear duct; moreover, Drescher (1977) found CA similar to that from red blood cells in thè membranous labyrinth of mammals. So far 7 isozymes of CA have been separated (Kaunisto et al., 1990). They can be localized individuali by thè immunocytochemical approach, which is much more sensitive and specific than thè cytochemical techni- ques currently used, in particular those aimed at detecting CA, which are constantly subject to criticism. Therefore, we availed ourselves of this technique, using polyclonal antibodies to localize CA I and CA II isozymes in thè chick membranous labyrinth during development, which had alrea- dy been investigated cytochemically by Marmo (1966). We also tried to elucidate their role in cells with different specialized functions, and in thè differentiation of thè inner ear structures mostlv occurring during embryo development. \ ì-.tii, <■'. /■' fu.. ! C. j ?-; ■ *« ■:> : ' I I : : v HIMMì 65 Material and methods Chick embryos at 2, 5, 7, 9, 11, 13 days of incubation (stage 12-39, according to Lilìie, 1952), as well as 1 day and 1 week old chicks were used. The embryos were removed in normal saline, fixed in Carnoy and embed- ded in paraffim The membranous labyrinths were taken from chicks after anaesthesia and decapitation, and subjected to thè sanie procedure. In Figure 1 - Three day chick embryo. Diffuse positivity can be observed in thè otocyst (OT) (small arrow) and in thè epithelium cells of thè acoustic ganglion bud (AG) (large arrow). PAP CAI.X 144 order to localize CA, thè direct, indirect and peroxidase-antiperoxidase (PAP) methods were used. Depara i il ned and rehydrated Spiri sections were incubated in 3% H202 for 5 min in order to inactivate endogenous peroxidase, and then pretreated with normal rabbit serum (1:20) for 30 min to block thè fragment crystallizable (Fc) receptors of ìmmunoglobuli- nes. The polyclonal antibodies (Serotec, Oxford, England) used were: peroxidase labelled and un labe l! ed sheep an ti human CA I and CA II, and 66 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) peroxidase labelled and unlabelled rabbit anti-sheep IgG; thè sera were diluted 1:50 (CA I, CA II, IgG) 1:40 (PAP) in phosphate buffer saline (PBS) 0.1M pH 7.2, with 1% bovine serum albumin (BSA). Each step was carried out in a moist chamber at room temperature for Ih. In order to reveal peroxidase, sections were then incubated in 3,3’-dia- minobenzidine tetrahydrochloride (9 mg DAB in 15 mi PBS with 30% H202), and dehvdrated and mounted in Canada balsam. At thè same time, negative and positive control procedures were performed bv omitting thè primarv antibody on thè sample sections, and by using guineapig kidnev sections, respectivelv. Results Despite thè different methods used, our investigation provided consi- stent data. Thev demonstrated that thè two isozvmes, CA I and CA II, are localized in thè same cells; however, a quantitative studv was not carried out, and hence it was not possible to establish which is thè more abundant in thè various sites. Figure 2 - Five day chick embrvo. It can be seen diffuse positivity of thè otocvst (OT) epithelium. Endolvmphatic sac (ES). PAP CA II.X60. Avallone B., Balsamo G Marmo F. 67 In embrvos at thè otic pit stage, a diffuse positi vitv was observed in thè epithelium, which persisted in thè next stages until thè 9th day (Fig 1 and 2). This positivity was also present in thè celi cvtoplasm of thè acoustic ganglion bud. Figure 3 - One day chick: intenselv stained sensorial epithelium (SE) of thè utricle. The otolith matrix (small arrow) appears positive. Only one otolith is indicated (O). PAP CA II.X560 From thè llth day thè enzvme was mostly localized in thè sensorial areas of thè saccule, thè utricle and thè lagenae, where sensorial, suppor- iting, transitional and dark cells showed positivity to thè immunocvtoche- mical reaction. Positivity had also been observed in thè otoconial matrix since thè early formation of otoconial crystals in thè 7 dav embrvo (Fig. 3). The same distribution of thè enzyme was also evident in thè ampullar crests (Fig. 4). The localization of thè enzyme in thè epithelial cells of thè endolymphatic duct and sac was alreadv possible at early stages of develo- pment (5 days). Intense immunostaining was visualized in thè dark cells of tegmentum vasculosum (Fig. 5) and in thè supporting and sensorial cells of thè Corti organ. 68 Boll. Soc. Natur. Napoli - Voi 101 (1992-1993) Immunocytochemistrv also evidenced abundant carbonic anhydrase in thè neuron cytoplasm of cochlear and vestibular ganglia at each developmental stage (Fig. 6). In addition, a particularlv intense CA reaction Figure 4 - Five day chick embrvo. Intense positivitv can be observed in thè endolvmphatic sac (ES) epithelium. PAP CA II.X225 was also present in thè epithelium of thè choroid plexns, which are alreadv known to show a high CA content (Fig. 7) Discussion and conclusion Our observations showed that CA I and CA II are diffuselv localized in thè membranous labyrinth bud during thè earlv developmental stages; in later stages, instead, thev are restricted to thè areas where thev fulfil diverse and specialized functions. CA is present in thè areas (maculae) implied in otoconia production. The morphogenetic function of thè enzvme is demonstrated by both thè inhibition of otoconia morphogenesis, which has been observed in em- brvos treated with carbonic anhydrase inhibitors (Marmo, 1965; Campanti- 69 Avallone B., Balsamo G ., Marmo F. co, 1968; Purichia & Erwav, 1972; Kido et al., 1991), and bv thè role that thè enzyme plays in crystal resorption (Lim, 1983; Kawamata et al., 1986; Igarashi, 1989). Ultrastructural investigations aimed at localizing CA in thè Figure 5 - One day chick: tegmentum vasculosum. It is possible to distinguish between negative light cells (small arrow) and intenselv positive dark cells (large arrow). PAP CA II. X 144 vestibular organ of thè guinea pig have confirmed this function; in fact, they have demonstrated that thè globular structures (considered otoconia precursors) that are present in thè supporting, transitional and “planum semilunatum” cells are surrounded bv reaction products (Takumida et al., 1989 a,b). The morphogenetic role of CA in these sites is also supported by thè occurrence of thè enzyme in thè otoconial matrix which is alreadv present in thè embryo on thè early formation of otolithic crvstals. It is noteworthy that CA occurs also in cells involved in fluid and ion transportation, such as vestibular dark cells and thè epithelial cells of thè endolympatic sac and of thè coroid plexus ; an intense activitv of Na+ K+ dependent ATPase and adenylate cyclase has also been demonstrated in these cells (Hsu & Nomura, 1985). However, CA is also present in cells not 70 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) being involved in fluid and ion transportation, such as supporting cells, that, as suggested bv Lim (1983), may play an important role in thè respiratory mechanism of sensorial cells. Figure 6 - Thirteen day chick embrvo: vestibular ganglion (VG). Positivitv is evident in thè neuron cytoplasm (small arrow). PAP CA I.X60 Figure 7 - Thirteen day chick embrvo: choroid plexsuses. Positivitv is clearlv evident in thè epithelium (small arrow). PAP CA 11X225 Interestingly, unlike thè cytochemical data obtained by Lim et al. (1983) and Hsu and Nomura (1985) in thè maculae, thè cristae and thè Corti organ, our investigation evidenced an intense CA reaction not onlv in supporting cells, but also in thè sensorial ones. As regards more specifical- ly thè chick embrvo membranous labyrinth, our data showed that thè enzyme fails to disappear in 15 day embryos, in contrast to what was demonstrated in previous cytochemical studies (Marmo et al., 1966), but persists after hatching showing thè same localization as in thè embrvo at advanced stages of development. In conclusion, thè present study does not provide any clue to thè possible role played by CA in thè inner ear. Here CA activity is different in Avallone B., Balsamo G., Marmo F . 71 thè various celi types (“secretory”, supporting and sensorial cells) , and hence carbonic anhydrase might be a ubiquitous enzyme. CA might be involved in specialized functions only in thè cells showing intense enzyma- tic activity. Therefore, it could be suggested that this enzyme mav play several functions in thè inner ear: i) regulation of thè endolymph ions and/or fluids; ii) removai of C02 from inner ear tissues; iii) otoconia formation and maintenance; iv) influence on thè endolymphatic potential, in agreement with Prazma (1978) and Vozumi et al. (1991), as well as on thè neural stimulus spread, in view of its occurrence in thè cvtoplasm of acoustic ganglion neurons, as already suggested bv other investigators (Giacobini, 1961; Korhonen et al., 1964; Korhonen & Korhonen, 1965). REFERENCES Campantico, E., 1968. L'azione della diclorofenamide sulla deposizione dei sali di Ca del sacco endolinfatico di larve di Bufo bufo. C.N.R., 37: 866-868. Drescher, D.G., 1977. Purification of a carbonic anhydrase from thè inner ear of thè Guinea pig. Proc. Nati. Acad. Sci., 74: 892-896. Erulkar, S.D. & T.H. Maren, 1961. Carbonic anhydrase and thè inner ear. Nature, 189: 459-460. Fermin, C.D., Y. Igarashi, 1986. Review of statoconia formation in birds and originai research in chicks (Gallus domesticus). Scan. Electron. Micr., 4: 1649-1665. Giacobini, E., 1961. Localization of carbonic anhvdrase in thè nervous svstem. Science, 134: 1524-1525. Hodges, R.D. & K. Lorcher, 1967. Possible sources of thè carbonate fraction of egg shell calcium carbonate. Nature, 216: 609-610. Hsu, C.J. & Y. Nomura, 1985. Carbonic anhydrase activity in thè inner ear. Acta Otolaryngol. (Stockh) [suppl.J, 418: 1-42. Igarashi, Y., 1989. Submicroscopic studv of thè vestibular dark celi area in human fetuses. Acta Otolaryngol. (Stock), 107: 29-33. Kaunisto, K., S. Parkkila, T. Tammela, L. Ronnberg & H. Rajanieml, 1990. Immunohistochemical localization of carbonic anhydrase isoenzvmes in thè human male reproductive tract. Misto chemistry , 94: 381-386. Kawamata, J., Y. Harada & N. Tagashira, 1986. Electron microscopie study of thè vestibular dark cells in thè crista ampullaris of thè Guinea pig. Acta Otolarvn- gol. (Stock), 102: 168-174. Kido, T., T. Sekitani, H. Yamashita, S. Endo, Y. Masumitsu & H. Shimogori, 1991. Effects of carbonic anhydrase inhibitor on thè otolithic organs of developing chick embryos. Am. J. Otolaryngol . Head Neck Med. Surg., 12 (4): 191-195. Korhonen, L.K., E. Naatanen & M. Hyyppa, 1964. A histochemical study of carbonic anhydrase in some parts of thè mouse brain. Acta Histochem., 18: 336-347. 72 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) Korhonen, E. & L.K. Korhonen, 1965. Histochemical demonstration of carbonic anhvdrase activitv in thè eyes of rat and mouse. Acta ophthal, 43: 475-481. Lillie, FR., 1952. Development of thè chick. Ed. H. Holt and Company, New York. Lim, D.J., C. Karabinas & D.R. Trune, 1983. Histochemical localization of carbonic anhvdrase in thè inner ear. Am. J. Otolaryngol, 4: 33-42. Marmo, F., 1965. Osservazioni sulla morfogenesi degli otoliti dell'embrione di pollo in presenza di inibitori dell'anidrasi carbonica. Boll. Zool., 32: 231-238. Marmo, F., 1966. L’anidrasi carbonica del labirinto membranoso deH’embrione di pollo durante lo sviluppo. Acta Embryol. et Morphol. Exp., 9: 1 18-126. Prazma, J., 1978. Carbonic anhvdrase in thè generation of cochlear potentials. Am. J. Physiol., 235: 317-320. Purichia, N. & L.C. Erway, 1972. Effects of dichlorphenamide zinc and manganese on otolith development in mice. Devel. Biol., 27: 395-405. Takumida, M., D. Bagger-Sjoback, J. Wersall & J. Harada, 1989 a. Ultrastructural localization of carbonic anhvdrase in thè vestibular end organs of thè guinea pig. Arch. Otorhinolaryngol , 246: 56-60. Takumida, M., Y. Harada, D. Bagger-Sjoback & J. Wersall, 1989 b. Carbohydrates of thè Guinea pig vestibular supporting cells. Anris-Nasns-Larvnx(Tokyo) , 16: 133-142. de Vincentiis, M. & F. Marmo, 1968. Inhibition of thè morphogenesis of thè otoliths in thè chick embrvo in thè presence of carbonic anhvdrase inhibitors. Expe¬ ri entia, 24: 818-820. Vozumi, N., N. Mori & S. Sakai, 1991. The effect of acetazolamide on thè endolym- phatic sac DC potential. Acta Oto-laryngol , 3 (5): 921-925. Watanabe, Y., 1963. Influence of Diamox (acetazolamide sodium) upon inner ear and histochemical studv of carbonic anhvdrase. J. Otorhinolaryngol. Soc. Jpn., 66: 657-670. Wilbur, K.M., L.H. Jodrey, 1955. Studies on shell formation. V. The inhibition of shell formation bv carbonic anhvdrase inhibitors. Biol. Bull., 108: 359-365. 73 Boll. Soc . Natur. Napoli - Voi 101 (1992-1993): 73-87 Ocurrence of (3-endorphin- and enkephalin- like immunoreactivity in thè hypothalamus of thè domestic fowls, Gallus domesticus Esposito V., De Girolamo P., Sammarco M., Gargiulo G. Dipartimento di Strutture, Funzioni e Tecnologie Biologiche, Università degli Studi «Federico II», Via Delpino, 1, 1-80137 Napoli, Italv Key words: Immunocytochemistrv, hypothalamus, enkephalins, P-endorphin, Gallus domesticus. Abstract. The distribution of P-endorphin and enkephalin-like immunoreacti¬ vity in thè hypothalamus of 2-week-old domestic chicks was studied with immu- nocytochemical methods, using antibodies to p-endorphin, met-enkephalin and leu-enkephalin. P-Endorphin-like neurons were observed in thè nucleus infundibu- li whereas p-endorphin-like fibers were detected both in thè infundibular area and in thè external layer of median eminence. Enkephalin-like immunoreactive peri- karya were observed in thè parvocellular division of thè nucleus paraventricularis and in thè nucleus infundibuli. The enkephalin-like immunoreactive fibers were observed in every part of thè hypothalamus, but mainlv concentrated in thè infundibular area and in thè external layer of median eminence. The distribution pattern of both p-endorphin and enkephalins is compared with that other neu- ropeptides present in thè chick hypothalamus. The results are discussed in relation to thè possibility that both P-endorphin and enkephalins may be involved in hypophysial regulation or neuromodulator activity in thè hypothalamus of dome¬ stic chick. Riassunto. Presenza di immunoreattività P-endorfìna ed encefalino-simile nell’ipotalamo di Gallus domesticus. Nel presente studio immunocitochimico eseguito sulla regione ipotalamica di pulcini di Gallus domesticus secondo il metodo di perossidasi antiperossidasi, ha evidenziato la presenza di immunoreattività ad anticorpi per la metionina-encefali- na, leucina-encefalina e p-endorfina. Test di specificità hanno dimostrato “ cross" - reattività tra i due antisieri per le encefaline ed i rispettivi antigeni e tra l’antisiero per la P-endorfina e la p-lipotropina, per cui l 'immunoreattività appresso descritta è da considerarsi relativa a sostanze encefalinosimile e p-endorfina e/o P-lipotropi- nasimile. L'immunoreattività all’anti-P-endorfina è stata messa in evidenza in corpi cellulari presenti nella regione del nucleo infundibulare ed in fibre principalmente frammiste alle cellule suddette; essa risulta anche presente, seppur scarsamente, nella regione ipotalamica anteriore e nella zona esterna dell’eminenza mediana anteriore e posteriore. Received 27.1 1.92, accepted 6.6.93 74 Boll. Soc . Natur, Napoli ~ Voi 101 ( 1992-1993 ) L’immunoreattività encefalino-simile è presente in neuroni appartenenti alla componente parvocellulare del nucleo paraventricolare ed in cellule del nucleo infundibulare; ed inoltre, in fibre sparse in tutto l'ipotalamo e nella zona esterna dell’eminenza mediana anteriore e posteriore. La presente localizzazione rapportata a quella di altri sistemi peptidergici ipotalamici, già caratterizzati in lavori precedenti, evidenzia correlazioni spaziali il cui significato funzionale è da stabilire, ma che suggeriscono complessi rapporti neuromodulatori soprattutto nella regione infundibulare. La presenza di immuno- reattività encefalino- e g-endorfino-simile nella zona esterna dell’eminenza media¬ na depone a favore dell’ipotesi che questi peptidi siano rilasciati nella circolazione portale ipofisaria e quindi, coinvolti nella funzione neuroendocrina del sistema ipotalamoipofisario. Introduction Both methionine-enkephalin (met-ENK) and leucine-enkephaline (leu-ENK) as well as g-endorphin (g-END), are all members of a naturai opioid peptide familv (Hughes et al., 1980) able to link endogenous opiate receptors in thè brain (Terenius & Wahlstrom, 1974; Hughes, 1975) and in thè pituitary gland of various vertebrates (Cox et al., 1975). At first, g-END was isolated and characterized from carnei and porcine pituitaries as a 3 lamino-acid peptide, identical to thè carboxyl terminal sequence of g-lipotropin (nLPH) which is considered its biosynthetic precursor (Brandburv et al., 1976; Li & Chung, 1976; Chretien et ah, 1976; Cox et al., 1976; Akil et al., 1984). Both met-ENK and leu-ENK were isolated and characterized from thè pig brain as pentapeptides (Hughes et al., 1975) and they stem from a large precursor molecole, called proenkephalin (Akil et al., 1984). In mammals thè enkephalin-containing neurons are distributed widely in thè centrai nervous System, both as locai circuit neurons and as projection neurons, whereas g-END-containing neurons are mainly concentrated in thè region of thè arcuate nucleus of thè mediobasal hypothalamus with fibers projecting rostrallv and caudallv to manv limbic, thalamic and lower brainstem targets; although, another celi cluster is present in thè nucleus tractus solitarius (Elde et al., 1976; Hokfelt et ai, 1977 ; Simantov et ai, 1977; Sar et al., 1978, Bloom et ai, 1978; Uhi et ai, 1979; Bugnon et ai, 1979; Bloch et al, 1979; Sofroniew, 1979; Pickel et al. , 1980; Finley et al 1981; Schwartzberg & Nakane, 1981; Khachaturian et al, 1985 a,b). Esposito V., De Girolamo P., Sammarco M., Garginlo G The very few observations on thè distribution of opioid peptide in thè avian brain, include mainly thè enkephalins (Bàlhser & Dubois, 1980; De Lanerolle et al., 1981; Ryan et al., 1981; Mikami et al., 1983; Ball et al., 1988). Further to our previous studies on characterization of hvpothalamic peptidergic systems in thè chick brain (Gargiulo et al. , 1 990; Esposito et al. , 1992 a,b), we have identified in thè present investigation, by immunocyto- chemical methods, enkephalin and g-endorphin-like centers in thè hv- pothalamus of thè chick Gallus domesticus. The probable interaction with other hypothalamic neuropeptides and their involvement in regulation of thè release of pituitary hormones have been discussed. Materials and methods Male chicks of Gallus domesticus were obtained from a locai breeder at thè age of two weeks. Chicks were killed by decapitation and their brains were rapidly removed and immersed in Bouin's fìxative solution. The fixed brains were then routinelv dehvdrated through a series of graded alcohols, placed in xylene, and embedded in paraffin. Sagittal and transverse serial sections of thè brains 5pm thick, were cut and mounted on glycerinealbu- min coated glass slides. Finally, sections were deparaffinized in xylene, rehydrated in a graded ethanol series and washed in 0.0 1 M phosphatebuffe- red saline (PBS), pH 7.4. The immunocytochemical staining was performed using thè peroxida- seantiperoxidase (PAP) technique (Sternberger, 1979). Briefly, after inhibition of endogenous peroxidase activitv with 3% hydrogen peroxide, thè sections were treated with normal goat serum (IgG, 1:5, 30 min.), to avoid possible background reaction; then incubated overnight at 4°C with antisera to met-ENK diluted 1:500/1500, leu-ENK diluted 1:500/1500 and g-END diluted 1:1000/2000. Subsequentlv, thè sections were treated with goat antirabbit immunoglobulin (1:50, 30min.) and PAP-complex (1:100, 30min.). The reaction was visualized with a solution of 3,3’-diaminobenzidine (DAB; 10 mg in 15 mi of 0.5 M Tris-buf¬ fer, pH 7.6 containing 1.5 mi hydrogen peroxide at 0.03%). Between each step, thè sections were thoroughlv rinsed in PBS. Antisera to g-END (Ì456/002), met-ENK (Ì672/002) and leu-ENK (i67 1/ 002) was purchased from UCB as well as g-END (VB056), met-ENK (VB051), leu-ENK (VB050), normal goat serum (Ì200/002), goat anti-rabbit serum (Ì200/003) and PAP-complex (Ì200/001). DAB was purchased from DAKO. 76 Boll Soc. Natur. Napoli - Voi 101 ( 1992-1993 ) Figure 1 - Schematic drawing of thè hvpothalamus of domestic chick in a parasagittal piane, showing thè distribution of thè immunoreactive perikarya and fibers to anti(3endorphin (▲, ▲) and to anti-enkephalins (•, •). AC: anterior commissure; C: cerebellum; IN: nucleus infundiboli; ME: median eminence; N: neostriatum; NC: neostriatum caudale; NL: neural lobe; Nili: nervus oculomo- torius; OC: chiasma opticum; PC: posterior commissure; PD: pars distalis; POA: preoptic area; PVN: nucleus paraventricularis; TSM: tractus septomesencepha- licus; V: third ventricle. Esposito V\, De Gìrotmmo P., Sammarco Al, Gargiulo G. The specificity of staining were verifìed with control experiments as follow: a) replacement of thè metENK antiserum with thè same antisera adsorbed by both enkephalins, b) replacement of thè leu-ENK antiserum with thè same antisera adsorbed by both enkephalins; c) replacement of thè g-END antiserum with thè same antisera adsorbed by g-END, g-LPH and both enkephalins, d) replacement of thè met-ENK, leu-ENK, and g-END- antisera with normal rabbit serum or phosphate-buffered saline. Some sections were Luxol fast bleu-cresyl violet stained to improve thè identifìcation of nervous structures. All thè sections were dehydrated, coverslipped and finally observed and photographed using a Leitz Aristoplan. Results Immunocytochemical reactions with thè g-END, met-ENK and leu- ENK-antisera were observed in different parts of thè hypothalamus of thè domestic chick, Gallus domesticus (Fig. 1). Figure 2 - Photograph showing g-endorphin-immunoreactive cells and fibers in thè n. infundibuli. Parasagittal section.(X350). IN: n. infundibuli. 78 Boll Soc. Natur. Napoli - Voi 101 (1992-1993) Immunocytochemical specificity Controls were carried out on adja- cent serial sections in each area where positive immunoreactivity to p-END, met-ENK and leu-ENK were identified. The absorption tests by both synthetic methionine-enkephalin and leucine-enkephalin showed that each studied enkephalin antisera revealed both homologous antigens and heterologous antigens; indeed, it was observed no immunoreactivity or attenuated staining when preabsorption of met-ENK antiserum was car¬ ried out with synthetic met-ENK or leu-ENK, on thè other hand thè preabsorption of leu-ENK antiserum with synthetic leu-ENK or met-ENK inhibited or attenuated respectivelv thè immunostaining. v ili ME Figure 3 - Photograph showing P-endorphin-immunoreactive fibers in thè zona externa of median eminence. Transverse section. (X300). ME: median eminence, V: third ventricle The P-END immunostaining was inhibited by absorption of thè p-END antiserum with both synthetic P-END and P-LPH; thus, thè employed antiserum can recognize both P-END and P-LPH. The P-END immunostai¬ ning was maintained when it was used thè p-END antiserum adsorbed by both synthetic met-ENK and leu-ENK. 79 Esposito V />• V f * *«.» 4 Figure 4 - Photograph showing P-endorphin-immunoreactive cells (arrows) in thè n. infundibuli. Transverse section. (X400). IN: n. infundibuli: third ventricle A large population of (3-ENDlike immunopositive celi bodies occurred in thè nucleus infundibuli, a neuron group located ventromedial to thè third ventricle (Figures 2 and 4). P-END-like immunopositive fibers were detected in thè mediobasal hypothalamus and in thè nucleus infundibuli intermingled with p-END-im- munopositive perikarya. Only few thin P END immunoreactive-fibers were found scattered in thè anterior hypothalamic area. Thin P-END-like immu¬ nopositive fibers were also distributed in thè zona externa of thè rnedian eminence (Fig. 3). 80 Boll Soc . Natur. Napoli - Voi. 101 (1992-1993) Enkephalin-immunoreactive neurons were found both in thè parvo- cellular division of thè nucleus paraventricularis and in thè nucleus infundibuli; thè later were very few and small in size (Figures 5 and 6). ENK-immunopositive fibers were detected throughout thè whole hy- pothalamus; anyhow they were mainly concentrated in thè anterior hy- Figure 5 - Photograph showing enkephalin-immunoreactive cells (arrow) and fibers in thè median eminence. Transverse section. (X250). IN: n. infundibuli, ME: median eminence pothalamus, ventrally to thè anterior commissure (Fig. 8), and in thè posterior hypothalamic region around thè noimmunoreactive perikarya of thè nucleus mammillaris medialis (Fig. 7). Discussion The findings of present immunocytochemical study indicate that both enkephalinergic and g-endorphinergic or lipotropinergic System are pre- Esposito V., De Girolamo P., Sammarco M.f Gargiulo G. sent in thè chick hypothalamus and that they have a different localization as well as mammals (Bloom et al., 1978; Watson et al, 1978). Specificity tests for immunocytochemical staining revealed a possible cross-reaction between thè anti-MET-ENK antisera and LEU-ENK, and thè anti-LEU-ENK antiserum and MET-ENK; thè present study, therefore, reports thè localization of an enkephalin-related peptide. Figure 6 - Photograph showing enkephalinimmunoreactive cells in thè n. para- ventricularis. Transverse section. (X300). PVN: n. paraventricularis, V: third ventricle On thè other hand, thè anti-human g-endorphin antiserum employed in this study reveal cross-reactivity with g-lipotropin, suggesting that they also contain antigenic determinants common to g-LPH. Similar behavior has been reported previously for antihuman and anti-porcine g-END (Bloch et ah, 1979; Doerr-Schott et al, 1981; Kiss et al, 1985). Other immunocytochemical studies on lower vertebrates (Doerr- Schott et al., 1981; Nozaki & Gorbman, 1984; Vallarino, 1985, 1986) indicate that cross reactions may occur between mammal anti-g-END and thè corresponding antigen from nonmammalian vertebrates, suggesting an immunogenic relationship between g-END molecules among vertebrates. 82 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) The g-endorphin-like immunoreactivity evidenced in thè present study is mainly concentrated in thè nucleus infundibuli that appears to be thè homologous of thè arcuate nucleus of mammals (Mikami, 1986), thè Principal site of g-END-containing neurons in mammalian species (Akil et al, 1984). Figure 7 - Photograph showing enkephalin-immunoreactive fibers in thè n. mammillaris. To remarke thè network fibers around thè noimmunopositive pe¬ ri karva of MM. Transverse section. (X300). MM: n. mammillaris, PVO: paraven- tricular organ Many kinds of neuropeptides have been immunocytochemically cha- racterized in thè avian nucleus infundibuli (Mikami, 1986; Esposito, 1990; Gargiulo et al. , 1 990; de Girolamo & Esposito, 1 99 1 ; Esposito et al. , 1 992 a, b); thè phvsiological significance of this spadai relationship between g-END and other peptides is unknown, but it is possible to postulate complex neuromodulator interaction. Furthermore, thè g-END-immuno- reactive fibers terminals in thè median eminence coming very likelv from nucleus infundibuli suggest a possible hypophvsiotropic role of g-END. Sakurai et al. (1986) demonstrated that g-END is involved in thè control of LH release in thè hen as an inhibitory agent. Esposito V., De Girolamo P., Sammarco M., Gargiulo G. 83 According to Blàhser and Dubois (1980) we have observed that immunocytochemical reaction for enkephalins reveals more extensive fìber network than immunoreactive perikarya confirming thè possibilitv of a discontinuous peptide synthesis within thè perikarya, or an unmasking of thè peptide molecule only within thè axons and dendrites. • V,' 4 ■ V ■ è i . .* . I:- , * / * \ >r à H ** k 4. ,f f ■ n 4 • V* % a * * ’4 • f * r . jf ^ // 4 > ...À" -fin J é ■ f*f 4 > v ' /;> V , , v ^ i - ■ '«A , * i : ■ ,** '* , À - . * -, « { | : •4 | a. ■ • $ 4 * 1 • 'V F / s jr ; - . 4 k I J y. r ,*» A ’ - • , » f ** «> . ,v t ti- I ' V I -■ , #? ; ; ’! 'G ' ■ v- ; ‘ v - •t / , ** ’ M - .. 8 Figure 8 - Photograph showing enkephalinimmunoreactive hbers and some cells (arrows) in thè anterior hvpothalamus. Parasagittal section. (X350) However thè hypothalamic distribution of immunoreactivitv to enke¬ phalins described in this study is similar to those reported in previous works (for review see Viglietti-Panzica & Panzica, 1991). 84 Boll Soc. Natur. Napoli - Voi 101 ( 1992-1993 ) The enkephalinergic centers observed in thè hypothalamic region, in both paraventricular and infundibular perikarya, may be related to thè presence in this area of a wide neurosecretory System producing hypophy- siotropic hormones (Scharrer & Scharrer, 1963; Blàhser, 1983). Generally, thè ENK appear to inhibit thè neuronal firing rate by inhibiting transmit- ter-induced depolarization of thè postsynaptic celi membrane (Zieglgan- sberger et al , 1976, North & Williams, 1 985), therefore they may modulate different excitatory signals in this area or in other hypothalamic sites. The present reports mainly emphasizes thè rich enkephalinergic in- nervation of thè infundibular area which is consistent with thè various hypophysiotropic effects of enkephalins (Tramu et al, 1981). The presence of perivascular enkephalins fiber terminals in thè me- dian eminence implies that enkephalin may be released from thè median eminence into thè portai circulation and involved in neuroendocrine function of thè hypothalamo-hypophvsial System. Finally, our observation show a spatial relationship between ENK and g-END in thè mediobasal hypothalamic area, which contains thè main accumulation of g-END perykaria, intermingled with ENK-fibers, but thè possible interaction between them will be able to demonstrate only at thè ultrastructural level. 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Brani Res., 115: 160-164. ' ' Boll. Soc. Natur. Napoli - Voi 101 ( 1992-1993 ): 89-103 89 Action of thè cadmium on thè Carassius auratus living in lentie waters containing catabolic ammonia Battaglini P.\ Soppelsa O.1, Improta C.2, Ferrara L.2 1 Dipartimento di Zoologia, Università degli Studi «Federico II», via Mezzocannone 8, 80126 Napoli, Italy 2 Dipartimento di Chimica, Università degli Studi «Federico II», via Mezzocannone 4, 80126 Napoli, Italy Key words: cadmium, ammonia, water hardness, Carassius auratus. Abstract. In a previous paper (Battaglini et al., 1991) concerning thè Cadmium ion absorption in ditte re nt Carassius auratus organs in “soft” and “hard” waters, thè Authors have shown that thè absorption of thè Cadmium is much more signifteant in softwater than in hard water. In this paper thè Authors have considered a further element characterizing thè habitat of thè Carassius auratus, i.e. thè limited environment of stagnant water in which, besides thè pollution substances like cadmium salts, thè same catabolic materials of thè Carassius auratus exist. The Carassius auratus were kept for 8 days to become acclimatized. We have then carried out a research on thè results obtained by our tested animals to thè Cadmium collecting thè survival and absorption data of this toxic in different organs by adding cadmium chloride CdCh.Z'/.FUO up to reach a 10 ppm concentration of ion Cd++ in experiment tanks where. We have observed that thè Storage in water of catabolic material such as ammonia is an element increasing cadmium toxicity related to thè Carassius auratus. Such toxicity is revealed both by higher values of absorption of this ion in different organs and in thè survival values of thè specimens which are definitely lower. Riassunto. Azione del cadmio su Carassius auratus viventi in acque lentiche contenenti NH, catabolica In un precedente studio relativo all’assorbimento dello ione cadmio nei vari organi di Carassius auratus in acque “dure” e “dolci”, abbiamo dimostrato che l’assorbimento del cadmio è molto più pronunciato in acqua dolce che in quella dura. Inoltre, avendo constatato in acqua dura contrariamente a quanto avviene in acqua dolce una immediata e quasi completa precipitazione dello ione cadmio sottoforma di CdC03, abbiamo ipotizzato nei due casi due differenti meccanismi di assimilazione del cadmio: a) per osmosi con bioaccumulo nel tempo, in acqua dolce; b) per ingestione di CdC03 solido precipitato, nel caso di acqua dura. Nel presente lavoro abbiamo voluto prendere in considerazione un ulteriore elemento che caratterizza l’habitat del Carassius auratus, ovvero l’ambiente limitato di acqua ferma in cui sono presenti, oltre ad eventuali sostanze inquinanti come i sali di cadmio, gli stessi prodotti di rifiuto dei carassi. Abbiamo quindi Received 27.1 1.92, accepted 16.6.93 Boll Soc . Natur. Napoli - Voi . 101 (19 effettuato uno studio sulla risposta fornita dai nostri animali da esperimento al cadmio, raccogliendo dati di sopravvivenza e di assorbimento di tale tossico nei vari organi. In particolare abbiamo aggiunto cadmio cloruro, CdCI2.2,/2H20, fino a raggiungere una concentrazione di 10 ppm di ione Cd2+ in vasche da esperimento ove erano stati tenuti i carassi per acclimatarli nei precedenti 8 giorni. Nell'acqua utilizzata, (“acqua dura“: pH=7,8; durezza 369 mg/L di CaC03; “acqua dolce” pH=7,6; durezza 152 mg/L di CaC03) erano presenti anche i prodotti catabolici dei carassi tra cui l’ammoniaca che, al momento della aggiunta del cadmio, presenta¬ va una concentrazione di 7. 1 0 mg/L. Le misure di assorbimento atomico sono state eseguite sugli organi mineralizzati. I pesci sono stati sacrificati ai seguenti tempi: Ih 30’, 24h, 72h, 7gg. La presenza nell’acqua di NH3, che è un forte complessante dello ione cadmio, ha notevolmente aumentato la solubilità dei suoi sali permet¬ tendo la sua permanenza in soluzione al 100% per oltre 4 giorni. Successivamente lo ione metallico è cominciato a precipitare come carbonato, rimanendo tuttavia per circa il 20% del suo valore iniziale ancora al 7U giorno dall’inizio dell'esperi¬ mento. La sopravvivenza nella “acqua dura” è stata del 100% dopo Ih 30’, del 50% dopo 24h, del 44% dopo 72h e del 12% dopo 7gg. Nella “acqua dolce” la sopravvivenza, molto simile alla precedente, è stata del 100% dopo Ih 30', del 50% dopo 24h, del 40% dopo 72h e del 10% dopo 7gg. I dati di assorbimento confermano che gli organi che presentano maggiore accumulo di cadmio sono, come nel nostro precedente esperimento, fegato, rene ed intestino, mentre si ottengono valori modesti o addirittura nulli per pelle, cervello, cuore e muscolo. Inoltre i valori di assorbimento di Cd2+ sono sempre più elevati rispetto a quelli riscontrati per esemplari posti in acqua senza ammoniaca. Ciò è stato attribuito al fatto che essendo il cadmio, nel caso attuale, presente in massima parte in soluzione, anche se come complesso cadmioammoniaca, esso possa essere più facilmente assimilato per assorbimento dai Ciprinidi (nel nostro caso Carassius auratus ) e accumulato nei vari organi. In conclusione si può dire che l’accumulo nell’acqua di un prodotto catabolico come l’ammoniaca costituisce un elemento di aggravamento della tossicità del cadmio nei confronti dei carassi, che si manifesta sia in più elevati valori di assorbimento di questo ione nei vari organi che nei valori di sopravvivenza degli esemplari che sono drasticamente più bassi. Introduction The pollution of thè waters caused by heavy metals and thè relevant consequences on flora and fauna of these ecosystems has become a very topic question following thè great development of human activities at industriai level. Among thè different heavy metals cadmium and mercury proved to be thè most toxic, (Ravera, 1984). This metal which is present in nature expecially as an impurity of thè zinc minerals (blenda, ZnS) or as sulphur (grenockite CdS), is spread out in thè biosphere through different ways such as: volcanic activity, exudates from vegetation, foresi fires, windblown dust and leaching of rocks and, in thè latest ten years, also 91 Battaglini P., Soppelsa O., Improta C., Ferrara L. through thè use of phosphate fertilizers, incinerator waste coal and oil combustion and thè same industriai production of cadmium minerals (Ravera, 1984; Polprasert, 1982). The cadmium, spread out in thè soil, in discharge waters and in atmosphere, is at last carried by wind and rain into thè streams of water (Absullah & Royle, 1972; Ajrnal et al, 1985; Ajmal et ai , 1987). The studies on cadmium toxicity on freshwater fish have shown a signifìcant dependence of this toxicity from thè Chemical characteristics of thè environment in which thè toxic is spread out, having sometimes increasing results, some other times decreasing results, ofthe toxic action ofthis heavy metal (Sprague, 1987; Calamari et al. , 1980; Enk & Mathis, 1977). In former studies (Battaglini et al., 1991; 1992a; 1992b; Gargiulo et al., 1991) concerning ion cadmium uptake in different organs of Carassius auratus in waters of different hardness, it was shown that thè metal uptake is much more signifìcant in soft than in hard water. In addition, owing to thè observation of a heavy and sometimes almost complete precipitation of ion cadmium as CdC03 in waters of higher hardness, two possible ways of absorption with consequent toxic action of cadmium were assumed: a) due to osmosis with bioaccumulation during thè time (above all in soft water); b) due to intake of CdC03 solid precipitate (above all in hard water) (Battaglini et al., 1991). The high and sudden mortality of fish in rivers and hatcheries is often caused by lethal concentrations of polluting toxicant substances (Tarazona et al., 1987). Anyway such pollution is not always due to thè intake of allochtoneous substances, as thè same catabolic materials in small habitat and without change water can cause an environmental change, being themselves toxic or simplv increasing thè toxicant action of other substan¬ ces already present in thè habitat (Ravera, 1984). To better understand thè environmental changes that are displayed on thè area, some behavioural and echotoxicology tests were carried out on goldfìsh (Carassius auratus ) aimed at focusing thè interrelation, from an ecotoxicology view, of some behavioural parameters. In this paper thè authors have considered an element that characteri- zes thè naturai habitat of Carassius auratus, i.e. thè feature of a limited habitat with stagnant water in which, besides thè possible polluting sub¬ stances, there is a Storage of catabolic materials of Carassius auratus (Mommsen & Walsh, 1992). Among these, ammonia is thè major nitroge- nous and product comprising usually more than 70% of total waste nitrogen in freshwater teleosts (Warde van, 1983). The importance of 92 Boll. Soc. Natur. Napoli - Voi. 101 ( 1992-1993 ) ammonia in this context is due not only to its reai toxicity but also because it is one of thè main chemical complexing substances of ion Cd2+, causing a modification of thè speciation of this metal in solution. Thus thè authors have carried out a study on Carassius auratus response to thè polluting action of cadmium with ammonia as catabolic product, testing such action in waters of different .hardness in order to compare these results with those obtained in former experiments carried out without ammonia. Materials and methods 20 tanks of 20 1 each were prepared, of which 10 tanks were filled up with tap water of Naples and 10 were filled up with thè same water, previously decalcified with ion exchange resins Soft C (line “C”) CARMAR, Naples. Both kinds of waters were utilised only after a period of aeration in a 600 1 glass aquarium to eliminate thè chlorine. The test fish, supplied by CARMAR Co., Naples, weighed 5 -e 7 g. All animals have been held for 10 days to have them acclimatized in two different kinds of waters in two 600 1 separate glass aquaria, equipped with air pump and filter Eheim, in thè Ecology and Ecotoxicology Laboratory of thè Department of Zoology University of Naples Federico II. Then 200 Carassius auratus, randomly chosen, were transferred in experiment tanks (10 fishes in each tank). The tanks had a photoperiod of 12 hrs and were supplied with an air pump, but without filter, to prevent catabolic materials from being eliminated To simulate thè lentie environ- ment, fishes were held for 8 days in thè same water to let catabolic materials store up, and particularly ammonia. During this period, fish were fed as usuai. The experiment began only after these eight days. Cadmium as CdCl2.2ViH20, equal to 10 ppm, was added to 8 tanks with water of higher hardness and to other eight tanks with water of lower hardness. The Carassius auratus which were in other 4 tanks, 2 tanks with soft water and two tanks with hard water, were utilized as control fishes during thè experiment. During thè whole experiment thè temperature was constantly at 16 + 1 °C. The analysis of thè different substances which are in thè two different kinds of waters utilized for thè experiment, was performed at zero time. Measures were taken utilizing thè traditional volumetrie titration, thè standard solution hardness of sodiumtilendiaminotetracetic acid salt for thè hardness, alkalinity with standard solution of HCl using bromocresol as Battaglini P., Soppelsa O., Improta C., Ferrara L. acidbasic indicator for thè alkalinity, ionchloride with AgN03 solution utilizing Mohr (Kolthoff et al., 1973) method for ionchloride. A pHmeter ORMA, model NK 300 was used to determine thè pH and a dissolved oxygenmeter HI 8543 (Hanna Instruments, USA) to determine thè dissol¬ ved oxygen in water. The NH3 produced and present in water was measured with a spectro- photometer utilizing Nessler reagent to obtain thè typical yellow colour. Cadmium concentration in solution in thè single tanks was measured every 24 hrs till thè end of thè experiment by using thè atomic absorption spectrophotometer VARlAN AA275. To get thè correct interpretation of cadmium concentration values present in solution at different phases, a kinetic precipitation of ion Cd2+ as CdC03 was carried out in parallel in thè same waters utilized during thè tests, but without Carassius auratus and its relevant catabolic materials. The survival values were taken up to 7 days from thè beginning of thè experiment, carrying out also thè pathological anatomy dissection of thè dead specimens. To evidence thè metal effects on Carassius auratus behaviour thè ventilation frequency of experimental and control goldfish was determi- ned by counting thè number of opercular movements per minute (Lang et al., 1987) of 5 fishes for each tank. The computation of 5 fishes for each tank was optimized by using thè average value, which was then compared to thè values obtained at different phases. Such computations were made every 15’ for thè first 90 minutes, every 30' for thè following 150 minutes and every 24 hours during 3 more days. A further parameter to understand thè behavioural reactivity in thè presence of toxic was taken counting thè movements of thè caudal fin per minute (Abel & Papoutsoglou, 1987): more beats = more movement. Of course thè same tests were carried out for thè Controls. For each kind of water two specimens were taken randomly in various periods of time (1.5 h, 24 h, 72 h and 168 h). The organs taken out, after being weighed on an analytic balance, were treated with a mixture (weighing as much as five times thè organs) of HN03/HC104 4:1 in a 10 mi pyrex tube plugged at 7080°C for 24 h in order to obtain a complete mineralization of thè tissues. The solution obtained was brought up to thè known volume by adding HN03 0.1 M and then analyzed by an atomic absorption spectrophotometer VARIAN AA275 in order to determi¬ ne thè cadrnium concentration as parts per million (ppm) of fresh organ. 94 Boll Soc . Ator. Napoli - Voi 101 (1992-1993) Results In both experiments thè concentration of NH3 catabolic reach a value (7 -e 10 mg/L) that have a remarkable influence on thè form in which cadmium (II) is present in thè System. Fig. 1 reports two precipitation kinetics of cadmium as carbonate (thè average cadmium concentration present in solution versus time) in water ppm Figure 1 - Storage of ion cadmium in solution with or without catabolic products. of higher hardness with thè Carassius auratus and, in comparison, in thè same kind of water but without thè Carassius auratus. It can be noted that thè precipitation occurs in significantly different amounts. In point of fact, in hard water and with Carassius auratus, we can notine that total cadmium remains in solution longer than four days of thè experiment. The precipitation occurs only at thè final stage of thè experiment, leaving in solution, however, a cadmium concentration of almost 2 ppm. In Kinetic of comparison, always in hard water but without goldfishes, thè cadmium carbonate precipitation is immediate with a residuai quantity in solution reducing itself to 3.5% of thè starting value after 24 hrs. In less hard water, Battagìmi SoppeJsa Gq Imgrota C., Ferrara L. 95 characterized by greatly lower alkalinity and thus with a lower carbonate cadmium precipitation, no carbonate cadmium precipitation at all occurs, with or without Carassius auratus. The survival, in water of higher hardness, was 100% after 1 hr 30', 50% after 24 hrs, 40% after 72 hrs and 10% after 7 days, Sudi values are defìnitely lower, as compared to thè results obtained in our previous experiments carried out in waters without ammonia, when survival was almost 100% after thè same experiment period of time. (Battaglini et al. , data unpublished). The pathologic anatomy analysis of thè dead specimens, has shown haemorrhagic gills, congested liver, haemorrhagic kidneys, and a hyper mucus production all over thè body and particularly at gills. As to thè beh avi our, fig. 2a reports thè average values of beats per min. of thè operculum and caudal fin in hard water, and fig. 3a reports thè movements/msn Figure 2a - Effect of cadmium + NH3 on thè Carassius auratus behaviour in hard water. relative values in soli water More frequent movements of opercular gill are signs of a greater request of Oxygen (Black 1 95 1 ; Hughes, 1 960) . Caudal fin movements are signs of regular activity, decrease or stop are signs of a significant suffering (Bainbridge, 1961). In thè Controls (Figures. 2b and 3b) thè Àuthors have noted that there is an almost continuous trend having 96 Boll Soc . Natur . Afapo/i - Vo/. 101 ( 1992-1993 ) average values very dose to normality (1040 beats per min. of thè oper- culum). As regards thè fishes treated (figures 2a and 3a), thè values of thè operculum beats were noted to be always high but, after a lowering to 60’, they turn to be stronger and stronger after 4 hours from thè beginning of thè experiment. movements/min Figure 2b - Behaviour of control specimens of Carassius auratus in hard water. The data of cadmium stored up in different organs are characterized by a slight measure error, estimated more or less by 2 3%, but subjected to a variability of cadmium values depending on thè different specimens, and such variability value is much more important. Thus thè values reported, which are thè average among couples of measures on different samples, are effected by a total uncertainty reaching sometimes a value of even 10%. Fig. 4a reports cadmium Storage values in some organs tested in our experiment, as compared to thè same values obtained in a previous experiment (Fig. 4b) (Battaglini et al, 1991), in which no catabolic materials were present when cadmium chloride was added. The data of atomic absorption confimi that organs having a higher cadmium Storage are, as in our previous test: liver, kidney, and gut; while low values or even no value were noted for skin, brain, heart and muscle. Battaglini P Soppelsa O., Improta C., Ferrara L. Discussion In this research, thè striking datum for his dramatic and unexpected low vaine, is thè one relative to thè survival. Such a dramatic discrepancy could not be expected indeed. In fact, among thè different softwater fishes (Flis, 1968) Cyprinids are known to be thè least sensitive to NH3 and Figure 3a - Effect of cadmium + NH3 on thè Carassius auratus behaviour in soft water. cadmium; on thè other hand, thè same results obtained in previous experiments suggested definitely different results (Battaglini et al., 1991). This discrepancy is not overcome even if thè Authors consider that ammonia itself develops its own toxic action which is to be added to thè action of cadmium. In fact, thè values of total ammonia measured by thè Authors in experiment waters, at thè pH values on which we are working, imply thè presence of molecular ammonia in hard and soft water of 0.33 and 0.22 mg/L, respectively. These values are definitely lower than thè standard value considered toxic for thè carp, which is 2.0 mg/L (Malacea, 1968), and for other Cyprinids, like Pimephales promelas, which is between 0.75 and 3.4 mg/L of NH3 (Thurston, Russo & Phillips, 1983). As a matter of fact, thè discrepancy is only apparent and is due to thè fact of considering thè toxic action of cadmium and ammonia as two 98 Boll Soc . Natur. Napoli- Voi 101 (1992-1993) additional phenomena, where, on thè contrary, thè simultaneous presence of such two substances deeply modifies thè chemical nature of both, and consequently, their own toxicity. movements/min Figure 3b - Behaviour of control specimens of Carassius auratus in soft water. To better understand thè environment moclified by these substances, we must consider thè main chemical processes obtained in solution. Ammonia, as already mentioned, is a strong complexing agent of ion cadmium making with this one several compounds up to thè tetraminocad- mium: 4 NH3(aq) + Cd2+(aq) = Cd(NH3)42+(aq) The progressive involvement of NH3 in thè complex with cadmium, gradually moves thè acidbase equilibrium of ammonia towards further molecular ammonia, according to such equilibrium: NH4+(aq) + H20 = NH3(aq) + H30 + (aq) and thus, even if at thè beginning there is a low amount of molecular NH3 at thè pH level on which we are working, thè presence of ion Cd2+ is capable of displacing this equilibrium towards thè molecular NH3 just 99 Battaglini P., Soppelsa O., Improta C., Ferrara L . because of thè capture caused by thè complexing of thè molecules NH3 produced. On thè other hand, thè production of thè complexes Cd (NH3)2+n aims at drastically reducing thè concentration of ion Cd2+ in solution, thus highly increasing thè solubility of CdC03 which is produced in calcareous waters with Cd2+: Cd"+(aq) + HCO 3_(aq) + H2O = CdC03(s) + H30+(aq) Thus, one of thè consequences produced, is thè lower and slower precipitation of CdC03 obtained in experiment tanks with calcareous water and Carassius auratus, as compared to thè one obtained in water of thè same kind but without Carassius auratus. PPm + kidney HW liver HW ^ kidney SW ^ liver SW Figure 4a - Cadmium Storage in liver and kidney of Carassius auratus specimens held in hard (HW) and soft (SW) water with ammonia. Furthermore, we assign to thè complexes Cd(NH3)n2+ a toxicity higher than thè one attributed to thè single Cd2+ and NH3; in fact, we have ascertained that even in soft water, where cadmium remains in solution for thè whole period of thè experiment, thè survival is, under thè same conditions, lower when catabolic ammonia is present together with ion cadmium. In view of thè above, also thè other data can be better explained. 100 Boll. Soc . Natur. Napoli - Voi. 101 (1992-1993) In this sense, we have shown that thè first symptom in goldfish exposed to cadmium + ammonia is respiratory alteration, measured by ventilation frequency, as reportedby Maki (1979). Smart (1978) reported hyperexcita- bility and hyperventilation such as acute toxic mechanism in rainbow trout. Both specimens treated in hard water and those treated in soft water suffer stress which shows an increase of thè opercular beats, and a dramatic decrease of thè caudal movement, showing thè stillness condi- tion of goldfish at thè bottom of thè tanks. No particular difference can be seen between thè two cases, which confirms that both in hard and soft water thè Carassius auratus during most of thè experiment time, are PPm Figure 4b - Cadmium Storage in liver and kidney of Carassius auratus specimens held in hard (HW) and soft (SW) water without ammonia. exposed to thè same amount of cadmium in solution. Similarly, thè dead specimens, no matter if placed in hard or in soft water, did shown a mucus hyperproduction which sometimes covered thè whole specimen like a shirt. This is in agreement with thè relevant literature, since it has been demonstrated that mucus production can be influenced by thè presence of harmful environmental factors, such as ammonia pollution (Jakowska, 1963; Dave & Garside, 1976; Zuchelkowski el al., 1981). As concerns thè Storage of cadmium data in different organs, thè comparison of uptake values obtained in two different water kinds, shows 101 Battaglini P., Soppelsa O., Improta C., Ferrara L. : that, while in harder water thè cadmium Storage occurs alreadv in thè first 24 hrs, in softer water thè Storage occurs only after a longer time. On thè other hand, after 7 days, Storage in softer water becomes more important than thè one in hard water. For thè gut only, higher cadmium values are ascertained in hard waters, even after 7 days, because of thè presence in thè intestinal lumen of CdC03 ingested from thè bottom of thè tank and accumulated there after thè fourth experiment day. Finally, it has to be pointed out that cadmium storages in organs, in thè presence of catabolic ammonia, are higher than those obtained without it, both in hard and soft water. In water of higher hardness, this can be easilv explained attributing thè higher cadmium Storage (in thè presence of ammoniaca! products) to a longer stay of cadmium solution as a complex which, therefore can be easily absorbed by fishes from solution. Viceversa, thè greater Storage observed in soft water, brings thè Authors to thè assumption that cadmium has a higher penetrating capacity into fish tissues when it is coordinated with ammonia, rather than with water molecules. In conclusion, it can be stated that Storage of a catabolic product (such as ammonia) in water will definitely increase cadmium toxicitv as regards fish. Acknowledgements: This study was supported by a contribution of Italian MURST (40% & 60%). REFERENCES Abdullah, M.I. & L.G. Royle, 1972. Heavv metal content of some rivers and lakes in Wales. Nature, 238: 329-330. Abel, P.D. & S.E. Papoutsoglou, 1987. Lethal toxicitv of cadmium to Cyprinus carpio and Tilapia aurea. Bull. Envir. Confam. Toxic., 38: 382-386. Ajmal, M., M.A. Khan & A. A. Nomani, 1985. Distribution of heavv metals in water and sediment of Yarnuna River, India. Envir. Monit. Assesm., 5: 305-314. Ajmal, M., A. Raziuddin & A.U. Khan, 1987. Heavy metals in water, sediment, fish and plants of river Hindon, U.P., India. Hidrobiologia, 148: 151-157. Bainbridge, R., 1961. Problems of fish locomotion. Symp. Zool. Soc. London, 5: 13-22. Battaglini, P., G. Andreozzi, R. Antonucci, P. de Girolamo, L. Ferrara & G. Gargiulo, 1992a. The effects of cadmium on thè gills of thè goldfish Carassius Boll Soc . Rotar. Napoli - Voi 10 1 (092-1 if Ai* 102 au rat us L.: metal uptake and histochemìcal changes. Comp . Biochem . Physiol., 2: 239-247. Battaglimi, P., L. Ferrara & O. Soppelsa, 1991. Assorbimento di Cd2" in vari organi di Carassius auratus in acque "dure” e “dolci”. Atti Soc. It. Sci. Vet., 45: 149-153. Battagline P., L. Ferrara, P. de Girolamo, A. Andreozzi, R. Antonucci & G. Gargiulo, 1992b. The influence of some abiotic factors on thè toxicity of cadmium to Carassius auratus . Toxicol. Letters, Suppl. '92, 278. Black, E.C., 1951. Respiration in fìshes. Univ . Toronto Stud. Biol. Ser 50: 91-102 Calamari, D., R. Marchetti & G. Vailatx, 1980. Influence of water hardness on cadmium toxicity to Salmo gairdneri Rich. Wat. Res. . 14: 1421-1426. Daye, P.G. & E.T. Carsi de, 1976. Histopathological changes in superfìcial tissues of brook trout, Salvelinus fontinalis (Mitchill). Can. J. Zoo L, 54: 2140-2155. Enk, M.D. & B.J. Mathis, 1977. Distribution of cadmium and lead in a stream ecosystem. H idrobio lo già, 52: 153-158. Flis, !.. 1968. Anatomicohistopathological changes induced in carp (Cyprinus carpio L.) by ammonia water. Part I. Effects of toxic concentrations. Part IL Effects of subtoxic concentrations. Acta Hydrobiol. , 10: 205-224, 225-238. Gargiulo, G., G. Andreozi, R. Antonucci, N. Arcamone, P. de Girolamo, L. Ferrara & P. Battagline 1991. Variazione dei mucopolisaccaridi in risposta ad altera¬ zioni ambientali da Cd ' " in Carassius auratus. Dati preliminari. Atti 45 " Conv. Soc. it. di Anat. Sassari, 199 Hughes, G.M., 1960. A comparative studv of gill ventilation in marine teleostes. Jour. Exp. Biol, 37: 28-45. Jakqwska, S., 1963. Mucus secretion in fish -a note. Ann. N.Y. Acad. Sci., 106: 458-462. Kolthoff, I.M., E.B. San dell, E.J. Meehan, & S. Bruckenstein, 1973. Analisi Chimica Quantitativa. Padova: Piccin. Lang, T.., G. Peters, R. Hoffinann & E. Meyer, 1987. Experimental investigations on thè toxicity of ammonia: effects on ventilation frequency, growth, epi der¬ ni al mucous cells, and gill structure of rainbow trout Salmo gairdneri. Dis. aquat. Org ., 3: 159-165. Maki, A.W., 1979. Respiratory activity of fish as a predictor of chronic fish toxicity values for surfactants. In: Aquatic toxicology , L.L. Marking & R.A. Rimerie Eds., American Society for testing and materials, pp. 77-95. Malacea, L, 1968. Untersuchungen iiber die Gewohnung der Fische an hohe Konzentrationen toxischer Substanzen. Arch. f Hydrobiol , 65: 74-95. Mommsen, T.P. & P.J. Walsh, 1992. Biochemical and environmental perspectives on nitrogen metabolism in fìshes. Experientia , 48: 583-593. Polprasert, C., 1982. Heavy metal pollution in thè Chao Phraya river estuary, Thailand. Wat. Res., 16: 775-784. Ravera, O., 1984. Cadmium in freshwater ecosystem. Experientia, 40: 214. Smart, G., 1978 Investigations of thè toxic mechanisms of ammonia to fish gas exchange in rainbow trout ( Salmo gairdneri) exposed to acutely lethal concen¬ trations. J. Fish Biol, 12: 93-104. Sprague, J.B., 1987. Effects of cadmuim on freshwater fish. In: Cadmium in aquatic environment , J.O. Nriagu & J.B. Sprague, Eds., New York, I. Wiley & Sons. pp. 139-169. B attagliili P.t Soppelsa O., Improta C., Ferrara L . 103 Tarazona, J.V., MaJ. Munoz, J.A. Ortiz, MaO. Nunez & J.A. Camargo, 1987. Fish mortality due to acute ammonia exposure. Aquacul. Fish Manag., 18: 167-172. Thurston, R.V., R.C. Russo & G.R. Phillips, 1983. Acute toxicity of ammonia to fathead minnows (Pimephales promelas). Trans. Am. Fish Soc., 112: 705-71 1. Waarde van A., 1983: Aerobic and anaerobic ammonia production by fish. A review. Comp. Biochem. Physiol. , 74B: 675-684. Zuchelkowski, E.M., R.C. Lantz & D.E. Hilton, 1981. Effects of acid-stress on epidermal mucous cells of thè brown bullhead Ictalurus nebulosns (Le Seur): a morphometric study. Anat. Ree., 200: 33-39. Boll Soc. Natur. Napoli - Voi. 101 (1992-1993): 105-120 Catabolic NH3 influence on cadmium toxicity to thè gut of Carassius auratus L. Andreozzi G.1, Antonucci R.1, Affatato C.\ De Girolamo P.\ Gargiulo G.1, Ferrara L.2, Sammarco M.\ Battaglini P.3 1 Dipartimento di Strutture, Funzioni e Tecnologie Biologiche, Università degli Studi «Federico II», via Delpino 1, 80137, Napoli; 2 Dipartimento di Chimica, Università degli Studi «Federico II», via Mezzocannone 4, 80126 Napoli; 3 Dipartimento di Zoologia, Università degli Studi «Federico II», via Mezzocannone 8, 80126 Napoli, Italv Key words: Cadmium, toxicity, gut, immunocytochemistry, C arassius auratus . Abstract. We studied thè toxic action that thè ion Cd:~ exerts on thè gut of Carassius auratus when thè metal is introduced into water containing materials of thè fish catabolism including ammonia. The results have shown that in hard water (369 mg/L of CaC03), thè cadmium produces damage to thè epithelium of thè bulb which appears detached from thè connective and an increase of thè cellular turnover evidenced by a higher number of thè cells in mitosis. On thè contrary, in soft water (125 mg/L of CaC03) thè following was noted: a suffering aspect of thè epithelium of thè bulb, an expantion of thè mucous cells and an increase in thè mucus mass contained in thè intestinal lumen. Riassunto. Influenza dell’NH3 catabolica nell’intossicazione da cadmio sull’intestino di Carassius auratus. È stata studiata la reazione tossica che il cadmio esercita su Carassius auratus quando il metallo viene immesso in acqua contenente anche prodotti del catabolismo dei pesci e in particolare tra questi 1NH3. Poiché Fazione tossica del cadmio è correlata alla durezza dell’acqua, sono sta prese in considerazione acque con diversi valori di durezza e precisamente una contenente 369 mg/L di CaC03 “acqua dura” e un’altra contenete 152 mg/L di CaC03 “acqua dolce”. Sono state allestite due serie di vasche contenenti acqua a diversa durezza. In ciascuna della vasche sono stati immessi 10 carassi. Dopo 8 gg., quando l’acqua si era arricchita dei prodotti catabolici dei pesci, in ogni vasca è stato aggiunto CdCL.2'/2FL0 in quantità pari ad una concentrazione di cadmio nell’acqua di 10 ppm. L’accumulo di cadmio nell’intestino è stato determinato mediante l’assorbimen¬ to atomico previa mineralizzazione dell’organo. Sono state inoltre usate le colorazioni con ematossilinaeosina per l’esame morfologico della mucosa intestinale, e, per la localizzazione e tipizzazione dei mucopolisaccaridi, la reazione PAS, la colorazione con Alcian a pH 2,5 e a pH 1 da sola o associata a digestione con neuroaminidasi. La Received 27.1 1.92, accepted 7.5.93 106 Boll Soc. Natur. Napoli - Voi. 101 ( 1992-1993 ) presenza di sostanze Metencefalina like e Leuencefalina like è stata rilevata con metodica PAP. I risultati ottenuti hanno mostrato che in “acqua dura” con NH, la precipitazione del Cadmio inizia solo dopo quattro giorni dall’inizio dell’esperimento. Inoltre, indipendentemente dalla durezza dell’acqua, in presenza di NH3, l’assorbimento del metallo è sempre elevato, e la sopravvivenza non raggiunge il 15%. Tali dati sono un indice di maggiore tossicità rispetto a nostri precedenti studi su Carassius auratus esposti alla stessa quantità di cadmio, ma senza NH3, ove abbiamo riscontrato valori di assorbimento minori e sopravvivenza del 100%. Le indagini istologiche hanno evidenziato in acqua dura alterazioni della mucosa del bulbo con un aumento del turnover cellulare, numerose mitosi e riduzione delle dimensioni delle cellule mucipa¬ re. In acqua dolce, invece, si osservano segni di sofferenza delle cellule epiteliali e dilatazione delle cellule mucipare. Inoltre, sia in “acqua dura” che in “acqua dolce”, sono presenti cellule immunoreattive per la Met e la Leuencefalina. È possibile quindi affermare che, in presenza di NH3, raggiunta di cadmio determina un ambiente molto più tossico. Viene ipotizzato che ciò avviene, non solo perché l’NH3 si lega al cadmio formando dei complessi che aumentano fortemente la solubilità di quest’ultimo, ma anche perché molto probabilmente le varie specie di cadmio presentano una diversa permeabilità attraverso gli organi bersaglio. INTRODUCTION In previous researches on thè cadmium action concerning thè Caras¬ sius auratus gut kept in strongly calcareous waters thè Authors noticed, in shortterm, remarkable histomorphologic changes of thè intestinal mucosa and, in longterm, a good recovery capacity of thè exposed animals (An- dreozzi et al., 1992). Of particular interest was thè resulting disappearance, after a treatment of 7 days, of thè Met and Leuenkephalinelike immuno- reactivity, probably connected to thè increase of thè mucus production induced by thè cadmium (Andreozzi et al, 1992). On thè other hand, modifications in thè intracellular distribution of a peptide metenkephali- nelike have been described in thè intestinal epithelium of Carcinus moenas contaminated by heavy metals (AmiardTriquet et al, 1986). Battaglini et al. (1991) have reported in Carassius auratus , exposed to thè cadmium action a remarkable metal uptake in thè gut and, furthermore this Storage was connected to thè different hardness of thè experiment water. On thè other hand, thè toxic action of thè Cadmium varies in relation to thè chemicalphysic conditions of thè environment (Calamari et al., 1980) and to thè presence of other substances that can develop a chelating action towards thè ion Cd2+ (humic acids, aminoacids, porphyrins, purins) (Ravera, 1984; Sprague, 1987). 107 Andreozzi G., Antonucci R., Affai ato C., De Girolamo P., et al Among these substances thè Authors focused their attention to ammo- nia, produci of thè Carassius auratus catabolism, which Stores up in lentie waters in which these fìsh live. In particular, tke NH3 is important because it is a strong chelating agent of Cd2+ and then it can alter thè toxicity both varying thè speciation of this metal in thè solution and preventing its precipitation as CdC03 in calcareous waters (Battaglini et al., 1992). The purpose of thè present paper is to study thè toxic action of thè cadmium in thè catabolic NH3 presence on thè Carassius auratus gut in waters of different hardness. In particular we will to study thè histological and immunohistochemical changes of thè intestinal mucosa as well as thè changes of some neuropeptides. Materlals and methods Animals The experiment was carried out with waters of different hardness. The first kind, “hard water”, was thè tap water of Naples (hardness 369 mg/L of CaC03) and was utilized after an aeration period in a tank for an appropria¬ te dechlorination. The second kind, “soft water”, (152 mg/L of CaC03), was obtained by treating tap water with ionie exchange resins “Soft C” (line “C”), CARMAR, Napoli. Samples of Carassius auratus L., supplied by CARMAR sas (Naples), weighing 6 + 1 g, have been kepi for ten days to get acclimatized, in thè different kinds of water in two separate 600 L glass aquaria, equipped with an air pump and a filler (EHEIM, Germany). To get thè experiment 8 tanks (30x30x40 cm) were equipped with an air pump, without fìlter. During thè whole experiment thè temperature was constantly at 16 ± 1°C, and thè photoperiod was 12 hrs. 4 tanks were filled up with 20 L of “hard water” and 4 tanks were filled up with 20 L of “soft water”. 4 groups of 10 Carassius auratus, randomly chosen in thè acclimatiza- tion “hard water” glass aquarium, were transferred in thè four “hard water” tanks and fed as usuai with Tetramin Tetramere, Melle. The same was made for thè four “soft water” tanks. After 8 days in 3 “hard water” tanks and in 3 “softwater” tanks, CdCl2.21/2H20 was added in such a quantity to obtain a cadmium concen- tration in water equal to lOppm in each tank. 108 Boll Soc . Natur. Napoli - Voi . 101 ( 1992-1993 ) In such a way thè toxic was added when thè experiment water, after 8 days of animai stay, was enriched with catabolic fish materials and among them thè NH3, as we have already mentioned. The specimens from thè other two tanks were utilized as control. The cadmium treatment ran out for 7 days The survival was calculated as percentage of thè survived animals seven days after thè beginning of thè experiment. Chemical tests The analyses of thè components dissolved in thè water were carried out through thè traditional methods of volumetrie titration (Kolthoff et ai, 1973). To determine hardness, calcium and magnesium a standard solu¬ tion af sodium ethilendiaminotetracetic acid salt was utilized; to get thè alkalinity a 0.0 1 N solution of HC1 as titrating solution and green bromocre- sol as acidbase indicator was used; at last for thè chlorides a dosage with AgN03 according to Mohr method was used. All chemical produets utilized are Carlo Erba RP reagents, used without any further purification. To determine thè pH a pHmeter ORMA, model NK 300 was utilized; to determine thè dissolved oxygen was utilized a dissolved oxygenmeter HI 8543 (Hanna Instruments, USA). The NH ; produced and present in water was measured with a spectro- photometer using thè Nessler reagent to identify thè NH3 (Kolthoffet ai, 1973). The cadmium concentration in solution in thè different tanks was regularly measured by an atomic absorption spectrophotometer VARIAN AA275. A parallel precipitation kinetic of Cd2+ as CdC03 was effected in each kind of water used during thè experiments, but without fish and relative catabolic materials. Determination of cadmium uptake For each group of experimental animals, taken after seven days of exposure, guts ere used to determine thè cadmium uptake. Guts were weighed and mineralized by thè action of a HN03/HC104 mixture (ratio of concentrated acids 4:1) following K. Bull's method (1975). The resulting solution was brought up to a volume of 10 mL in a calibrated flask and analvsed by an atomic absorption spectrophotometer VARIAN AA275 to determine thè amount of cadmium. H ; • .. Andreozzi G.} Antonucci R., Affettato C., De Girolamo P., et al. 109 P ■" . ■ ■ . ■ ; Histology and Histochemistry After a treatment of 7 days for each experiment group, 2 Carassius auratus were taken and decapitated. At thè same time 2 control fishes were sacrificed for each kind of water. The gut, cranially dissected at intestinal sphincter level and caudally dissected at thè rectum end, was completely taken out. All thè specimens, after being Bxed in thè Bouin’s fiuid, were embed- ded in paraffin and serially cut into 7 pm sections. To study thè mucopolysaccharides thè following methods were car- ried out: - Periodic acid Schiff reaction. PAS was used in order to identify neutral mucopolysaccharides. - Alcian blue procedure. At pH 2.5 (A.B. pH 2.5) and at pH 1 .0 (A.B. pH 1.0) thè Alcian blue procedure was used alone or in combination with other procedures for thè Bnding and subsequent localisation of acid mucopolysaccharides. - Enzyme digestion test. Sections immediately following thè ones stained with A.B. pH 2.5 were digested with neuroaminidase (from Clostridium perf rigens type V, Sigma) at a concentration of 0.2% in phosphate buffer for 24 hr at 37°C to put in evidence thè sialomu- cins. The immunocytochemical tests were carried out by PAP method (Sternberger, 1979) to find out thè possible presence of Met and Leuenke- phalinelike material. In both cases thè primary antibody was used at 1:500 dilution. Then thè reaction product was displayed with 3.3’ diamine benzidine (DAB). The reaction specifity was tested both by replacing thè primary antibody with PBS and by thè absorption procedure. The control sections were stained with ematoxylineeosine (E. E.). Results Survival The survival analyses showed that aBer 7 days survival was inferior to 15% both in hard water and in soB water. Chemical characteristics Table I reports Chemical and physicochemical parameters of two diRerent waters utilized for thè experiments. It must be noted that thè 110 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) presence of catabolic ammorba, at zero time of thè treatment, reached a 7 -e 10 ppm concentration. Table I - Chemical and physico-chemical parameters of thè different waters Water properties Hard water Soft water Hardness (mg/1 CaCO, 369 152 Aìcalinity (mg/1 HC03~ 346 9,8 Ammonia (mg/1 NH3) 7-10 7-10 Chloride (mg/1 Cl" 32 30 Sulphate (mg/1 SO,2-) 25 25 pH 7,8 7,6 Dissolved oxygen (mg/1 0,) > 7 > 7 Temperature (°C) 16 ± 1 16 ± 1 Fig. 1 reports thè average concentration of cadmium in solution in thè experiment tanks with water having a higher hardness as a function of time ppm Figure 1 - Concentration of Cd2+ ion in solution in thè presence and in thè absence of catabolic products. Andreozzi G., Antonucci R., Affettato C., De Girolamo P.t et al 111 and, in comparison with thè sanie trend of thè cadmium concentration in thè same kind of water, but without Carassius auratus and thè relative catabolic materials. It is easy to note in thè two cases that thè kinetic of precipitation of CdC03 is completely different. In fact, in thè sample of water for comparison (without Carassus auratus) it is possible to note already in thè first hours, a fast and practically complete cadmium disappearance from thè solution. On thè contrary, with thè Carassius auratus thè precipitation occurs only after thè fourth day from thè begin- ning of thè treatment and, however, in a lower quantity, with a left concentration in solution of almost 2 ppm after 7 days. Vice versa, in water of lower hardness, thè cadmium lasts in solution for thè whole length of thè test, aside from thè Carassius auratus presence. Table II - Concentration of Cd2 in thè Carassius gut treated for seven days with NH., without NH; Hard water 71 1 412 Soft water 336 103 Cadmium uptake Tab. 2 reports thè cadmium Storage values measured with thè atomic absorption spectrophotometry in thè gut at thè seventh day of thè treat¬ ment for thè Carassius auratus treated in two different types of waters. In comparison, thè data of a previous research (Battaglini et al., 1992) are reported in thè same table, a research relative to thè cadmium uptalce in thè Carassius auratus guts treated for seven days in two different waters having characteristics similar to those utilized in this paper, but at thè beginning of thè previous research no catabolic ammonia was noted. It can be noticed that thè quantity of cadmium in thè organ is higher for thè Carassius auratus treated in water of higher hardness, as observed in thè previous experiment. It has also to be underlined that thè uptake is always higher when ammonia is present at thè beginning, no matter what kind of water is utilized. Carassius auratus gut structure The digestive System of thè Carassius auratus as all Cyprinids is rather simple because it has no stomach. 112 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) Thus, in thè Carassius auratus, thè oesophagus is in direct communi- cation with thè gut through thè oesophageal sphincter. The gut is of uniform size, except for a short cranial part, more dilated, called bulb ofthe gut. (Caceci, 1984). The gut mucosa, made of thè epithelium and thè connective tunic, raises in folds having a connective axes (Fig. 2). The epithelium is a single layer of cylindrical cells and contains several mucous cells (McVay and Kaan, 1940) less numerous in thè bulb area than thè other parts ofthe gut. They have a typical “drumstick” shape and produce a secretion made of neutral PASpositive mucins and AB pH 2.5 and pH 1.0 positive sulphurated acid mucins, neuroaminidase digestion resistant (Fig. 3). Also Metenkepha- line (Fig. 6) and Leuenkephaline (Fig. 9) positive neuroendocrine cells are mixed up with thè epithelial cells (Andreozzi et al., 1992). Such roughlv pyramidal and open cells are located onlv in thè bulb area and in thè most cranial part of thè gut. Figure 2 - Carassius auratus control -intestinal bulb - Alcian pH 2,5240X. Figure 3 - Carassius auratus control -intestinal bulb - Alcian pH 2,5380X. il 3 Apiér'eozjd G\, Antonucci Aifatato C\, De Girolamo P., et ah Figure 4 and 5 - Carassius auratus treated with Cd2' in hard water for seven davs - intestinal bulb - Alcian pH-3,5. Note very thin mucous cells and cells flankìng away in thè top of thè yiiìus - 600X. Boll Soc , Haiur. Napoli ~ Volò! 01- ( 1992-1993 ) ■y. 9 Figure 6 -- Caras- sius auratus con¬ tro! - intestinal bulb - metenke- phalin 800X Figures 7 and 8 - Carassius au¬ ratus treated wi~ th Cd2+ in hard water for seven days - intestinal bulb - metenke- phaìin 800X Figure 9 - Caras¬ sius auratus con¬ trol - intestina! bulb - leuenke- phalin 800X Figures 10 and 1 1 - Carassius auratus treated with Cd2+ in hard water for seven days - intestinal bulb - ìeu-enke- phaiin 800X Andreozzì G., Antonucci R,f Affettato C., De Girolamo P., et ah 115 Hard water experiment In thè animals exposed for seven days to thè cadmium action in hard water at thè presence of catabolic ammonia, thè gut mucosa appears to be rather damaged at thè bulb level and at thè more cranial part of thè gut. In fact, in these areas thè epithelium is often detached from thè inferior connective and it was noticed that some cells were flaking away. (Fig. 4, 5). The mucosa keeps a normal aspect only at thè bottom of thè folds and at thè remaining part of thè gut. The mucous cells, often much more elongated and thinned as compared to those of thè Controls, have positive granules scattered in thè whole cytoplasm up to thè base. In addition there are several mitosis. The histochemical reactions for thè mucopolysaccharides have shown, as for thè Controls, thè presence of positive A.B. pH 2.5 and pH 1 .0 positive acid mucins and neuroaminidase mucins resistant. There are also eells containing PAS positive neutral muans. The immuno reactive Metenkephaline cells seem to be more nume- rous and more significantlv positive as compared to thè Controls (Figures 7, 8). Their shape and distribution result unchanged. The IR (immunoreac- tive) cells for thè Leuenkephaline seem to be more significantlv positive as compared to thè Controls (Figures 10, 11). Their number and shape are similar to those of thè Controls. Soft water experiment In thè gut of thè animals treated for seven days with cadmium in softwater with catabolic ammonia, thè bulb mucosa appears suffering. In fact, thè epithelial cells appear coarted and thè mucous cells located at thè top of thè folds are often so swollen as to look like a “ball” or a “bag” with a highly thickened secretion. Sometimes it seems that thè nearbv cells merge themselves (Figures. 12, 13). Furthermore there is an increase of thè mucus mass contained in thè intestinal lumen. The histochemical reac¬ tions have shown, as in thè Controls, thè presence of PASpositive mucins and A.B. positive mucins, neuroaminidase resistant. Positive Metenkephaline and Leuenkephaline cells were found and their frequency and distribution were similar to those found in thè animals of Controls. 116 Boll. Soc . Natur Napoli - Voi. 101 (1992-1993) * V - • ^ v - ** 1 * _ ^ ■*{ * %4 * l vv -A*' £ 2* • v# -' «./:■''* «f >%•&* ». 44»?^ * * ' " ■:; * ; ; ^ 1 3r .: . r4* ^ ì; ,i ' : -ù «. » , "■'i WùwA • » * *ÀÌz^«! \ ^ ir V-4 - V A Mv> N * ?• g*^% ' /fè> l,; ■ * ' .v??; * a 4f'A/ . ^ Figure 1 2 and 1 3 - C arassi us anratus treated with Cd2+ in soft water for seven davs - intestina! bulb - Alcian pH 2,5 - Note thè mucous cells enlarged and sometimes merged (arrows). 380X. Andreozzi G Antonucci R Affatalo C., De Girolamo P., et Discussion The results obtained on thè Carassius auratus after 7 day treatment, suggest that thè cadmium shows a higher toxicity in thè presence of catabolic NH3. In addition, unlike what was noticed in our previous researches (Battagliai et ai, 1991) this action is not strictlv influenced by thè water hardness. The most signifìcant results obtained in this experiment are those concerning thè survival. In fact, in thè present experiment, after 7 days thè survival had not reached thè value of 1 5%. On thè contrary, in our previous experiments on Carassius auratus, we have reported that with equal cadmium concentration and lack of catabolic NH3, a survival up to 100% after 40 days in hard water (520 mg/L of CaC03) (Battaglini et al. , 1 992) and up to 90% after 40 days in soft water (150 mg/L of CaC03) (not yet published data). The histological researches, after 7 days of exposure to cadmium with catabolic ammonia, have focused signifìcant changes of thè intestinal mucosa, in particular at thè bulb level, with changes of thè mucus Storage and mucous celi shape. In thè specimens treated in “hard water” thè mucous cells appear thinner and elongated, with positive granules up to thè basai area, while in thè specimens treated in soft water they are verv swollen “bag” shaped with a very thickened secretion. In both cases thè immunoreactive Met and Leuenkephaline cells are positive and more numerous in thè specimens treated in hard water. These data differ from those described in our previous researches (Andreozzi et al, 1992; Andreozzi et al. 199 la, 199 lb). In highlv calcareous waters thè AA have observed, after a treatment of 7 days with cadmium, less damage at thè gut mucosa level and thè disappearance of immunoreac- tivity to Met and Leuenkephaline; in a longer period a remarlcable capacitv of restoring thè histological and immunocytochemical features was noted. Thus, a higher toxicity of cadmium in thè presence of catabolic NH 3 is evident and it appears with different characteristics in environments having different hardness. In fact, while in hard water thè numerous mitoses, thè detached epithelium and thè reduced sizes of thè mucous cells induce us to think of a turnover celi increment, on thè contrary, in soft water thè coarted aspect of thè epithelial cells is a sign of a suffering tissue condition, while thè increase of thè mucous celi size and a greater mucus quantity in thè intestinal lumen make us suppose a defensive reaction of thè epithelium itself. 118 Boll Soc . Natur. Napoli - Voi 101 ( 1992-1993 ) These data match with those described in Fnndulus by Gardner and Yevich (1970) and in Salmo gairdneri by Crespo et al ( 1 986) influenced by cadmium alone. In fact, these authors describe thè cellular “suffering” and thè mucus secretion increase. In addition, Crespo et al (1986), always in trout, describe also an increase in thè mitoses number. The presence of immunoreactive cells for thè Leu and Metenkephaline, after 7 day treat¬ ment, in contrast to what reported by Andreozzi et al (1992) could be related to an emergency situation from which thè animai cannot recover any longer. On thè contrary, thè atomic absorption data in thè gut after 7 days of treatment show a higher metal Storage in thè specimens treated in hard water compared with those treated in soft water. This datum is similar to what previouslv reported in goldfish by Battaglini et al (1991) on thè action of thè cadmium in waters of different hardness, without catabolic ammonia. In this case too, thè higher value in hard water is likely to be attribute to thè ingestion, even if in a lower quantity, of CdC03 which begins to precipitate on thè bottom after four days of experiment. In soft water, at thè same cadmium quantity dissolved in solution, thè presence of NH3 deter- mines a clear increase of metal Storage in thè gut as compared to what reported in specimens exposed onlv to thè cadmium (Battaglini et al, 1991). We can assert now that to thè same quantity of cadmium added thè “experimental environment” created results to be definitely more toxic. Th e reasons of such a higher toxicity can be, in our opinion, attributed just to thè presence of NLL expelled by thè fishes as catabolic material. In fact, thè first effe et of thè molecular ammonia is to bind itself to Cd2+ producing several complexes that stronglv increase thè CdCCft solubility developed in calcareous waters with Cd2+. In fact, in test tanks with thè goldfish and their catabolic materials, thè CdCCb precipitation is slower and inferior as compared to that which occurs in waters of thè same kind but without Carassius anratus. Thus, thè presence of catabolic ammonia determines a cadmium permanence in hard water as we observed in soft water. On this matter, a first hvpothesis would lead us to state that, in waters of higher hardness, thè highest toxicity of Cd2+ with NH3 can be connected to thè higher and longer presence of thè toxic in solution than in thè case in which ammoniacal materials. are lacking. But this element, even if important, cannot explain whv even in water of less hardness where thè CdCO , precipitation does not occur it is possible to obtain a definitely Andreozzi G.. Antonucci R., Affatalo C., De Girolamo P., et ah 119 lower survival with respect to that obtained in absence of NH3. As in ibis second case, thè Carassius auratus, with or without NH3, are in contact with thè same total amount of cadmium dissolved in solution (10 ppm) and are in environmental conditions almost similar, thè different survival observed could be ascribed to thè different cadmium speciation in solution and very likely to a different permeability, of different forms in which cadmium is present in solution, through thè organ targets of thè test animals. Acknowledgements This study was supported by a contribution of italian MURST (40% & 60%). REFERENCES Amiard-Triquet, C., J.C. Amiard, R. Ferrand, A.C. Andersen & M.P. Dubois, M.P. 1986. Disturbance of MetEnkephalinlike hormone in thè hepatopancreas of crabs contaminated bv metals. Ecofoxicologv and environmental s afe tv, 11: 198-209. Andreozzi, G., C. Affatato, R. Antonucci, P. Battagli ni, & G. Gargiulo, 199 la. Comportamento di alcuni peptidi nell’intestino di Carassius auratus trattato .con cadmio. Atti Soc. It. Sci. Vet. , 45: 277-280. Andreozzi, G., C. Affatato, R. Antonucci, P. Battagline G. Gargiulo, & P. Russo, 1 99 1 b. Effetti dell'esposizione al cadmio sulla mucosa intestinale di Carassius auratus. Atti 45" Conv. Soc. It. Anat. Sassari, 261. Andreozzi, G., R. Antonucci, C. Affatato, G. Gargiulo, & P. Battagline 1992. Influence du cadmium sur l’intestin de Carassius auratus. Anat. Histol. Embryol. , (in press). Battagline P-, G. Andreozzi, R. Antonucci, L. Ferrara, G. Gargiulo & C. Affatato, 1992. Azione del cadmio in presenza di NH, catabolico sull’intestino di Carassius auratus. Atti 54 Cong. U.Z.I. , 219. Battagline P., L. Ferrara, & O. Soppelsa, O., 1991. Assorbimento di Cd2+ in vari organi di Carassius auratus in acque HdureU e “dolci”. Atti Soc. It. Sci Vet., 4sT 149-153. Bull, K., 1975. Routine heavv metal analvsis of biological samples. Science Chelsea J. Res. Chel, 7: 23-25. Caceci, T. 1984. Scanning electron microscopv of goldfish, Carassius auratus, intestinal mucosa. J. Fish Biol. , 25: 1 12. Calamari, D., R. Marchetti, & G. Vailati, 1980. Influence of water hardness on cadmium toxicitv to Salmogairdneri Rich. WaterRes. , 14: 1421-1426. 120 Boll. Soc . Natur. Napoli - Voi 101 (1992-1993) Crespo, S., G. Nonnotte, D.A. Colin, C. Leray, L. Nonnotte, & A. Aubree, 1986. Morphological and functional alterations induced in trout intestine bv dietary cadmium and lead. J. Fish Biol., 28: 69-80. Gardner, G.R. & P.P. Yevich, 1970. Histological and hematological responses of an estuarine teleost to cadmium. J. Fish Res. Bd. Can., 27: 2185-2196. Kolthoff, I.M., E.B. Sandell, E.J. Meehan & S. Bruckenstein, 1973. Analisi Chimica Quantitativa. Padova, Piccin. Me Vay, J.A. & H.W. Karm, 1940. The digestive tract of Carassius auratus. Biol. Bull., 78: 53-67. Ravera, O. 1984. Cadmium in freshwater ecosystem. Experientia, 40: 214. Sprague, J.B. 1987. Effect of cadmium on freshwater fish. In Cadmium in Aquatic Environment, Nriagu, J.O. & Sprague, J.B. Eds., New York, J.Wiley, pp. 139-169. Sternberger, L.A. 1979. Imm u nocytochem istry , New York J. Wiley & Sons, Eds. CONTRIBUTI IN ITALIANO Boll Soc » Naiur. Napoli - Voi 101 (1992-1993); 1 23-140 123 Mammiferi olocenici provenienti da uno scavo effettuato nell 'isola di Capri (Italia meridionale) Barbera C., Lene! G., Rapuano M., Virgili A. Dipartimento di Scienze della Terra, Università degli Studi «Federico II», L.go San Marcellino 10, 80138 Napoli, Italy Riassunto, In questo lavoro si segnala la presenza di una mammofauna olocenica rinvenuta durante uno scavo recente nell'isola. Associati a reperti ceramici di età romana sono stati rinvenuti resti di Equus, Sus , Capra, Ovis, Bos e gallinacei. Per la prima volta, viene segnalata la presenza del Bos primigenius, specie non facente parte delle faune endemiche dell'isola. Gran parte dei reperti mostra chiari segni di bruciatura che sono riferibili ad avanzi di pasto, appartengono sia ad animali giovani che ad animali adulti ad eccezione di quello riferito al cavallo che sicuramente è appartenuto ad un individuo adulto. Premessa Questa nota si pone come obbiettivo l’identificazione di alcuni resti ossei rinvenuti nell'isola di Capri, in uno scavo effettuato a scopo edilizio in via Truglio 19. Lo studio dì questi reperti ha portato ad identificare la specie Bos primigenius Boi, mai segnalata prima nell'isola. I resti dei mammiferi in oggetto sono depositati presso il Centro documentale A. Ciccogliano di Capri e siglati con la lettera C seguita da numeri progressivi. Precedenti conoscenze Sulla zona esistono pochi dati bibliografici sia dal punto di vista geologico che paleontologico specialmente per i sedimenti della copertura pleistocenica. Received 14.5.92, accepted 27.1 1.92. 124 Boll Soc. Naiur. Napoli - Voi 101 (1992-1993) Rei lini (1910) riconosce, nel giacimento Qu isisan a Certosa ritrovato casualmente durante uno scavo per fondazioni edilizie e segnalatogli da E. Cerio, appassionato collezionista e raccoglitore di tutto il materiale rac¬ chiuso nel museo di Capri che porta il suo nome, una parte superiore di età olocenica con presenza di ceramiche del bronzo ed industrie del Neolitico medio, una intermedia di età pleistocenica-terminale presentante interca¬ lazioni di terra rossa con resti di cervidi e di una parte inferiore (Pleistoce¬ ne medio) con industrie litiche acheuleane e resti di grandi mammiferi. Bassani e Galderi (1911) verificano la stratigrafia dello scavo di Quisisana creando una apposita sezione ad esso adiacente. Azzaroli (1961) nel suo lavoro sul nanismo dei cervidi insulari dopo aver rivisto il materiale del livello intermedio di Cerio, Pigorini e Pelli. ni (1906), descrive una nuova specie di cervide nano dell’isola di Capri come Cervus tyrrenicus. Successivamente Piperno e Segre (1984) propongono una stratigrafia più aggiornata dei giacimenti Qu isisana C e rto sa e identificano cinque livelli, che dall’alto in basso sono: 1) Suoli e detriti non consolidati. 2) Pozzolane stratificate del Pleistocene superiore finale. 3) Terra rossa . 4) Tufo grigio campano , facies cineritica. 5) Argilla rossa con industria acheuleana e grandi mammiferi. Cinque, G bozzi ed Esu (1988) e successivamente Gliozzi (1989) ricono¬ scono in un riempimento della grotta “ Vascio o’ furino ” localizzata sul lato Sud Est dell’isola, una nuova specie di roditore Apodemus silvaticus thyrre- nicus con un cranio di grandi dimensioni e denti arcaici. Barbera e Cimmino (1990) in materiale subattuale di una grotta del versante orientale di Monte Solaro riconoscono resti di Suncus etruscus (SAVI), Rattus rattus (L.), Mus domesticus RUTTY, Apodemus sp.} Eliomys quercinus (L.). Alcune di queste specie, Suncus etruscus ed Eliomys quercinus non erano mai state segnalate nell’isola. Serie stratigrafxca Lo scavo in via Truglio, come da premessa, è stato effettuato quale sbancamento per uso edilizio. Esso ha raggiunto una profondità di circa 3,50 m e la successione dei sedimenti affioranti dall’alto verso il basso è la seguente: Burbera C\, Retici jjj , Rapitane J§|§ Virgili A, 125 m. 2,80 - terreno di copertura agraria m. 0,50 - ceneri vulcaniche m. 0,80 - pozzolane stratificate m. 0,30 - intercalazioni di terra rossa Data la vicinanza del sito di provenienza del materiale allo scavo di Quisisana Certosa descritto da Piperno e Segre (1984) è stato possibile confrontare le colonne stratigrafiche relative ai due giacimenti si è così notato che il materiale proveniente da via Truglio si rinviene in un livello che corrisponde al livello 3 (intercalazione di terra rossa) del giacimento di Quisisana. Probabilmente se lo scavo non fosse stato interrotto sarebbe stato possibile raggiungere il livello 5 con i grandi mammiferi e Pindustria litica di età acheuleana. Descrizione del materiale Per la descrizione del materiale viene usata la classificazione di Grzimek (1974). Tutto il materiale è stato confrontato con quello presente nei Musei Universitari Napoletani. èssendo la quasi totalità dei reperti in frammenti, i parametri delle tabelle sono riferiti alle ossa sulle quali è stato possibile effettuare misura¬ zioni. Caballus caballus (L.) Materiale esaminato: Un solo frammento di tibia di grandi dimensione appartenente ad un individuo adulto (Cl). Numero di esemplari 1. Sus scrofa (L.) Materiale esaminato. 2 canini sinistri, 1 superiore (C2) ed 1 inferiore (C3) 1 canino destro superiore (C4) 1 incisivo mandibolare sinistro (C5) 126 Boll Soc. Natur. Napoli - Voi , 101 (1 992-1 993 ) 2 PM superiore sinistri (C6, C7) 1 M2 superiore sinistro (C8) 2 frammenti mascellari, 1 sinistro (C9) ed 1 destro (CIO) 4 frammenti mandibolari, 3 sinistri (CI 1, CI 2, CI 3) ed uno destro (CI 4) 2 omeri destri frammentari (CI 5, CI 6) 1 omero sinistro frammentario (CI 7) 1 femore destro frammentario (CI 8) Numero minimo di individui: tre. Osservazioni : Due delle mandibole esaminate appartengono ad un individuo di età avanzata (C 11, C 14), mentre una delle mascelle appartiene ad un individuo di giovane età. Anche i canini appartengono ad individui giovani. Le ossa lunghe sono rotte a livello della dialisi. I parametri sono riportati in tab. I e II. Tab. I - Parametri morfometrici dei denti: Sus scrofa Linneo masc. dx clO h diam. meso-dist. diam. vest.-lingu. PM4 0,59 1,09 1 MI 0,33 1,38 1,31 M2 0,67 1,85 1,17 masc. dx c9 h diam. meso-dist. diam. vest.-lingu. PM4 0,83 1,17 0,86 MI 0,66 1,5 1,13 M2 0,99 1,7 1,24 masc. dx cl 1 h diam. meso-dist. diam. vest.-lingu. PM4 0,27 1,59 1,05 MI 0,76 1,54 1,85 M2 0,35 1,82 1,18 denti isolati h diam. meso-dist. diam. vest.-lingu. I C5 0,53 0,3 P M2 inf. dx C7 1,15 1,23 0,77 P M2 inf. sx C6 1,26 1,28 0,45 M 2 sup. sx C8 0,9 1,23 1,12 Barbera C,, Leuci G., Rapuano M., Virgili A. 127 Tab. II ■ ■ Parametri morfometrici delle ossa: Sus scrofa Linneo OMERO: misure longitudinali C 15 C 16 Diametro trasversale max estremità inf. 3,93 3,25 Diametro trasversale inf. troclea (f. post.) 2,77 2,58 Diametro trasversale sup. troclea (f. anter.) 1,5 1,2 Diametro verticale max troclea 3,62 3,12 Diametro trasversale sup. artic. (f. anter.) 2,82 2,29 Lunghezza foro oleocraneo 0,67 0,56 Larghezza foro oleocraneo 0,57 0,54 FEMORE: misure trasversali C 18 Lunghezza collo 1,78 Diametro trasversale della testa 2,47 TIBIA: misure trasversali C 17 Diametro trasversale epifisi inf. 2,88 Diametro antero-post. sup. art. inf. 1,74 Diametro trasversale sup. art. sup. 1,9 Capra hircus (L.) Materiale esaminato. 1 incisivo destro (CI 9) 2 MI inferiori destri (C20, C21) 2 M2 inferiori destri (C22, C23) 1 frammento di atlante (C24) 3 frammenti mandibolari, due destri (C25, C26) ed uno sinistro (C27) 1 frammento di radio destro (C28) 2 frammenti di coxale sinistro (C29, C30) 1 frammento di tibia destra (C31) Numero minimo di esemplari: due. Osservazioni : Tutte le mandibole, per quanto frammentarie presentano la serie dentale completa dai premolari. Alcune mandibole appartengono ad individui giovani (C26, C27), in quanto le cuspidi sono poco usurate. Le ossa lunghe sono rotte all’altezza della diafìsi. I parametri sono in tabella III e IV. 128 Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) Tab. Ili - Parametri morfometri dei denti: Capra hircus Linneo mand. dx C25 h diam. meso-dist. diam. vest.-lingu. PM1 0,94 0,54 0,53 PM2 1,02 0,74 0,67 PM3 1,1 1 1 0,78 MI 1,13 1,25 0,83 M2 1,18 1,61 0,93 M3 1,27 2,37 0,91 mand. sx C26 h diam. meso-dist. diam. vest.-lingu. PM2 1,07 0,82 0,58 PM3 1,16 0,93 0,6 MI 1,55 1,33 0,77 M2 1,46 1,51 0,84 M3 1,36 1,7 0,77 mand. sx CI 1 h diam. meso-dist. diam. vest.-lingu. PM2 1 0,71 0,61 PM3 1,1 0,84 0,62 MI 1,08 1,05 0,72 M2 1,31 1,31 0,87 M3 1,58 2,25 0,93 Ovis sp. vel Capra sp. Materiale esaminato: 1 calcagno sinistro (C32). Numero minimo di esemplari: uno. Osservazioni: Alcune rugosità decorrono dalla destra del corpo delhosso sino alla suspentaculum, ciò fa pensare che esso dovesse appartenere ad un animale selvatico. Barbera C., Leuci G., Rapuano M., Virgili A . 129 Tab. IV — Parametri morfometrici delle ; ossa: Capra hircus Linneo RADIO: misure trasversali C 28 Diametro trasversale della testa 2,57 Diametro trasversale del collo 2,05 Diametro trasversale fossetta radiale 1,83 Diametro antero-posteriore della testa 1,56 RADIO: misure longitudinali C28 Diametro antero-post. oleocraneo 1,05 Diametro antero-post. del corpo 0,52 Diametro antero-post. apofisi stiloide 0,52 BACINO: misure trasversali C 29 C 30 Diametro branca discendente pube 2,41 2,74 Diametro antero-post. cavità cotiloidea 2,54 TIBIA: misure trasversali C 31 Diametro trasversale del corpo 1,43 Diametro trasversale epifisi inf. 2,88 Diametro antero-posteriore sup. art. inf. 1,32 Diametro trasversale sup. art. sup. 1,82 Bos primigenius Boj Materiale esaminato: 1 MI superiore destro (C33) 1 porzione prossimale di ulna destra (C34) 1 metatarso destro rotto longitudinalmente e trasversalmente (C35) 1 II falange interna destra (C36) Numero minimo di individui: almeno due in quanto la porzione prossima¬ le di ulna appartiene ad un individuo di grandi dimensioni, mentre il metatarso appartiene ad un individuo adulto le cui dimensioni rientrano tra le minori della specie. Osservazioni : Sono stati fatti diversi tentativi di ricercare dei caratteri diagnostici nei denti isolati per distinguere il bove dal bisonte. Houle, 1906, indica come Boll Soc. Natur . Napoli « Voi IO 1 (1992-1 993} 130 caratteristica la forma più quadrata dei molari del bisonte. Altri AA. insistono di più sui caratteri del solo M3 della mandibola (Boessneck et al , 1963). Tuttavia i molari del bisonte sono più quadrati di quelli del bove; il lato labiale è meno appuntito, la copertura di smalto più forte. Il dente del bisonte effettivamente, è reso più corto e tozzo dalla diversa morfologia delle pieghe laterali e da una differente forma e posizione del talonide (Corridi, 1987). I confronti effettuati con materiale presente nel Museo di Paleontologia dell'Università di Roma hanno permesso di attribuire ad un MI superiore destro di Bos primigenius BOJ il reperto (C33) da noi esaminato. La porzione prossimale dell'ulna destra (C34) appartiene ad un indivi¬ duo giovane, dato il tipo di ossificazione, ma di grandi dimensioni; manca della tuberosità superiore e della porzione prossimale del becco dell'ole erano. Il reperto C35 è la porzione mediale di metatarso destro che oltre a rotture dovute all'estrazione probabile del midollo, presenta caratteristi- che striature dovute all'azione dell'uomo. I parametri sono in tabella V. Tab. V - Parametri morfometrici delle ossa: Bos primigenius : Boi SECONDA FALANGE int. dx: mis. longitud. C 36 Lunghezza massima 4 Altezza massima 2,08 SECONDA FALANGE int. dx: mis. trasvers. C 36 Diametro trasversale sup. 2,88 Diametro antero-posteriore estr. sup. 2,9 Diametro trasversale troclea 1,93 Diametro trasversale estr. inf. 2,24 Diametro antero-posteriore condilo interno 2,1 Diametro antero-posteriore condilo esterno 2,85 Diametro trasversale 2,44 Diametro antero-posteriore 2,23 Aves sp. et gen. ind. Tra il materiale da noi esaminato sono stati rinvenuti frammenti lunghi di ossa di gallinacei. Particolarmente ben conservati appaiono: 1 cubito destro (C37) 1 tibia sinistra (C38) 1 metatarso sinistro (C39) Numero minimo di esemplari: uno. B Utf pepli C.t Le&pì C , Mapuan® À, m Osservazioni : I gallinacei osservati sono di discrete dimensioni. Il cubito ed il metatarso sono in buone condizioni di fossilizzazione, la tibia si presenta rotta a circa i due terzi del corpo. I parametri sono in tabella VI. Taf*. VI - Parametri morfometrici delle ossa: Gailineacei TIBIA: misure longitudinali C 38 Lunghezza della cresta 2,47 TIBIA: misure trasversali C 38 Lunghezza incavo popliteo 0,7 Diametro trasversale del corpo 0,92 Diametro trasversale max estr. inf. 1,6 METATARSO: misure trasversali C 39 Diametro trasversale estremità sup. 1,45 Diametro anten>posteriore estr. sup. 1,05 Diametro trasversale del corpo 0,78 Diametro trasversale epifisi inf. 1,34 Diametro antero-posteriore epifisi inf. 0,37 Conclusioni L’insieme faunistico, seppure con i limiti dovuti alla tipologia del giacimento ed al metodo alquanto sommario di recupero può dare alcune informazioni sulla popolazione mammaliana dell’isola di Capri nel tardo Olocene. I grandi mammiferi come: Furo, Bos primigenius Boi, erano ivi rappresentati e probabilmente anche utilizzati dall’uomo sia come cibo che per il lavoro nei campi. Come cibo probabilmente venivano utilizzati gli altri animali costituenti la fauna (cinghiale, pecora, capra ecc.). Gran parte dei resti mostrano tracce di bruciature e tagli longitudinali, caratteristici dell’opera dell’uomo, tesi all’estrazione delle parti edibili in essi contenuti. Gli scarsi resti di ceramica, associati alle ossa che abbiamo fatto esaminare da colleghi archeologi della sovrintendenza ai Beni AA. di Napoli e Caserta ci hanno dato un arco temporale compreso tra il 1° secolo 132 Boll Soc . Natur . A/apo/i - FoT 101 {1991 1993} A.C.: ed il 11° D.C., periodo questo della urbanizzazione da parte dei romani dell'isola di Capri. L'interesse di questa nota resta quindi principalmente limitato alla prima segnalazione certa, con resti accertati di Bos primige- nius BOJANUS in epoca romana nell'isola di Capri. Ringraziamenti Ringraziamo il Prof. F. Barattolo del Dipartimento di Paleontologia per averci fornito il materiale dello scavo. I Direttori dei Musei di Zoologia della Facoltà di Scienze e di Anatomia Veterinaria dell'omonima Facoltà per averci permesso di confrontare il materiale. Ringraziamo le Dr. L. Caloi e E. Gliozzi per le proficue discussioni su Capri e per l'aiuto datoci nel determinare alcuni dei reperti di Bos. Ringraziamo la Dottoressa P. Gargiulo della sovrintendenza archeologica di Napoli e Caserta per l'esame del materiale ceramico. LAVORI CONSULTATI Azzaroli, A., 1961 . Il nanismo nei cervi insulari. Palaeont. It., Pisa, 56, n. s.: 1-32, 25 figg. 10 tavv. Barbera, C. &l M.G. Cimmino, 1990. Resti di insettivori e roditori di età recente raccolti in una grotta dell’isola di Capri (Italia). Histrix, Roma n. s. 2: 1 10, 1 tav. Bassani, F. & A. Galdieri, 1911. Scavo geologico eseguito a Capri. Atti Soc. It. Progr. Se., 4: 671-676, 3 figg. Bassani, F. & A. Galdieri, 1911. Strumenti chelleens dell'isola di Capri. Bull. Paleon., Parma, s. 4, 7: 5762, 3 figg. Boessneck, J., J.P. Jequier & H.R. Stampfli, 1963. Seeberg burgaschiseesud. Acta Bernensia, Berna, II Teil 3. Boule, M., 1906. Paleontologie. In: Villeneuve, Boule, Vernan, Cartallhac, Les grottes de Grimaldi (Baousse Rousse) , Monaco 1: 234-236. Cerio, L, L. Pigorni & U. Rellini, 1906. Materiali paleontologici dell'isola di Capri. Bull. Paleont. It., Roma, 23: 1 16. Cinque, A., E. Gliozzi & V. Esu, 1 986. Il riempimento della grotta “ Vascio ‘o funno" a Capri, primi risultati dello studio geomorfologico e paleontologico. Pubbl. Dip. Se. Terra Napoli, 33: 105-1 16, 2 figg., 1 tav. Corridi, C., 1 987. Faune pleistoceniche del Salento 2 La fauna di fondo Cattie, Maglie, Lecce. Ediz. Scient. Mus. comunale di Paleont. Quaderno 3: 730, 18 tav. Gliozzi, E., 1989. Apodemus sylvaticus tyrrenicus n. ssp. ( Muridae , Rodentia) from thè Upper Pleistocene of ndo Cattie, Maglie, Lecce. Ediz. Scient. Mus. comuna¬ le di Paleont. Quaderno 3: 730, 18 tav. Grzimek, A., 1974. La vita degli animali. Voi. 13. Ed. Bramante, Milano. Piperno, M. & A.G. Segre, 1984. Capri. In: I primi abitanti d’Europa. Scheda 77: 146-149. De Leca editore, Roma. Rellini, U., 1910. L'uomo preistorico nell'isola di Capri. Natura, Pavia, 1: 310. Rellini, U., 1923. La grotta delle Felci a Capri. Monum. Ant. Ac. Lincei, Roma, 29: 305-406, 36 figg., 2 tavv. Rellini, U., 1928. Il Paleolitico italiano secondo il Dr. R. Vaufrey. Bull. Palent. It., Roma, pt. 1: 110. 134 ' Boti, Soc . Natur. Napoli - Voi 101 (1992-1993) Tav. 1 - Capra hircus Linneo. 1. Emimandibola sinistra (C 26). Norma labiale. 2. Emimandibola sinistra (C 27). Norma linguale. 3. Emimandibola destra (C 25). Norma labiale. Boll Soc . Natur. Napoli - Voi 101 ( 1992-1993 ) 136 Tav. 2 - a) Bos primigenius Boj. 1. Porzione prossimale di ulna destra (C 34). Circa 1/2. 2. Primo molare superiore destro (C 33). b) Sus scrofa Linneo. 3. Femore destro (C 18). Norma anteriore. 4. Omerotro (C 16). Norma posterodistale. 5. Omero destro (C 15). Norma posterodistale. 6. Omero sinistro (C 38). Norma posterodistale. 7. Emimandibola sinistra (C 10). SKff 138 Boll Soc. Natur. Napoli - Voi 101 (1992-1993) t Tav. 3 - a) Aves gen. et sp. indet . 1. Cubito destro (C 37). 2. Cubito destro (C 37). 3. Tibia (C 38). 4. Tibia (C 38). 5. Metatarso (C 39). b) Ovis vel Capra 6. Calcagno sinistro (C 32). c) Ceramica. 7 Frammento di vaso. Tutte le figure sono in grandezza naturale tranne C 34 che è circa 1 /2 delToriginale. JMJ, Soc.., Nitur. mpbU ' ir/t Wì '{1992-1 9^3 j: 14J-14S • 141 Il Dissesto Idrogeologico Vallarlo A, Professore Ordinario di Geologia Applicata Dipartimento di Scienze della Terra Facoltà di Scienze» Università degli Studi «Federico II» da una Conferenza alla Società dei Naturalisti in Napoli Gli eventi naturali ed antropici succedutisi negli ultimi due secoli sono stati caratterizzati da un crescendo» rapido superamento di fasi storiche e sociali» in relazione alla progressiva affermazione e diffusione della società industriale» alFincremento della popolazione» all 'ampl iarsi di centri urba¬ ni» alla concentrazione delle aree industriali» al veloce progresso dello sviluppo tecnologico e all 'utilizzo indiscriminato delle risorse naturali» trascurando nel contempo la qualità della vita, le condizioni di lavoro e gli effetti alterativi ed inquinanti che le attività antropiche avrebbero potuto determinare all'ambiente nell'immediato e nel futuro (Dì Donna e Valla¬ no» 1992» 1993a.» 1993b; Vallano, 1992a). In tale contesto il rapporto dell'uomo con l'ambiente naturale è stato improntato» prevalentemente, al principio dello sfruttamento. Posizione questa sviluppata dalle filosofie occidentali per le quali l’uomo è l'essere superiore in grado di sottomettere la natura. Va ricordato a tal proposito che anche l'insegnamento cristiano si pone nella stessa posizione come specificato in un versetto della Genesi che esorta l'uomo e la donna a crescere e moltiplicarsi ed ad usare la terra, rendendosela soggetta. (Dorsi.. 1988). Solo negli ultimi decenni l'incalzante ripetersi di catastrofi e di disastrosi fenomeni alterativi dell'ambiente fisico (Catenacci» 1992), tra l'altro conseguenti al modelli socioeconomici prevalenti» ha determinato l'unanime ammissione che l'uomo ha avuto il molo di agente attivo nell'alterazione degli equilibri naturali. Infatti le attività antropiche» sem¬ pre più incisive ed irrispettose dell'ambiente fìsico e delle risorse naturali» hanno agito come fattori della dinamica esogena al pari delle acque superficiali del vento e delle escursioni termiche» con l'aggravante che l'uomo agisce senza soluzione di continuità ritenendo» tra l'altro» di essere l'unico indiscusso padrone e beneficiario dì tali beni» mentre avrebbe avuto interesse ad assumere il molo del rispettoso e raziocinante custode Boll Soc. Natur. Napoli - Voi 101 (1992-1993) di un patrimonio unico, comune a tutti gli esseri viventi, e non rinnovabile in tempi umani Nel vasto panorama di equivoci voluti e determinati per perseguire lo sfruttamento intensivo ed estensivo delle potenzialità naturali ha svolto un ruolo determinante la mancanza di una visione complessiva delle proble¬ matiche ambientali e, soprattutto, di un disegno programmatico di indiriz¬ zo politico e gestionale che ha agevolato, quando non direttamente inne¬ scato, il progressivo depauperamento dell'ambiente fisico e delle risorse naturali (Ministero dell'Ambiente, 1992, Vallario, 1992b). Ambiente fisico e potenzialità naturali Ambiente è quanto comprende ed interagisce, mediante complesse relazioni funzionali dirette ed indirette con l’uomo, gli altri esseri viventi, il mondo inorganico, le condizioni geologiche, biologiche, fìsiche e chimi¬ che che costituiscono e, quindi caratterizzano un determinato spazio geografico. Tutti gli elementi costituenti l'ambiente risultano tra loro interdipendenti in vario modo e con diversa intensità, in tempi a scala geologica e umana, a seconda delle circostanze, dei processi e dei fenome¬ ni considerati. Un ambiente rappresenta un sistema in cui al variare di condizioni interne e/o esterne possono mutare i rapporti tra le sue varie componenti; in tal modo alcune di esse, col procedere del tempo, possono perdere il carattere di prevalenza per essere sostituiti da altri che rappre¬ sentano l'effetto dei nuovi mutamenti. Il sistema ambiente non può, quindi, ritenersi statico ma in continua evoluzione dinamica (Vallario, 1992a). La complessità degli elementi costitutivi e le loro ampie interrelazioni lasciano intendere che l'ambiente va considerato come una realtà unitaria nella sua struttura, nei suoi meccanismi e nei suoi equilibri dinamici e che l’uomo ha assunto, via via nel tempo, un ruolo sempre più determinante quale parte integrante del sistema. Le tematiche inerenti all’ambiente che più direttamente interessano l’uomo devono avere come obiettivi gli strumenti per giungere ad una approfondita analisi dei fenomeni e la conoscenza delle potenzialità naturali, ciò per consentire una corretta pianificazione e gestione antropi¬ ca del territorio. Gli elementi di giudizio necessari a sviluppare un approccio culturale corretto delle problematiche ambientali derivano dalla conoscenza dei Vallano A . 143 fenomeni naturali. Questa, partendo dall'analisi delle componenti dell'am¬ biente, può consentire di giungere alla ricostruzione dei modelli morfoe- volutivi e quindi alle previsioni sia sull’innesco di nuovi fenomeni alterati¬ vi che sulle reazioni agli stessi. Ciò equivale a prevedere e quindi program¬ mare un'adeguata prevenzione ai conseguenti rischi per la vita e per le opere dell’uomo. Le potenzialità naturali sono rappresentate oltre che dalle risorse rinnovabili e non,, quali le acque superficiali e sotterranee, l'aria, i combustibili fossili, i materiali naturali da costruzione, le fonti energeti¬ che, le materie prime, anche dal paesaggio, dal suolo, dalla fauna, dalla flora, dai parchi naturali, dalle risorse alimentari e dalle caratteristiche fisiche dell'ambiente che in diversi casi hanno costituito presupposti indispensabili per lo sviluppo economico e sociale di alcune regioni (Vallario, 1991). L'assetto e l’uso razionale del territorio dovrebbero scaturire dalle conoscenze acquisite, dalle caratteristiche fisiche dell’ambiente e dalla entità e tipologia delle potenzialità naturali disponibili in un certo ambito geografico. Nell'approccio all’ambiente fisico sembra opportuno ricordare che la configurazione geomorfologica attuale di un certo sito rappresenta solo un istante a scala umana della sequenza che ha dato luogo nei tempi geologici al susseguirsi di processi e forme che hanno determinato l'evoluzione a cui è stata sottoposta quella porzione di superficie terrestre sotto l'azione degli agenti esogeni (acque meteoriche, escursioni termiche, ecc ) ed endogeni (eventi tettonici, fenomeni vulcanici, sismi, ecc.). Aspetti questi che hanno costituito, da circa quaranta anni, argomenti di studio da parte di molti ricercatori italiani quali, ad esempio: Gisotti e Bruschi, 1990; Guida et al., 1974, 1979, 1981; Ippolito, 1954, 1962, 1967, 1972a, 1972b, 1973; Vallario, 1973, 1992b, 1993a, 1993b). Il rischio geologico L'uomo vive ed opera, prevalentemente, in corrispondenza della porzione più superficiale della crosta terrestre; proprio in quella parte in cui avvengono, o si avvertono, gli effetti dei fenomeni di modellamento, di trasformazione, di alterazione, di adattamento o di reazione connessi, in modo diretto o indiretto, agli agenti della dinamica endogena ed esogena, (Bolt et al, 1975, Vallario, 1992b). L'insieme dei fenomeni geologici e dei loro effetti sulla superficie terrestre rappresenta quella che possiamo definire la pericolosità geologi¬ ca, la porzione della superficie terrestre dove vivono ed operano comunità antropiche rappresenta, invece, la potenziale vulnerabilità’ antropica di un dato territorio ai fenomeni geologici. Il rischio geologico è la combinazione della pericolosità geologica e della potenziale vulnerabilità antropica di un territorio, espresso in termini di rapporto tra i prevedibili eventi di pericolosità geologica, la loro intensità e frequenza e le relative interferenze con le attività antropiche. Tra gli eventi di pericolosità geologica devono rientrare sia i fenomeni naturali che quelli indotti dalle attività antropiche quali, ad esempio, i fenomeni vulcanici, i terremoti, le alluvioni, i maremoti, le erosioni intense della superficie terrestre, le frane, la subsidenza, il bradisismo, gli effetti delle grandi infrastrutture antropiche sull'evoluzione della superfi¬ cie terrestre, l'inquinamento, ecc. La potenziale vulnerabilità antropica può comprendere l’intensità e il tipo di urbanizzazione, l’uso del territorio, l’industrializzazione, la presen¬ za di infrastrutture viarie, le opere di captazione di importanti sorgenti, opere di adduzione da liquidi o gas, opere di scarico di liquami, la presenza di bacini artificiali, ecc. Da ciò deriva, quindi, che il rischio geologico è strettamente connesso alle attività antropiche e che può essere ridotto agendo non tanto sui fenomeni geologici, peraltro difficilmente controllabili, ma soprattutto, mediante un uso oculato e razionale del territorio da parte dell’uomo (Vallano 1991). Aspetto particolarmente significativo per la definizione del rischio geologico in un determinato sito è la individuazione di tutti gli elementi geologici e delle cause che, di volta in volta, si combinano negativamente concorrendo a turbare gli equilibri, tali conoscenze dovranno applicarsi ai fattori di potenziale vulnerabilità per definire le strategie di intervento che costituiranno oggetto ed obiettivo della programmazione, della pianifica¬ zione e della gestione del territorio, per ben rispondere alle esigenze umane (Benedini e Gisotti, 1985; Greco, 1992; Vallario, 1992b). Boll. Soc. Natur. Napoli - Voi. 101 (1992-1993) Il dissesto idrogeologico Tra i processi evolutivi di maggiore incisività e velocità che sconvolgo¬ no l’ambiente fisico sono da includere le frane, i fenomeni di intensa erosione e le alluvioni; fenomeni questi di primaria importanza per gli effetti catastrofici che possono produrre sulle opere, sulle attività e sulla Vallano A. 145 vita stessa degli uomini. Questi fenomeni che sconvolgono tanto profonda¬ mente l'ambiente fìsico ed il territorio rientrano nelle fenomenologie del così detto dissesto idrogeologico, definizione questa che tende a mettere in rilievo che tali fenomeni alterativi hanno cause determinanti nelle acque superficiali e sotterranee. Le catastrofi naturali che più frequentemente incombono sul territo¬ rio del nostro paese, sono da collegare a fenomeni di intensa erosione, a movimenti in massa o frane o ad alcuni particolari aspetti della dinamica fluviale (alluvioni) in quanto costituenti gli elementi più diffusi e maggior¬ mente incisivi nell’evoluzione rapida dell'ambiente fìsico, eventi questi che vengono comunemente indicati con la denominazione di rischio idrogeologico e comprendono quelle catastrofi, che derivano dalla fre¬ quente combinazione di irrazionali utilizzazioni antropiche dell'ambiente fìsico e da, più o meno sfavorevoli, condizioni geologiche e morfologiche. Sembra opportuno ribadire che l’evoluzione dell'ambiente fìsico è condizionata prevalentemente dai processi di rapido modellamento conse¬ guenti alla dinamica fluviale (alluvioni), alla dinamica dei versanti (feno¬ meni erosionali e frane) e alla dinamica dei litorali (variazioni delle linee di costa e dei fondali). Si definisce alluvione l’insieme dei fenomeni legati all'alta velocità dell’acqua nella rete drenante superficiale, all’erosione, al trasporto e successivo deposito di ingenti quantità di materiale solido fine e grossola¬ no, sia nell’alveo che nelle aree limitrofe, in occasione dello straripamento dei corsi d'acqua. Gli effetti di tali fenomeni sono disastrosi in quanto 1' onda di piena che si propaga da monte a valle aumenta in portata e velocità. Con l’aumento della portata l’acqua, non più contenuta nell’al¬ veo, può invadere le aree circostanti, con l’aumento della velocità essa si carica di detriti e incrementa ancor più la propria energia, provocando intensi fenomeni erosionali con successivo deposito del materiale eroso e trasportato. Tali fenomeni stravolgono interi bacini imbriferi modificando sia le condizioni morfologiche precedenti e sia i modelli morfoevolutivi; i loro effetti disastrosi sono da collegare, oltre che a condizioni Onaturali, anche all’utilizzazione insensata dell'uomo di quelle parti pianeggianti, prospi¬ cienti gli alvei, che vengono invase dalle acque solo nei periodi di eccezionale piovosità. Adeguate opere idrauliche di regimazione delle piene e di regolazione delle sponde e dei profili di fondo, la sistemazione dei bacini montani e il mantenimento di aree di rispetto per lo smaltimento delle piene sono gli 146! Boll Soc. Natur. Napoli - Voi mi (1992-1993) interventi che hanno consentito di ridurre notevolmente gli effetti distrut¬ tivi delle alluvioni. Tra gli interventi antropici particolarmente incidenti sulla dinamica fluviale è indispensabile ricordare l'asportazione di ingenti quantità di materiali alluvionali dagli alvei dei corsi d'acqua; queste azioni hanno avuto incidenza via via crescente a partire dagli anni cinquanta, quando sotto la spinta del forte sviluppo economico sono iniziate le massicce realizzazioni di infrastrutture viarie e di innumerevoli costruzioni di ogni genere e tipo che hanno utilizzato i depositi alluvionali per realizzare rilevati stradali e per la confezione del calcestruzzo. Questo fenomeno, nel complesso rapporto tra i diversi elementi dell'ambiente fisico, ha provoca¬ to anche sostanziali modificazioni, a volte irreversibili, al regime dei litorali; inoltre, le asportazioni hanno generato l'abbassamento progressi¬ vo degli alvei con conseguenti crolli di manufatti, franamento delle difese di sponda e modificazioni, anche profonde, degli articolati sistemi erosio¬ ne-trasporto-sedimentazione. La dinamica dei versanti comprende i fenomeni di intensa erosione ed i movimenti in massa. I fenomeni erosionali sono legati quasi esclusiva- mente all'azione meccanica delle acque dilavanti che, per la forza di gravità, si spostano da monte a valle. I movimenti in massa o frane sono costituiti dalla caduta più o meno rapida o, comunque, dallo spostamento lento e differenziale di masse rocciose o di materiali sciolti, per gravità. In tal senso appare evidente che i fenomeni erosionali e le frane sono agenti modellatori particolarmente incisivi che non solo modificano localmente, ma intervengono in maniera determinante nell'evoluzione dell'ambiente fisico in quanto, alterando la geometria dei versanti e le forme del suolo, agevolano l'insorgere di nuovi meccanismi di trasformazione che si so¬ vrappongono ai precedenti e, in alcuni casi, si sostituiscono ad essi. In molte zone del territorio nazionale le caratteristiche geologiche inducono all' instaurarsi diffuso di fenomeni di tal tipo che spesso raggiungono l'entità di vere e proprie catastrofi naturali (Vallano, 1992a e b). L'agente principale della dinamica dei litorali è costituito dall'azione del moto ondoso; un ruolo del tutto subordinato spetta alle correnti marine. La tendenza evolutiva delle coste basse, quelle di maggiore interesse per le attività antropiche, oltre che dagli elementi naturali, dipende dagli interventi dell'uomo. I tratti di costa che si possono ritenere naturalmente stabili sono estremamente limitati in quanto è difficile che si possa realizzare l'equilibrio duraturo tra apporti, erosioni e trasporto dei materiali. Vallano A. 147 1 Altra azione antropica di alterazione degli equilibri è la costruzione di opere costiere quali moli, pennelli e scogliere che, modificando le modali¬ tà di trasporto del materiale lungo costa, provocano erosioni ed accumuli anomali rispetto agli schemi naturali. Val la pena di ricordare che se non si ripristinano le condizioni naturali alterate dall’escavazione dei materiali dagli alvei dei corsi d'acqua, non si potranno raggiungere condizioni di equilibrio naturali. Unica alternativa concreta a tali situazioni è il ripascimento artificiale delle coste basse. Il ripetersi di eventi catastrofici di ampiezza ed entità sempre maggio¬ re e, in particolare, l'alluvione dell'Arno del 1966 suggerirono l'istituzione di una Commissione Interministeriale per avviare finalmente una ricogni¬ zione conoscitiva sul territorio nazionale. Gli studi ed i rilevamenti effettuati misero in evidenza nel 1970 che era necessaria una spesa di 8.932 miliardi, da investire in un trentennio, per la difesa del suolo e la sistemazione idraulica sul territorio nazionale. In particolare erano previsti 5.300 miliardi per la difesa idraulica del suolo, 429 miliardi per la sistemazione di frane e la prevenzione di valanghe, 2.370 miliardi per la sistemazione idraulicoagraria e per il potenziamento silvo-pastorale e 824 miliardi per la difesa dei litorali (Commissione Interministeriale, 1970). Da allora molto è cambiato soprattutto nello sfruttamento del territo¬ rio e delle risorse naturali, con conseguenze sempre più catastrofiche ed irreversibili. In ciò l'uomo ha avuto un ruolo prioritario e determinante ed è da ritenere l'agente modellatore che ha avuto le maggiori responsabilità rispetto agli eventi naturali. BIBLIOGRAFIA Benedini, M. & G. Gisotti, 1985. Il dissesto idrogeologico. Cause, effetti e interventi a difesa del suolo. La Nuova Italia Scientifica, Roma. Bolt, B.A., W.L. Horn, G.A. Macdonald & R.F. Scott, 1975. Geologie al Hazards, Springer-Verlag, Berlin. Catenacci, V., 1992. Il dissesto idrogeologico e geoambientale in Italia dal dopo¬ guerra al 1990. Serv. Geol. Naz., Mem. Descr. della Carta Geologica d’Italia, voi 47, Istituto Poligrafico e Zecca dello Stato, Roma. Commissione Interministeriale per lo studio della sistemazione idraulica e della difesa del suolo, 1970. Atti della Commissione, Camera dei Deputati, Roma. Di Donna, V. & A. Vallario, 1992. Ambiente fisico, territorio e realtà socio-econo¬ mica. Geologia Tecnica & Ambientale , Ordine Nazionale dei Geologi, n. 2, Roma. 148 Boll Soc . Natur. Napoli - Voi 101 (1992-1993) Di Donna, V. & A. Vallario, 1993a. Uomo e ambiente fìsico. Istituto di Ricerca e di Didattica Ambientale Napoli (IREDA), Bollettino delle Attività, voi 2. Di Donna, V. & A. Vallario, 1993b. Ambiente: risorse e rischi. Liguori Editore. Dorst, J., 1988. Prima che la natura muoia. Verso una riconciliazione dell’uomo e della natura. Muzzio Editore, Padova. Gisotti, G. & S. Bruschi, 1990. Valutare V ambiente. La Nuova Italia Scientifica, Roma. Greco, N., 1992. La pianificazione dell’ambiente fisico in Italia. Quaderni Ambien¬ te, Edistudio, Roma. Guida, D., M. Guida, G. Iaccarino, G. Metcalf, A. Vallario, V. Vecchio & G. Zicari, 1979. Il bacino del Mingardo (Cilento): evoluzione geomorfologica, fenomeni franosi e rischio a franare, Geol. Appi, e Idrogeologia, voi. 14, p. II, Bari. Guida, D. , M. Guida, D. Luise, G. Salzano, A. Vallario, 1981. Geologia e franosità del Fiume Lambro (Cilento). Geologica Romana, voi. 20, Roma. Guida, M., G. Iaccarino, A. Vallario, 1974. Il dissesto idrogeologico del territorio comunale di Cardeto (Reggio Calabria). Considerazioni di Geologia ambienta¬ le, Geol. Appi, e Idrogeologia, voi. IX Bari. Ippolito, F., 1954. L'ambiente geologico della montagna meridionale. La Ricerca Scientifica CNR, voi 24, n. 10, Roma. Ippolito, F., 1962. La geologia e l’uomo. Saggi e studi di geologia, Venezia. Ippolito, F., 1967. Il disordine idrogeologico. Nord e Sud, n. 86, Napoli. Ippolito, F., 1972a. La geologia nella difesa del suolo. Atti II Conv. Naz. di Studio sui problemi della Geologia Applicata, Genova. Ippolito, F., 1972b. La geologia ambientale. Simp. sulla gestione delle risorse naturali e sulla protezione dell’ambiente di Città del Messico. Ippolito, F., 1973. L ‘ambiente e 1 ‘uomo. Le Scienze, Milano. Ministero dell’Ambiente, 1992. Relazione sullo stato dell’ambiente, Istituto Poligra¬ fico e Zecca dello Stato, Roma. Vallario, A., 1973. Geologia e franosità nell’area ad oriente del Taburno-Campo- sauro e del Partenio (Provincie di Benevento ed Avel lino). Geol. Appi, e Idrogeologia, voi. Vili, parte II, Bari. Vallario, A., 1991. Uomo, ambiente e rischio geologico. Orizzonti Economici. Rivista della Camera di Commercio di Napoli, n. 71. Vallario, A., 1992a. L’ambiente. Geologia Tecnica & Ambientale , Ordine Nazionale dei Geologi, Roma. n. 1 . Vallario, A., 1992b. Frane e territorio. Le frane nella morfogenesi dei versanti e nell’uso del territorio. Liguori Editore, Napoli. Vallario, A., 1993a. Un approccio metodologico allo studio delle frane e alla cartografia previsionale. Conferenza Dibattito su “I fenomeni franosi nella gestione del territorio”. Associazione Geologi Palermo. Vallario, A., 1993b. Il rischio idrogeologico nell’evoluzione dell’ambiente fisico e dei versanti. Corso Introduttivo alla Geologia Ambientale, Società Italiana di Geologia Ambientale (S.I.GE.A.) e Ordine dei Geologi del Lazio, Roma. 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