^G9-A? 2:
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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
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d"
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rn
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co
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m
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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
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d
d
04
d
d
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d
d
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d
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1— 1
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NO
fN
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d
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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
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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
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o
o
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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).
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Kawamata, J., Y. Harada & N. Tagashira, 1986. Electron microscopie study of thè
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Kido, T., T. Sekitani, H. Yamashita, S. Endo, Y. Masumitsu & H. Shimogori, 1991.
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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.
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Boll Soc . Natur. Napoli - Voi 101 (1992-1993)
Korhonen, E. & L.K. Korhonen, 1965. Histochemical demonstration of carbonic
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Lillie, FR., 1952. Development of thè chick. Ed. H. Holt and Company, New York.
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de Vincentiis, M. & F. Marmo, 1968. Inhibition of thè morphogenesis of thè otoliths
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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 /> Girolamo P.t S ammaro o M., Gargiulo G.
No immunoreactive reaction was detected when control slides were
treated with normal rabbit serum or with phosphate-buffered saline in-
stead of thè specific antiserum.
For thè identification of thè anatomical structure, and thè following
nomenclature we referred to Kuenzel and van Tienhoven (1982).
IN '
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 ’ - •
,
»
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. ,v
t ti-
I
'
V I
-■ , #? ;
; ’! 'G ' ■
v- ; ‘ v -
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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.
In conclusion, these observation indicate thè presence of both enke-
phalin-like and g-endorphin-like immunoreactive substance in thè chicken
hvpothalamus, which might be involved in thè pituitary regulation and/or
in other neuronal functions as neuromodulator.
This studv also provide a foundation for further studies to elucidate thè
role of g-END in thè brain of thè domestic chick and other birds.
Acknowledgments
This studv was partiallv supported by a contribution of Italian Murst
(40% and 60%).
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'
'
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%).
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Waarde van A., 1983: Aerobic and anaerobic ammonia production by fish. A
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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.
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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
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149
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