UTRECHT MICROPALEONTOLOGICAL BUllETINS

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Editor C. W. Drooger Department of Stratigraphy and Paleontology State University of Utrecht Oude Gracht 320, Utrecht, Netherlands Bull. 1. T. FREUDENTHAL - Stratigraphy of Neogene deposits in the Khania Province, Crete, with special reference to foraminifera of the family Plan orbulinidae and the genus Heterostegina. 208 p., 15 pl., 33 figs. (1969) f32,- Bull. 2. J. E. MEULENKAMP - Stratigraphy of Neogene deposits in the Rethymnon Province, Crete, with special reference to the phylogeny of uniserial Uvigerina from the Mediterranean region. 172 p., 6 pI, 53 figs. (1969)f 29,- Bull. 3. J. G. VERDENIUS - Neogene stratigraphy of the Western Gualdalquivir basin, S. Spain. 109 p., 9 pl., 12 figs. (1970) f28,- Bull. 4. R. C. TJALSMA - Stratigraphy and foraminifera of the Neogene of the Eastern Guadalquivir basin, S. Spain. 161 p., 16 pl., 28 figs (1971) f 44,- Bull. 5. C. W. DROOGER, P. MARKS,/A. PAPP et al. - Smaller radiate Nummulites of northwestern Europe. 137 p., 5 pl., 50 figs. (1971) f 37,- Bull. 6. W. SISSINGH - Late Cenozoic Ostracoda of the South Aegean Island arc. 187 p., 12 pl., 44 figs. (1972) f57,- Bull. 7. author's edition. F. M. GRADSTEIN - Mediterranean Pliocene Globorotalia, a biometrical approach. 128 p., 8 pl., 44 figs. (1974) f 39,- Bull. 8. J. A. BROEKMAN - Sedimentation and paleoecology of Pliocene lagoonalshallow marine deposits on the island of Rhodos (Greece). 148 p., 7 pl., 9 figs. (1974) f47,- Bull. 9. D. S. N. RAJU - Study of Indian Miogypsinidae. 148 p., 8 pl., 39 figs. (1974) f38,- Bull. 10. W. A. VAN WAMEL - Conodont biostratigraphy of the Upper Cambrian and Lower Ordovician of north-western bland, south-eastern Sweden. 128 p., 8 pl., 25 figs. (1974) f 40,- Bull. 11. W. J. ZACHARIASSE - Planktonic foraminiferal biostratigraphy of the Late Neogene of Crete (Greece). 171 p., 17 pl., 23 figs. (1975) f52,-
QUANTITATIVE FORAMINIFERAL ANALYSIS AND ENVIRONMENTAL INTERPRETATION OF THE PLIOCENE AND TOPMOST MIOCENE ON THE SOUTH COAST OF SICILY
Page 1: UTRECHT MICROPALEONTOLOGICAL BUllET
Page 5 and 6: The foraminifera. . . . . . . . . .
Page 7 and 8: Benthonic and planktonic foraminife
Page 9 and 10: and considerable lowering of the er
Page 11 and 12: topmost Messinian evaporites, chara
Page 13 and 14: literature together with Pachysphae
Page 16 and 17: Data and conclusions from the earli
Page 18 and 19: 2 3 Ammonia beccarii Bolivina dente
Page 20 and 21: LITHOLOGY The new exposure to be de
Page 22 and 23: may interfinger. Evidently biogenic
Page 24: CONCLUSIONS The mediocre preservati
Page 27 and 28: 107 107G B.C 107A 106 1394 64 1393
Page 29 and 30: Fig. 9 Laterally displaced loadcast
Page 31 and 32: Orbulina, which in turn seem to dep
Page 33 and 34: 0 10 20cm. L--L--J ~II\\ :::0 if.-
Page 35 and 36: whether its assumed intermediate st
Page 37 and 38: cate that larger burrowing organism
Page 39 and 40: The foraminiferal faunas from the T
Page 41 and 42: 42 43 44 45 sa~ 3 4 4 Astrononion i
Page 43 and 44: the accumulation of silica-rich sed
Page 45 and 46: 1 1 i z 1 1 11 3 1 i ~ . 2 •• 7
Page 47 and 48: ently favoured clayey substrates bu
Page 49 and 50: The next higher part of the section
Page 51 and 52: Cibicides pseudoungerianus appears
Page 53 and 54:
In the next higher interval the alt
Page 55 and 56:
high. It remains equally possible t
Page 57 and 58:
I 106 55 52 j 8 Ij I " ~ ~ ! I ll11
Page 59 and 60:
107A 107B 107C 107D 107E 107F 107G
Page 61 and 62:
of the faunas remains practically t
Page 63 and 64:
5 -- 4 3 2 7 - - - - - - - - - - -
Page 65 and 66:
;.Monica Say(32) Todos Santos 8ay (
Page 67 and 68:
1000 m, the latter corresponding to
Page 69 and 70:
In this respect it is interesting t
Page 71 and 72:
for this interval at the three loca
Page 73 and 74:
near-absence and bloom. The level o
Page 75 and 76:
Fig. 30 Punta Piccola section, show
Page 77 and 78:
Chlorite/montmorillonite and albite
Page 79:
most of them are of the order of 15
Page 83 and 84:
The change in colour from cream to
Page 85 and 86:
The foraminiferal faunas from the M
Page 87 and 88:
, " ~ " , , . ~ . ~
Page 89 and 90:
posite- reactions with higher a-val
Page 91 and 92:
------ Cibicides lobatu(us -- Hanza
Page 93 and 94:
Bulimina inflata, Hopkinsina bononi
Page 95 and 96:
Parker, 1954). In the Andaman Sea t
Page 97 and 98:
athymetric distribution is shown in
Page 99 and 100:
in the manganese-rich interbeds (B
Page 101 and 102:
50 1~N 47 46 45 43 4 M 42 L 41 4 39
Page 103 and 104:
Emiliani (1974) analyzed core mater
Page 105 and 106:
20323, was deposited at the transit
Page 107 and 108:
it is realized that the latter two
Page 109 and 110:
FREQUENCY D ISTR I BUTION OF SOME S
Page 111 and 112:
BENTHONIC FORAMINIFERAL ASSOCIATION
Page 113 and 114:
IK < .o~
Page 115 and 116:
ed by the increase of epiphytes and
Page 117 and 118:
G. puncticulata, recorded from Aren
Page 119 and 120:
our sample 93 suddenly shows a B/P
Page 121 and 122:
loss may be due to the folding. The
Page 123 and 124:
shallowing tendency. This quiet sed
Page 125 and 126:
One of the major aims of this inves
Page 127 and 128:
anean evidently had a nutrient supp
Page 129 and 130:
A taxonomical treatment of all figu
Page 131 and 132:
Remarks: Globigerina pseudobesa (Sa
Page 133 and 134:
Remarks: Colalongo and Sartoni (196
Page 135 and 136:
30. Earland, A. (1934). Foraminifer
Page 137 and 138:
Anderson, G. ]. (1963). Distributio
Page 139 and 140:
Hsii, K. J., Cita, M. B. and Ryan,
Page 141 and 142:
Wright, R. (1977). Neogene paleobat
Page 144:
Figs. 1a-b Figs. 2a-b Figs.3a-b Fig
Page 148:
Figs. 1a-c Figs. 2a-c Figs. 3a-c Fi
Page 152:
Fig. 1 Fig. 2 Figs.3a-b Fig. 4 Fig.
Page 156:
Morphological gradation from Globor
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UTRECHT MICROPALEONTOLOGICAL BUllETINS

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