- Page 1 and 2: UTRECHT MICROPALEONTOLOGICAL BUllET
- Page 3 and 4: QUANTITATIVE FORAMINIFERAL ANALYSIS
- 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: literature together with Pachysphae
- Page 17 and 18: Fig. 3 Subhorizontally stratified a
- Page 19 and 20: Mappa. These successions are hard t
- Page 21 and 22: Transitional interval showing the g
- Page 23 and 24: 2 3 4 2 3 1 5 2 6 1 8 10 1 1 9 2 4
- Page 26 and 27: A composite section of the Trubi is
- Page 28 and 29: Section 3 The sampled section 3 cov
- Page 30 and 31: sediment, corresponding in colour t
- Page 32 and 33: 98 and 99). The total thickness of
- Page 34 and 35: Figs. 12 and 13. Chondrites-burrows
- Page 36 and 37: sedimentation have not been found.
- Page 38 and 39: drites are trace-fossils consisting
- Page 40 and 41: 45 42 \ Sample numbers I' '07 107G
- Page 42 and 43: of planktonic individuals decreased
- Page 44 and 45: stabilizing bottom conditions. The
- Page 46 and 47: i i " J~ u ! " ~ , ~ II~ , ~ " If C
- Page 48 and 49: " " ~ 1 ~ .~ ~ " " · ~ .2> ~ · I
- Page 50 and 51: Siphonina bradyana and Pullenia are
- Page 52 and 53: "0 l/l ~.!? ~c w ...J c> c_ o. ._~
- Page 54 and 55: sediments are concerned. Stabilizat
- Page 56 and 57: 10 and 16 per 300 counted individua
- Page 58 and 59: Graph showing the numerical distrib
- Page 60 and 61: extremely rare in our Trubi materia
- Page 62 and 63: figs. 20 and 22, which possibly ind
- Page 64 and 65:
in label appreciation that addition
- Page 66 and 67:
N.padfic(54} [ $. PaciFic (54) Paci
- Page 68 and 69:
la alternans, Sigmoilopsis celata,
- Page 70 and 71:
elatively high B/P ratio (29/200) a
- Page 72 and 73:
(/) W FREQUENCY ~ ~ ...J ~'" '" DIS
- Page 74 and 75:
ing very hypothetical and unreliabl
- Page 76 and 77:
Although the top of the Trubi and t
- Page 78 and 79:
29 • 28 • 27 • . 0 $ E E Q 0
- Page 82 and 83:
pyrIttc cores similar to those from
- Page 84 and 85:
pyntlc limestone mud may have resul
- Page 86 and 87:
The sharply increased B/P ratio in
- Page 88 and 89:
1 I S 1 3" ' I , 6 I 3 ' 9 I z , 4
- Page 90 and 91:
The lower O'-indices in most of the
- Page 92 and 93:
------ Cibicides lobatu/us -- Hanza
- Page 94 and 95:
the bottom-bound vegetation. It sho
- Page 96 and 97:
N ,. ~ I~ ~ .. ~ , ~ ~ ~ g -u ~ I~
- Page 98 and 99:
ed from the uppermost sample (figs.
- Page 100 and 101:
~ '53 18 D 17 16 C 15 ~ '4 13 Ul B
- Page 102 and 103:
seems reasonable to hold the additi
- Page 104 and 105:
Graph showing the relative proporti
- Page 106 and 107:
4 200 ṃ N 0 FA U N A - - - - - -
- Page 108 and 109:
ticulata and the appearance of Glob
- Page 110 and 111:
Mrs. Cita), which causes our G. inf
- Page 112 and 113:
6) Uvigerina peregrina-pygmea and H
- Page 114 and 115:
throughout the Trubi and Narbone fo
- Page 116 and 117:
assemblages, after which the gradua
- Page 118 and 119:
ting oxygen-dependent bottom life.
- Page 120 and 121:
studied by Wright from site 371 (19
- Page 122 and 123:
layers. This movement must have bee
- Page 124 and 125:
fauna experience this change in env
- Page 126 and 127:
etween site 371 and Sicily. These o
- Page 128 and 129:
find support in the description of
- Page 130 and 131:
Epistominella exigua (Brady) PI. 2,
- Page 132 and 133:
Globorotalia bononiensis Dondi PI.
- Page 134 and 135:
NUMBERED LITERATURE REFERRING TO BA
- Page 136 and 137:
67. Egger, J. G. (1893). Foraminife
- Page 138 and 139:
North Atlantic. J. For. Res., v. 4,
- Page 140 and 141:
(1971). Repartition des biocoenoses
- Page 142:
Fig. 1 Fig. 2 Figs.3a-b Figs.4a-b F
- Page 146:
Figs. la-b Fig. 2 Figs.3a-b Figs. 4
- Page 150:
Pachysphaera. Small and large speci
- Page 154:
Variation of Globorotalia puncticul
- Page 158:
Bull. 12. J. T. VAN GORSEL - Evolut