Smaller Foraminifera From Guam - USGS
Smaller Foraminifera From Guam - USGS
Smaller Foraminifera From Guam - USGS
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Significant benthonic <strong>Foraminifera</strong> in the Miocene samples of<br />
the Janum Formation Continued<br />
Species<br />
Nodosaria insecta<br />
Schwager.<br />
Nodosaria skobina<br />
Schwager.<br />
Orthomorphina fijiensis<br />
(Cushman).<br />
Orthomorphina perversa<br />
(Schwager).<br />
Osangularia culter (Parker<br />
and Jones).<br />
Pleurostomelia alternans<br />
Schwager.<br />
Pleurostomelia brevis<br />
Schwager.<br />
Pyrulina labiata<br />
(Schwager).<br />
Siphogenerina striata<br />
(Schwager).<br />
Stilostomella verneuili<br />
(d'Orbigny).<br />
Vulvulina spinosa<br />
Cushman.<br />
SMALLER FORAMINIFERA FROM GUAM 111<br />
Reported occurrences elsewhere<br />
Miocene of Kar Nicobar and Java;<br />
late Miocene and early Pliocene<br />
of Borneo; Tertiary of Japan.<br />
Miocene of Kar Nicobar.<br />
Pliocene of Fiji.<br />
Miocene of Kar Nicobar; Miocene of<br />
Jamaica; Oligocene of Cuba;<br />
Pliocene of Italy.<br />
Miocene of Kar Nicobar; Eocene,<br />
Oligocene, and Miocene of Sai-<br />
pan; Eocene of Mexico and Cali<br />
fornia ; middle Eocene to lower<br />
Oligocene of Barbados; Eocene<br />
and Miocene of Spain; Aquita-<br />
nian of Algeria; Eocene of Bul<br />
garia.<br />
Miocene of Kar Nicobar; Miocene<br />
and Pliocene of Borneo ; Pliocene<br />
of Fiji; Miocene of Jamaica;<br />
Tertiary of Dominican Republic ;<br />
Eocene and Oligocene of Bar<br />
bados ; Miocene of Spain, France,<br />
and Egypt; Pliocene of Italy and<br />
Greece.<br />
Miocene of Kar Nicobar; Pliocene<br />
of Fiji; Miocene of Japan; Eo<br />
cene of Saipan; Miocene of Ja<br />
maica and Dominican Republic;<br />
Miocene of Spain, France, and<br />
Algeria.<br />
Miocene of Kar Nicobar; Pliocene<br />
of Fiji.<br />
Miocene of Kar Nicobar; Miocene<br />
and Pliocene of Borneo and Java;<br />
Eocene and Miocene of Saipan;<br />
Eocene and Oligocene of Trinidad.<br />
Miocene of Vienna Basin; Miocene<br />
of Sumatra; Eocene, Oligocene,<br />
and Miocene of West Indies; Eo<br />
cene, Oligocene, and Miocene of<br />
Spain.<br />
Oligocene, Alazan Formation of<br />
Mexico; upper Eocene of Vene<br />
zuela ; Oligocene of Trinidad;<br />
upper Oligocene of Dominican<br />
Republic; middle Eocene to lower<br />
Oligocene of Barbados; Miocene<br />
of Spain; Pliocene of Japan ; Re<br />
cent of Philippines.<br />
The chief local differences between the Miocene and<br />
the Recent benthonic faunas are in the families Textu-<br />
lariidae (7 species in the Recent and 1 in the Miocene),<br />
Miliolidae (52 in the Recent and 2 in the Miocene),<br />
Spirillinidae and Discorbidae (15 in the Recent and<br />
not represented in the Miocene), and the families<br />
Rotaliidae, Pegidiidae, Amphisteginidae, Calcarinidae,<br />
and Cymbaloporidae (27 in the Recent and only 3<br />
rotaliids in the Miocene). Thus there is not much in<br />
common between the Miocene benthonic and the Recent<br />
benthonic faunas. If anything, I believe the kinds of<br />
benthonic species present in the Miocene, supported by<br />
the negative evidence of the kinds that are not present<br />
in the Miocene, indicate that the beds represented by<br />
the few Miocene samples studied were deposited at<br />
greater depths and farther from shore than the Recent<br />
outer slope samples that were taken from depths less<br />
than 200 fathoms.<br />
Table 3 gives by localities the smaller <strong>Foraminifera</strong><br />
of Miocene age found in the Janum Formation on<br />
<strong>Guam</strong>. Discrepancies are to be found between the<br />
species noted in my original examination of these same<br />
samples (Tracey and others, 1964, p. A43) and the<br />
species given in table 3. These discrepancies have re<br />
sulted from (a) the shifting of a species from one genus<br />
to another (such as Eponides umbonatus to Oridorsalis<br />
and Siphonodosaria fijiensis to Orthomorphina) ; (b)<br />
the synonymizing of one species with another (such as<br />
Globigerina veneziwlana, a synonym of G. conglom-<br />
erata, and Osangularia bengalensis, a synonym of 0.<br />
culter) ; (c) the correction of identification (such as<br />
Pulleniatina obliquiloculata for Globigerina inflata and<br />
Globorotalia hirsuta for G. canariensis) ; and (d) the<br />
refinement of identification (such as Gyroidina lamar-<br />
ckiana and G. soldanii for G. spp.). In addition, some<br />
of the indeterminate species and those whose generic<br />
placement was questioned in the original study have<br />
been eliminated from table 3.<br />
TABLE 3. Distribution of smaller <strong>Foraminifera</strong> in the Miocene<br />
of <strong>Guam</strong><br />
Species<br />
Textulariidae:<br />
Vulvulina spinosa Cushman___________<br />
Valvulinidae:<br />
Eggerella bradyi (Cushman)___________<br />
Karreriella bradyi (Cushman)__________<br />
Miliolidae:<br />
Quinqueloculina lamarckiana d'Orbigny.<br />
Pyrgo murrhina (Schwager)___________<br />
Lagenidae:<br />
Robulus sp__________________________<br />
Dentalina communis d'Orbigny. _______<br />
tauricornis Schwager. ____________<br />
sp. A_____-___-_--_______.______<br />
Dentalinal spp._____-___-___-____--_<br />
Nodosaria equisetiformis Schwager _<br />
insecta Schwager.________________<br />
skobina Schwager ________________<br />
Lagena gracilis Williamson.___________<br />
Poly m orphinidae:<br />
Pyrulina labiata (Schwager) ____ _______<br />
Buliminidae:<br />
Buliminella septata Keyzer____________<br />
Bulimina aguafrescaensis Todd and<br />
Kniker. __________-____-__-__--_--<br />
Fissurina alveolata (Brady)__________<br />
circulum Seguenza____-___-__-___<br />
formosa (Schwager)______________<br />
globosa Bornemann_______________<br />
Bolivina aff. B. nitida Brady __________<br />
pusilla Sehwager_________________<br />
silvestrina Cushman______________<br />
aff. B. sinuatum Galloway and<br />
Wissler_ ______________________<br />
X<br />
X<br />
X<br />
X<br />
Localities<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X