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Chaproniere, George C H (1994): (Table 1) Distribution of larger benthic and planktonic foraminifers in ODP Hole 135-841B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.802252, Supplement to: Chaproniere, GCH (1994): Middle and late Eocene larger foraminifers from Site 841 (Tongan Platform). In: Hawkins, J; Parson, L; Allan, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 135, 231-243, https://doi.org/10.2973/odp.proc.sr.135.118.1994

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Abstract:
Larger foraminifers were recovered from three levels within Hole 841B, located on the Tongan Platform. The lowest faunas are from Eocene beds (Unit V) in fault contact with an older rhyolitic volcanic sequence. These Eocene faunas are typified by two assemblages: one with Amphistegina waiareka, Astewcyclina matanzensis, Discocyclina omphala, Operculina pacifica, together with rare Heterostegina saipanensis and Sherbornina carteri; the second assemblage contains these species and, in addition, Spiroclypeus vermicularis. The lowest assemblage is associated with a middle Eocene planktonic foraminifer fauna (Acarinina, Morozovella), and the upper faunas with a late Eocene assemblage. This Eocene unit is disconformably overlain by a middle Miocene sequence (Unit IV) containing assemblages dominated by planktonic foraminifers. Two samples were found to contain shallow-water benthic foraminifers: one contained Amphistegina radiata, Cycloclypeus sp., Lepidocyclina (Nephrolepidina) ?howchini, and Sphaerogypsina globula; a second sample from this section contained only Amphistegina radiata. The third level at which larger foraminifers were found was in the lower part of the late Miocene section (Unit III), where late Eocene larger foraminifers (Asterocyclina matanzensis, Discocyclina omphala, Nummulites pengaronensis, and Pellatispira madaraszi) are present in a conglomeratic sequence with late Miocene planktonic foraminifers present in the matrix.
The two larger foraminifer assemblages of Unit V are typical of the Ta3 and Tb Letter Stages, which are distinguished by the presence of Spiroclypeus vermicularis. The Ta3 Letter Stage assemblage is associated with a Zone P14 planktonic fauna, and the Tb Letter Stage assemblage with Zones PI5 to PI6 fauna.
The larger foraminifers associated with middle and late Eocene planktonic foraminifers are almost certainly in situ, and indicate water depths from between 50 and 100 m in the middle Eocene, shallowing to <50 m, and then gradually deepening to >100 m by the end of the Eocene. The middle Miocene faunas have been derived from shallow-water environments adjacent to the sites of deposition (which would have been in excess of 100 m), and may have been contemporaneous or reworked from rocks no older than the Ta5 Letter Stage. Late Eocene larger foraminifers (Tb Letter Stage) were reworked into the deep-water, late Miocene environments as products of erosion from adjacent exposures of Eocene carbonates.
A hiatus is probably present in the lower part of the Eocene section, separating the middle and late Eocene (Ta3 and Tb Letter Stages-Zones P14 and P15). This is probably the result of eustatic changes. Unit V almost certainly contains the Eocene/Oligocene boundary, based on the planktonic foraminifer evidence, but larger foraminifers disappear some distance below this boundary, within Zones P15 or P16. The larger foraminifer faunas from Units III and V provide evidence that water depths at this part of the Tongan Platform have increased from approximately 50 m during the late middle Eocene to below the calcium carbonate compensation depth by the late Miocene, respectively.
Project(s):
Coverage:
Latitude: -23.346000 * Longitude: -175.297000
Date/Time Start: 1991-02-02T15:40:00 * Date/Time End: 1991-02-10T20:30:00
Minimum DEPTH, sediment/rock: 345.09 m * Maximum DEPTH, sediment/rock: 605.02 m
Event(s):
135-841B * Latitude: -23.346000 * Longitude: -175.297000 * Date/Time Start: 1991-02-02T15:40:00 * Date/Time End: 1991-02-10T20:30:00 * Elevation: -4821.0 m * Penetration: 834.2 m * Recovery: 182.54 m * Location: South Pacific Ocean * Campaign: Leg135 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 70 cores; 664.4 m cored; 0 m drilled; 27.5 % recovery
Comment:
X = present, ? = questionable occurrence, - = absent.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Sample code/labelSample labelChaproniere, George C HDSDP/ODP/IODP sample designation
DEPTH, sediment/rockDepth sedmGeocode
Globigerinatheka sp.Globigerinatheka sp.Chaproniere, George C H
Globigerinoides extremusG. extremusChaproniere, George C H
Globigerinoides ruberG. ruberChaproniere, George C H
Globoquadrina dehiscensG. dehiscensChaproniere, George C H
Globorotalia sp.Globorotalia sp.Chaproniere, George C H
Globorotalia tumida plesiotumidaG. tumida plesiotumidaChaproniere, George C Hquestionable
Foraminifera, planktic indeterminataForam plankt indetChaproniere, George C H
10 Morozovella sp.Morozovella sp.Chaproniere, George C H
11 Orbulina universaO. universaChaproniere, George C H
12 Pulleniatina sp.Pulleniatina sp.Chaproniere, George C H
13 Sphaeroidinellopsis spp.Sphaeroidinellopsis spp.Chaproniere, George C H
14 Subbotina eocaenaS. eocaenaChaproniere, George C H
15 Amphistegina radiataA. radiataChaproniere, George C H
16 Amphistegina awiarekaA. awiarekaChaproniere, George C H
17 Asterigerina tentoriaA. tentoriaChaproniere, George C H
18 Asterocyclina matanzensisA. matanzensisChaproniere, George C H
19 Biarritzina sp.Biarritzina sp.Chaproniere, George C H
20 Cibicides sp.Cibicides sp.Chaproniere, George C H
21 Cycloclypeus sp.Cycloclypeus sp.Chaproniere, George C H
22 Discocyclina omphalaD. omphalaChaproniere, George C H
23 Discogypsina discusD. discusChaproniere, George C H
24 Halkyardia minimaH. minimaChaproniere, George C Hgenus questionable
25 Heterostegina saipanensisH. saipanensisChaproniere, George C H
26 Foraminifera, benthic porcelaneous indeterminataForam benth porc indChaproniere, George C H
27 Foraminifera, benthic rotalidia indeterminataForam benth rotalidia indetChaproniere, George C H
28 Foraminifera, benthic agglutinated indeterminataForam benth agg indChaproniere, George C H
29 Lenticulina sp.Lenticulina sp.Chaproniere, George C H
30 Lepidocyclina howchiniL. howchiniChaproniere, George C HL. (Nephrolepidina) ?howchini
31 Nonionella sp.Nonionella sp.Chaproniere, George C H
32 Nummulites pengaronensisN. pengaronensisChaproniere, George C H
33 Operculina pacificaO. pacificaChaproniere, George C H
34 Pellatispira madarasziP. madarasziChaproniere, George C H
35 Sherbornina carteriS. carteriChaproniere, George C H
36 Sphaerogypsina globulusS. globulusChaproniere, George C H
37 Spiroclypeus vermicularisS. vermicularisChaproniere, George C H
38 BryozoaBryozoaChaproniere, George C H
39 Algae abundanceAlgae abundChaproniere, George C Hcoralline, articulated
40 Algae abundanceAlgae abundChaproniere, George C Hcoralline, nodular
41 EchinoideaEchinoideaChaproniere, George C H
42 HalimedaHalimedaChaproniere, George C H
43 MolluscaMolluscaChaproniere, George C H
44 OstracodaOstracChaproniere, George C H
Size:
860 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Sample label

Depth sed [m]

Globigerinatheka sp.

G. extremus

G. ruber

G. dehiscens

Globorotalia sp.

G. tumida plesiotumida
(questionable)

Foram plankt indet
10 
Morozovella sp.
11 
O. universa
12 
Pulleniatina sp.
13 
Sphaeroidinellopsis spp.
14 
S. eocaena
15 
A. radiata
16 
A. awiareka
17 
A. tentoria
18 
A. matanzensis
19 
Biarritzina sp.
20 
Cibicides sp.
21 
Cycloclypeus sp.
22 
D. omphala
23 
D. discus
24 
H. minima
(genus questionable)
25 
H. saipanensis
26 
Foram benth porc ind
27 
Foram benth rotalidia indet
28 
Foram benth agg ind
29 
Lenticulina sp.
30 
L. howchini
(L. (Nephrolepidina) ?howchini)
31 
Nonionella sp.
32 
N. pengaronensis
33 
O. pacifica
34 
P. madaraszi
35 
S. carteri
36 
S. globulus
37 
S. vermicularis
38 
Bryozoa
39 
Algae abund
(coralline, articulated)
40 
Algae abund
(coralline, nodular)
41 
Echinoidea
42 
Halimeda
43 
Mollusca
44 
Ostrac
135-841B-20R-2,111-115345.09------X-?----X-----X---------X-X----------
135-841B-20R-3,66-69346.14-----XX-XX--------------------------------
135-841B-21R-2,131-135354.91----X-X-?------X---X----X-------------X---
135-841B-21R-3,88-92355.95------X---X-------------X-----------------
135-841B-22R-1,5-8361.45-?----X--------X---X----------------------
135-841B-22R-2,146-150364.36-------------------X-----------?----XX--X-
135-841B-22R-3,10-14364.50-------------X-----X----------X----XXX----
135-841B-40R-4,23-27539.96---?--X-----X------------X----------X---X-
135-841B-41R-2,110-114547.60--?---X-----X-----X-----XX-X-----X--X-----
135-841B-45R-CC585.07-------------------X----------------------
135-841B-46R-1,35-39593.25X-----X------XXX---X--X-XX----X--XXXX-X-X-
135-841B-46R-1,88-91593.78?-----X-------XX---X---------XX--X-XX-X-X-
135-841B-46R-2,62-65595.02------X----?-X-X---X----X-----X----XX-X-X-
135-841B-46R-2,140-143595.80-------------XXXX--X--X-XX----X--X-XX-X-X-
135-841B-46R-3,10-13595.96-------------XXX---X----XX----X----XX---X-
135-841B-46R-CC596.47-------------X-XX--X?-X-X-----X-X-XXXXXX--
135-841B-47R-1,92-96603.52?-----XX-----XXX---X-X-XXX----X----XX-X---
135-841B-47R-2,37-42604.47-------------XX--X----------X-X----X--X--X
135-841B-47R-2,79-83604.89-------------XXX-X-?----X-X-X-X----X--X-XX
135-841B-47R-2,92-9605.02X-----XX-----XX----X----XX----X-X--XXXX---