DIATOM ZONATION

Thalassiosira lentiginosa Partial Range Zone

Author: McCollum (1975), renamed by Kellogg and Kellogg (1986)
Definition of top: LO of Thalassiosira lentiginosa (still extant)
Definition of base: LO of Actinocyclus ingens
Age: 0-0.64 Ma
Discussion and remarks: Gersonde and Bárcena (1998) determined the first abundant occurrence (FAO) and last abundant occurrence (LAO) of Hemidiscus karstenii to be 0.19 and 0.42 Ma, respectively. These ages agree with those observed by Harwood and Maruyama (1992). In the material from this leg, H. karstenii was observed in low numbers in Holes 1095C, 1096A, 1096B, and 1101A. The LAO of this species was noted to be at 0.15 Ma (Hole 1095C) and 0.16 Ma (Holes 1096A and 1096B), and the FAO occurred at 0.29 Ma (Hole 1095C) and 0.26 Ma (Holes 1096A and 1096B). As the upper portions of all the holes exhibit noncontinuous diatom abundance and barren intervals, these ages should be considered with this in mind. H. karstenii was rarely observed in two samples from Hole 1101A, making age determinations in this hole imprudent. Site 1095 was the only one to include the last occurrence datum of Actinocyclus ingens, thereby definitely placing the lower boundary of the T. lentiginosa Zone at this site.

Actinocyclus ingens Partial Range Zone

Author: Gersonde (1990), modified by Harwood and Maruyama (1992), further modified in this zonation
Definition of top: LO of Actinocyclus ingens
Definition of base: LO of Thalassiosira kolbei
Age: 0.64-1.85 Ma
Discussion and remarks: This zone is a combination of two from Harwood and Maruyama (1992). The LO of Fragilariopsis barronii was used to define a boundary between their A. ingens and F. kerguelensis Zones. As F. barronii was not consistently observed in large numbers, we combined the two into one. The last occurrences of Thalassiosira elliptipora and Thalassiosira torokina were observed for this zone at Site 1095. This zone was not identified at Site 1096. The LO of T. torokina was also observed at Site 1101, as were F. barronii (LO) and Thalassiosira fasciculata (LO). The species datum indicating the base of this zone, the LO of T. kolbei, was not seen at any of the three sites; this taxon was only rarely observed in the present study.

Thalassiosira kolbei Partial Range Zone

Author: Ciesielski (1983), renamed by Baldauf and Barron (1991)
Definition of top: LO of Thalassiosira kolbei
Definition of base: LO of Thalassiosira vulnifica
Age: 1.85-2.4 Ma
Discussion and remarks: The base of this zone was defined at all three sites with the LO datum of T. vulnifica. The LOs of T. complicata and T. inura were also noted at both Sites 1095 and 1096, whereas the LO of Actinocyclus karstenii was the only datum observed within this zone at Site 1101.

Thalassiosira vulnifica Partial Range Zone

Author: Ciesielski (1983), renamed by Fenner (1991)
Definition of top: LO of Thalassiosira vulnifica
Definition of base: LO Thalassiosira insigna
Age: 2.4-2.6 Ma
Discussion and remarks: The LO datums of F. interfrigidaria and T. insigna were not observed at Site 1095, but some well-preserved specimens of these two species were observed in Holes 1095A and 1095D. Sites 1096 and 1101 did preserve the LO datums for both of these species. Sample 178-1096B-29X-CC (239.6 mbsf) contained an abundance of T. insigna poorly preserved central areas. These were often noted, in lower numbers, in other samples as well.

Thalassiosira insigna-Thalassiosira vulnifica Concurrent Range Zone

Author: Harwood and Maruyama (1992)
Definition of top: LO of Thalassiosira insigna
Definition of base: LO of Thalassiosira vulnifica
Age: 2.6-3.23 Ma
Discussion and remarks: The LO of T. vulnifica was found to occur at all three sites. Another datum within this zone, the LO of Thalassiosira striata, also occurred in Hole 1101A.

Fragilariopsis interfrigidaria Partial Range Zone

Author: McCollum (1975), modified in Weaver and Gombos (1981) and Harwood and Maruyama (1992)
Definition of top: FO of Thalassiosira vulnifica
Definition of base: FO of Fragilariopsis interfrigidaria
Age: 3.23-3.8 Ma
Discussion and remarks: The base of this zone was clearly defined at Sites 1095 and 1096 with the first occurrence of F. interfrigidaria. The base of Hole 1101A ended within this zone; F. interfrigidaria was included in the assemblage through the deepest sample. The FO of T. insigna, a datum occurring within this zone, was observed in Hole 1101A. This same species datum also occurred at Site 1096, but not at Site 1095. The FO of Thalassiosira lentiginosa was seen only at Site 1095.

Fragilariopsis barronii Partial Range Zone

Author: Weaver and Gombos (1981), renamed by Gersonde and Burckle (1990)
Definition of top: FO of Fragilariopsis interfrigidaria
Definition of base: FO of Fragilariopsis barronii
Age: 3.8-4.46 Ma
Discussion and remarks: The first occurrence of F. barronii was observed at both Sites 1095 and 1096. Each site also had an additional datum from within this zone. The FO of Thalassiosira striata was noted at Site 1095 and the LO of Fragilariopsis praeinterfrigidaria at Site 1096.

Thalassiosira inura Partial Range Zone

Author: Gersonde and Burckle (1990)
Definition of top: FO of Fragilariopsis barronii
Definition of base: FO of Thalassiosira inura
Age: 4.46-4.89 Ma
Discussion and remarks: The base of this zone occurs near the bottom of Hole 1096C. The FO datum of T. inura, was observed at both Sites 1095 and 1096. The FO datums of T. fasciculata and T. complicata also occur within this zone at Site 1095.

Thalassiosira oestrupii Partial Range Zone

Author: Baldauf and Barron (1991)
Definition of top: FO of Thalassiosira inura
Definition of base: FO of Thalassiosira oestrupii
Age: 4.89-5.59 Ma
Discussion and remarks: Three datums within this zone were observed at Site 1095: the FOs of T. oestrupii, F. praeinterfrigidaria, and Thalassiosira tetraoestrupii.

Nitzschia reinholdii Partial Range Zone

Author: Harwood and Maruyama (1992), modified in this study
Definition of top: FO of Thalassiosira oestrupii
Definition of base: FO of Thalassiosira oliverana
Age: 5.59-6.42 Ma
Discussion and remarks: The FO of Thalassiosira oliverana was substituted for the FO of Thalassiosira miocenica (the species used in the original zonal definition) (Harwood and Maruyama, 1992). The stratigraphic age of this boundary is not compromised with this substitution, as their previously observed ages are very close. Even though this change was made to facilitate zonal determination, the FO of T. oliverana was not observed at Site 1095. The LO of A. ingens var. ovalis was observed in this zone in Hole 1095B, which is well constrained above and below by several paleomagnetic reversals.

Actinocyclus ingens var. ovalis Partial Range Zone

Author: Harwood and Maruyama (1992)
Definition of top: FO of Thalassiosira oliverana
Definition of base: FO of Actinocyclus ingens var. ovalis
Age: 6.42-8.68
Discussion and remarks: The FO of A. ingens var. ovalis marks the base of this zone and occurs in Hole 1095B, bounded by paleomagnetic reversals that are interpreted with the ages of 6.57 and 6.94 Ma. The LO of Thalassiosira mahoodii occurs upcore from A. ingens var. ovalis, and is also well constrained with paleomagnetic ages.

Thalassiosira torokina Partial Range Zone

Author: Baldauf and Barron (1991), modified in Harwood and Maruyama (1992)
Definition of top: FO of Actinocyclus ingens var. ovalis
Definition of base: FO of Thalassiosira torokina
Age: 8.68-8.97 Ma
Discussion and remarks: This zone is the lowermost one in Hole 1095B. There are three diatom datums and three paleomagnetic reversals within this zone. The diatom datums, in order of increasing age, are the FO of T. mahoodii, the LO of Denticulopsis crassa, and the FO of T. torokina.

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