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Allen, Carl P; Warnke, Detlef A (1991): (Table 5) Age model of ODP Site 114-701 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.735003, In supplement to: Allen, CP; Warnke, DA (1991): History of ice rafting at leg 114 sites, Subantarctic/South Atlantic. In: Ciesielski, PF; Kristoffersen, Y; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 114, 599-607, https://doi.org/10.2973/odp.proc.sr.114.118.1991

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Project(s):
Coverage:
Median Latitude: -52.485000 * Median Longitude: -23.212000 * South-bound Latitude: -52.985000 * West-bound Longitude: -23.212300 * North-bound Latitude: -51.985000 * East-bound Longitude: -23.211700
Date/Time Start: 1987-04-04T14:35:00 * Date/Time End: 1987-04-10T21:15:00
Minimum DEPTH, sediment/rock: 17.02 m * Maximum DEPTH, sediment/rock: 234.18 m
Event(s):
114-701A  * Latitude: -51.985000 * Longitude: -23.212300 * Date/Time Start: 1987-04-04T14:35:00 * Date/Time End: 1987-04-06T06:29:00 * Elevation: -4647.0 m * Penetration: 74.8 m * Recovery: 69.66 m * Location: South Atlantic Ocean * Campaign: Leg114 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 74.8 m cored; 0 m drilled; 93.1 % recovery
114-701C  * Latitude: -52.985000 * Longitude: -23.211700 * Date/Time Start: 1987-04-08T01:30:00 * Date/Time End: 1987-04-10T21:15:00 * Elevation: -4647.0 m * Penetration: 481.4 m * Recovery: 331.06 m * Location: South Atlantic Ocean * Campaign: Leg114 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 51 core; 481.3 m cored; 0 m drilled; 68.8 % recovery
Comment:
Hole 701A has not been studied in sufficient detail to determine depths of unconformities, which are therefore inferred using data from Hole 114-701C. There may be some difference, as the Brunhes/Matuyama boundary is shallower in Hole 114-701A (17.02 vs. 23.00 mbsf) and the Matuyama/Gauss boundary is deeper (68.73 vs. 66.70 mbsf), which may alter the ice-rafted debris data near hiatuses. The hiatus at 71.40 mbsf is inferred as the midpoint between bracketing datums 71.63 and 71.17 mbsf in Hole 114-701C. The hiatus at 174.27 mbsf is inferred as the midpoint between bracketing samples from 178.30 and 170.23 mbsf (P. F. Ciesielski, pers. comm., 1990). Repeated entries in DEPTH signify hiatuses.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
DEPTH, sediment/rockDepth sedmGeocode
Age modelAge modelkaAllen, Carl P
Ageprofile Datum DescriptionAgeprof dat desAllen, Carl PFAD = first appearance datum, LAD = last appearance datum, LAAD = last abundant appearance datum
Size:
56 data points

Data

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Event

Depth sed [m]

Age model [ka]

Ageprof dat des
114-701A 17.02730Brunhes/Matuyama
114-701A31.50910Top Jaramillo (as recognized in Hole 701C)
114-701A32.501200Top Actinocyclus ingens acme (as recognized in Hole 701C)
114-701A37.001450Base Actinocyclus ingens acme (as recognized in Hole 701C)
114-701A44.931660Top Olduvai
114-701A50.951880Base Olduvai
114-701A68.732470Matuyama/Gauss
114-701A71.402630LAAD (>10%) Nitzschia weaveri (top acme 2)
114-701A71.403110Last consistent Nitzschia interfrigidaria (s. str.)
114-701C 74.483400Gauss/Gilbert
114-701C99.054100Top Nunivak
114-701C102.974240Base Nunivak (based on Hole 701B)
114-701C106.834400Top Sidufjall (based on Hole 701B)
114-701C110.594470Base Sidufjall (based on Hole 701B)
114-701C113.994570Top Thvera (based on Hole 701B)
114-701C116.104770Base Thvera
114-701C140.275680C3AN.61
114-701C144.205890C3AN/C3AR
114-701C165.546360FAD Cosmiodiscus insignis v. triangulata
114-701C174.276550Age above hiatus based on sedimentation between 114.20 and 165.54 mbsf extrapolated to hiatus depth
114-701C174.277600Age of hiatus based on sedimentation rate between 7.90 and 8.21 Ma extrapolated to hiatus depth
114-701C179.077900C4R/C4AN
114-701C183.988210C4AN.52
114-701C188.248410C4AN.50
114-701C194.768500C4AN/C4AR
114-701C204.028920C4AR/C5N
114-701C228.4010060C5N/C5R
114-701C234.1811360LAD Cyrtocapsella tetrapera