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Dickens, Gerald Roy; Backman, Jan (2013): (Table S4) Depths and ages of polarity chron boundaries at DSDP Site 86-577 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.809252, In supplement to: Dickens, GR; Backman, J (2013): Core alignment and composite depth scale for the lower Paleogene through uppermost Cretaceous interval at Deep Sea Drilling Project Site 577. Newsletters on Stratigraphy, 46(1), 47-68, https://doi.org/10.1127/0078-0421/2013/0027

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Related to:
Bleil, Ulrich (1985): The magnetostratigraphy of northwest Pacific sediments, Deep Sea Drilling Project Leg 86. In: Heath, GR, Burckle, LH, et al. (eds.), Initial Reports of the Deep Sea Drilling Project, Washington (U.S. Government Print Office), 86, 441-458, https://doi.org/10.2973/dsdp.proc.86.117.1985
Cande, Steven C; Kent, Dennis V (1995): Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic. Journal of Geophysical Research: Solid Earth, 100(B4), 6093-6095, https://doi.org/10.1029/94JB03098
Westerhold, Thomas; Röhl, Ursula; Raffi, Isabella; Fornaciari, Eliana; Monechi, Simonetta; Reale, Viviana; Bowles, Julie; Evans, Helen F (2008): Astronomical calibration of the Paleocene time. Palaeogeography, Palaeoclimatology, Palaeoecology, 257(4), 377-403, https://doi.org/10.1016/j.palaeo.2007.09.016
Westerhold, Thomas; Röhl, Ursula; Wilkens, Roy H; Pälike, Heiko; Lyle, Mitchell W; Dunkley Jones, Tom; Bown, Paul R; Moore, Ted; Kamikuri, Shin-Ichi (2012): Revised composite depth scales and integration of IODP Sites U1331, U1332, U1333, U1334 and ODP Sites 1218, 1219, 1220. Proc. IODP: Tokyo (Integrated Ocean Drilling Program Management International, Inc.), 320/321, https://doi.org/10.2204/iodp.proc.320321.201.2012
Project(s):
Coverage:
Median Latitude: 32.442000 * Median Longitude: 157.723250 * South-bound Latitude: 32.441800 * West-bound Longitude: 157.723200 * North-bound Latitude: 32.442200 * East-bound Longitude: 157.723300
Date/Time Start: 1982-05-23T00:00:00 * Date/Time End: 1982-05-23T00:00:00
Minimum DEPTH, sediment/rock: 67.70 m * Maximum DEPTH, sediment/rock: 121.55 m
Event(s):
86-577  * Latitude: 32.441800 * Longitude: 157.723300 * Date/Time: 1982-05-23T00:00:00 * Elevation: -2675.0 m * Penetration: 118.8 m * Recovery: 111.1 m * Location: North Pacific * Campaign: Leg86 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 118.8 m cored; 0 m drilled; 93.5 % recovery
86-577A  * Latitude: 32.442200 * Longitude: 157.723200 * Date/Time: 1982-05-23T00:00:00 * Elevation: -2675.0 m * Penetration: 123.4 m * Recovery: 110.8 m * Location: North Pacific * Campaign: Leg86 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 13 cores; 123.4 m cored; 0 m drilled; 89.8 % recovery
Comment:
DEPTH, sediment is the old depth [mbsf]. Base C30n below depth of coring in Hole 86-577.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Ageprofile Datum DescriptionAgeprof dat desDickens, Gerald Roypolarity chron boundaries
Sample code/labelSample labelDickens, Gerald RoyDSDP/ODP/IODP sample designationtop
Sample code/label 2Sample label 2Dickens, Gerald RoyDSDP/ODP/IODP sample designationbottom
Depth, top/minDepth topmDickens, Gerald Roycore top [mbsf]
DEPTH, sediment/rockDepth sedmGeocode
Reference/sourceReferenceDickens, Gerald Roy
OffsetOffsetmDickens, Gerald Roy
Depth, compositeDepth compmcdDickens, Gerald Roynew depth
10 Age modelAge modelkaDickens, Gerald Royreported age
11 Age model, optionalAge model optkaDickens, Gerald RoyAge on Option 1 time scale suggested by Westerhold et al. (2008); WO-1 = Westerhold et al. (2008) Option 1. Note these authors do not report ages above the top of Chron C24n.3n or below the top of Chron C30n; ages for polarity chron boundaries beyond are assumed to be the same as reported by Cande and Kent (1995).
12 CommentCommentDickens, Gerald Roy
Size:
362 data points

Data

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


Event

Ageprof dat des

Sample label

Sample label 2

Depth top [m]

Depth sed [m]

Reference

Offset [m]

Depth comp [mcd]
10 
Age model [ka]
11 
Age model opt [ka]
12 
Comment
86-577 Top C22n86-577-8-3,9086-577-8-3,14063.867.70Bleil, 1985-2.6065.105195049000
86-577Base C22n86-577-8-4,9086-577-8-4,14063.869.20Bleil, 1985-2.6066.605262049700
86-577Top C23n.1n5388050800Likely in core gap
86-577Base C23n.1n5403050900Likely in core gap
86-577Top C23n.2n5409051000Likely in core gap
86-577Base C23n.2n5470051700Likely in core gap
86-577Top C24n.1n86-577-9-2,4086-577-9-2,9073.375.20Bleil, 19850.0075.205514052300
86-577Base C24n.1n86-577-9-3,4086-577-9-3,9073.376.70Bleil, 19850.0076.705537052630
86-577Top C24n.2n86-577-9-4,4086-577-9-4,9073.378.20Bleil, 19850.0055660C24n.2n and C24n.3n not distinguished by Bleil (1985)
86-577Base C24n.2n86-577-9-5,4086-577-9-5,9073.379.70Bleil, 19850.0056140C24n.2n and C24n.3n not distinguished by Bleil (1985)
86-577Top C24n.3n86-577-9-4,4086-577-9-4,9073.378.20Revised0.0078.2053030C24n.2n and C24n.3n not distinguished by Bleil (1985)
86-577Base C24n.3n86-577-9-5,4086-577-9-5,9073.379.70Revised0.0079.7053530C24n.2n and C24n.3n not distinguished by Bleil (1985)
86-577Top C25n86-577-10-2,9086-577-10-2,14082.885.20Bleil, 19851.5086.705864056660
86-577Base C25n86-577-10-3,14086-577-10-4,8082.887.20Bleil, 19851.5088.705924057200
86-577Top C26n86-577-10-6,9286-577-10-6,14282.891.22Bleil, 19851.5092.726021058550
86-577Base C26n86-577-10-7,1186-577-11-1,3982.891.91Bleil, 19856075058880This constraint disappears with core overlap (see below)
86-577Top C27n6303061770Likely in core gap
86-577Base C27n6354062100Likely in core gap
86-577Top C28n86-577-12-1,11086-577-12-1,120101.8102.90Bleil, 19852.70105.606429063080
86-577Base C28n86-577-12-3,4086-577-12-3,50101.8105.20Bleil, 19852.70107.906512064030
86-577Top C29n86-577-12-4,1086-577-12-4,20101.8106.40Bleil, 19852.70109.106550064210
86-577Base C29n86-577-12-5,5086-577-12-5,60101.8108.30Bleil, 19852.70111.006617064910
86-577Top C30n86-577-13-1,12086-577-13-1,140111.3112.50Bleil, 19852.65115.156674065630
86-577Base C30nBelow depth of coring in Hole 577*
86-577A Top C22n5195049000Likely in core gap
86-577ABase C22n5262049700Likely in core gap
86-577ATop C23n.1n86-577A-8-2,9086-577A-8-2,14066.468.80Bleil, 1985-0.4068.405388050800
86-577ABase C23n.1n86-577A-8-2,14086-577A-8-3,4066.469.30Bleil, 1985-0.4068.905403050900
86-577ATop C23n.2n86-577A-8-3,4086-577A-8-3,9066.469.80Bleil, 1985-0.4069.405409051000
86-577ABase C23n.2n86-577A-8-4,4086-577A-8-4,9066.471.30Bleil, 1985-0.4070.905470051700
86-577ATop C24n.1n86-577A-8-6,2086-577A-9-1,4166.474.10Bleil, 19855514052300This constraint disappears with core gap
86-577ABase C24n.1n86-577A-9-1,13186-577A-9-2,4475.977.21Bleil, 19850.1077.315537052630
86-577ATop C24n.2n86-577A-9-2,8286-577A-9-2,12575.978.22Bleil, 198555660C24n.2n and C24n.3n not distinguished by Bleil (1985)
86-577ABase C24n.2n56140
86-577ATop C24n.3n86-577A-9-2,8286-577A-9-2,12575.978.22Revised0.1078.3253030
86-577ABase C24n.3n53530Likely in missing core
86-577ATop C25n56660Likely in core gap
86-577ABase C25n57200Likely in core gap
86-577ATop C26n86-577A-10-3,3086-577A-10-3,7185.488.70Bleil, 19851.8090.506021058550
86-577ABase C26n86-577A-10-3,10086-577A-10-4,3185.489.40Bleil, 19851.8091.206075058880
86-577ATop C27n86-577A-11-4,13086-577A-11-5,3094.9100.70Bleil, 19852.10102.806303061770
86-577ABase C27n86-577A-11-5,8086-577A-11-5,13094.9101.70Bleil, 19852.10103.806354062100
86-577ATop C28n86-577A-11-6,7086-577A-11-6,12094.9103.10Bleil, 19852.10105.206429063080
86-577ABase C28n86-577A-12-1,9686-577A-12-1,116104.4105.36Bleil, 19852.20107.566429064030
86-577ATop C29n86-577A-12-2,7686-577A-12-2,94104.4106.66Bleil, 19852.20108.866550064210
86-577ABase C29n86-577A-12-3,11686-577A-12-3,135104.4108.56Bleil, 19852.20110.766617064910
86-577ATop C30n86-577A-12-6,11186-577A-12-6,126104.4113.01Bleil, 19852.20115.216674065630
86-577ABase C30n86-577A-13-5,11986-577A-13-5,137113.9121.09Bleil, 19852.10123.196842067600
86-577ATop C30n86-577A-13-6,1586-577A-13-6,35113.9121.55Bleil, 19852.10123.656852067700