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Dickens, Gerald Roy; Backman, Jan (2013): (Table S3) Nannofossil datums at DSDP Site 86-577. PANGAEA, https://doi.org/10.1594/PANGAEA.809248, 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:
Backman, Jan (1986): Late Paleocene to middle Eocene calcareous nannofossil biochronology from the Shatsky Rise, Walvis Ridge and Italy. Palaeogeography, Palaeoclimatology, Palaeoecology, 57(1), 43-59, https://doi.org/10.1016/0031-0182(86)90005-2
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
Thibault, Nicolas; Gardin, Silvia; Galbrun, Bruno (2010): Latitudinal migration of calcareous nannofossil Micula murus in the Maastrichtian: Implications for global climate change. Geology, 38(3), 203-206, https://doi.org/10.1130/G30326.1
Westerhold, Thomas; Röhl, Ursula; Laskar, Jacques (2012): Time scale controversy: Accurate orbital calibration of early Paleogene. Geochemistry, Geophysics, Geosystems, 13, Q06015, https://doi.org/10.1029/2012GC004096
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
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: 68.91 m * Maximum DEPTH, sediment/rock: 122.94 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]. Placement of nannofossil datums for Upper Cretaceous and Lower Paleogene sediment according to composite depth scale and an updated time scale (Westerhold et al., 2008, 2012).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Event labelEvent
Ageprofile Datum DescriptionAgeprof dat desDickens, Gerald Roy
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 [m]
DEPTH, sediment/rockDepth sedmGeocode
Reference/sourceReferenceDickens, Gerald Roy
OffsetOffsetmDickens, Gerald Roycore offsets from Table 2
Depth, compositeDepth compmcdDickens, Gerald Roynew depth
10 Age modelAge modelkaDickens, 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).
11 CommentCommentDickens, Gerald Roy
Size:
277 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 
Comment
86-577 LCO D. sublodoensis86-577-8-4,60-6186-577-8-4,90-9163.868.91Backman, 1986-2.666.3149500
86-577Top T. orthostylus86-577-8-6,36-3886-577-8-6,46-4863.871.67Backman, 1986-2.669.0750700
86-577Base D. lodoensis86-577-9-4,30-3186-577-9-4,60-6173.378.11Backman, 19860.078.1153240
86-577Top D. multiradiatus86-577-9-4,60-9186-577-9-4,90-9173.378.56Backman, 19860.078.5653240
86-577Top T. contortus86-577-9-5,0-186-577-9-5,30-3173.379.31Backman, 19860.079.3153800
86-577Base S. radians86-577-9-5,30-3186-577-9-5,60-6173.379.61Backman, 19860.079.6153850
86-577Base T. orthostylus86-577-9-5,30-3186-577-9-5,60-6173.379.61Backman, 19860.079.6154000
86-577Base T. contortus86-577-9-5,113-11486-577-9-6,0-173.380.44Backman, 19860.080.4454340
86-577Base D. diastypus86-577-9-5,113-11486-577-9-6,0-173.380.44Backman, 19860.080.4454480
86-577Top Fasciculithus spp.86-577-9-6,120-12186-577-9CC-7,8-973.382.01This study0.082.0155110
86-577Base D. multiradiatus86-577-10-3,60-6186-577-10-3,90-9182.886.41Backman, 19861.587.9156760
86-577Top D. okadai86-577-10-3,30-3186-577-10-3,60-6182.886.11Backman, 19861.587.6156850
86-577Base D. okadai86-577-10-4,30-3186-577-10-4,60-6182.887.61Backman, 19861.589.1156950
86-577Base D. nobilis86-577-10-4,120-12186-577-10-5,0-182.888.51Backman, 19861.590.0156970
86-577Top H. kleinpellii86-577-11-2,60-6186-577-11-2,90-9192.394.41Backman, 1986-1.093.4158330
86-577Com D. mohleri86-577-11-2,100-10186-577-11-2,100-10192.394.81Backman, 1986-1.093.8158550
86-577Base H. kleinpellii86-577-11-3,30-3186-577-11-4,60-6192.395.61Backman, 1986-1.094.6159020
86-577Base Fasciculithus spp.86-577-11-6,140-14186-577-11-6,140-14192.3101.21Backman, 1986-1.0100.2161210
86-577A LCO D. sublodoensisThis study49500Possibly in core gap
86-577ATop T. orthostylus86-577A-8-2,146-14886-577A-8-3,5-766.469.37This study-0.468.9750700
86-577ABase D. lodoensis86-577A-9-2,120-12186-577A-9-3,0-175.978.61This study0.178.7153240
86-577ATop D. multiradiatusThis study53240Likely in missing core interval
86-577ATop T. contortus86-577A-9-3,30-3186-577A-9-3,60-6175.979.21This study0.179.3153800
86-577ABase S. radians86-577A-9-CC,9-10This study53850Likely in missing core interval
86-577ABase T. orthostylus86-577A-9-CC,9-10This study54000Likely in missing core interval
86-577ABase T. contortus86-577A-9-CC,9-10This study54340Likely in missing core interval
86-577ABase D. diastypus86-577A-9-CC,9-10This study54480Likely in missing core interval
86-577ATop Fasciculithus spp.86-577A-9-CC,9-10This study55110Likely in missing core interval
86-577ABase D. multiradiatus86-577A-10-1,78-7985.486.19This study56760Likely above upper sample or in core gap
86-577ATop D. okadai86-577A-10-1,78-7985.486.19This study56850Likely above upper sample or in core gap
86-577ABase D. okadai86-577A-10-2,29-3086-577A-10-2,79-8085.487.20This study1.889.0056950
86-577ABase D. nobilis86-577A-10-2,129-13086-577A-10-3,29-3085.488.20This study1.890.0056970
86-577ATop H. kleinpellii86-577A-10-5,80-8186-577A-11-5,129-13085.492.21This study1.894.0158330
86-577ACom D. mohleri86-577A-10-5,129-13086-577A-10-6,34-3585.492.70This study1.894.5058550
86-577ABase H. kleinpellii86-577A-10-5,129-13086-577A-10-6,34-3585.492.70This study1.894.5059020
86-577ABase Fasciculithus spp.86-577A-11-3,59-6086-577A-11-3,90-9194.998.50This study2.1100.6061210
86-577ABase Sphenolithus86-577A-11-4,120-12186-577A-11-5,1-294.9100.61This study2.1102.7161590
86-577ABase M. murus86-577A-13-7,4-586-577A-13-CC,-94.9122.94Thibault et al.2.1125.0467970