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Moore, Theodore C (2008): (Table DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.723883, Supplement to: Moore, TC (2008): Biogenic silica and chert in the Pacific Ocean. Geology, 36(12), 975-978, https://doi.org/10.1130/G25057A.1

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Published: 2008 (exact date unknown)DOI registered: 2009-08-10

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Abstract:
Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution and reprecipitation of this silica by hydrothermal waters. As ocean bottom waters flow into and through the crust, they become warmer. Initially they remain less saturated with respect to dissolved silica than pore water in the overlying sediments. With the diffusion of heat, dissolved ions, and to some extent the advection of water itself, biogenic silica in the basal part of the sedimentary section is dissolved. Upon conductively cooling, these pore waters precipitate chert layers. The most common thickness for the basal silica-free zone (20 m) lies below the most common height of the top of the chert interval above basement (50 m). This mode of chert formation explains the frequent occurrence of chert layers at very shallow subbottom depths in pelagic sections of the Pacific. It is also consistent with the common occurrence of cherts </=150 m above basement.
Other version:
Table DR1 - Biogenic Silica and Chert in the Pacific Ocean [dataset]. ftp://rock.geosociety.org/pub/reposit/2008/2008243.pdf
Coverage:
Median Latitude: 7.818637 * Median Longitude: -152.910655 * South-bound Latitude: -63.680700 * West-bound Longitude: 124.650800 * North-bound Latitude: 39.961800 * East-bound Longitude: -69.355800
Date/Time Start: 1969-04-23T00:00:00 * Date/Time End: 2002-11-14T00:00:00
Minimum Elevation: -6100.0 m * Maximum Elevation: -1389.0 m
Event(s):
5-34 * Latitude: 39.470200 * Longitude: -127.275700 * Date/Time: 1969-04-23T00:00:00 * Elevation: -4322.0 m * Penetration: 384 m * Recovery: 102.2 m * Location: North Pacific/PLAIN * Campaign: Leg5 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 17 cores; 126 m cored; 0 m drilled; 81.1 % recovery
7-66 * Latitude: 2.393500 * Longitude: -166.121800 * Date/Time: 1969-09-19T00:00:00 * Elevation: -5310.0 m * Penetration: 193 m * Recovery: 48.8 m * Location: North Pacific/BASIN * Campaign: Leg7 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 11 cores; 72 m cored; 0 m drilled; 67.7 % recovery
15-146 * Latitude: 15.116500 * Longitude: -69.377800 * Date/Time: 1970-12-22T00:00:00 * Elevation: -3949.0 m * Penetration: 762 m * Recovery: 145.3 m * Location: Caribbean Sea/BASIN * Campaign: Leg15 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 43 cores; 370 m cored; 4 m drilled; 39.3 % recovery
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4Elevation of eventElevationm
5Depth, top/minDepth topmMoore, Theodore Cof chert interval
6Layer thicknessThicknessmMoore, Theodore Cthickness of chert interval
7Age, minimum/youngAge minkaMoore, Theodore Ctop of chert interval
8Age, maximum/oldAge maxkaMoore, Theodore Cbase of chert interval
9Depth, bottom/maxDepth botmMoore, Theodore Cbase of silic microfossils, mbsf
10Depth, bottom/maxDepth botmMoore, Theodore Cbasement depth, mbsf
11DifferenceDiffMoore, Theodore Cbasement depth - base of silic microfossils, m
12Age, datedAge datedkaMoore, Theodore Cbasement age
Size:
408 data points

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