Biosiliceous sedimentation at ODP Site 128-798


Autoria(s): Dunbar, Robert B; deMenocal, Peter B; Burckle, Lloyd H
Cobertura

MEDIAN LATITUDE: 37.038424 * MEDIAN LONGITUDE: 134.799700 * SOUTH-BOUND LATITUDE: 37.038300 * WEST-BOUND LONGITUDE: 134.799600 * NORTH-BOUND LATITUDE: 37.038500 * EAST-BOUND LONGITUDE: 134.799800 * DATE/TIME START: 1989-08-27T00:00:00 * DATE/TIME END: 1989-08-31T23:40:00

Data(s)

22/02/1992

Resumo

Upper Pliocene through Holocene sediments recovered at Site 798 in the Japan Sea (Oki Ridge) exhibit rhythmic variation in weight percent biogenic opal at intervals of ~5 m and periods equivalent to the 41-k.y. obliquity cycle. Variance at 17 and 100 k.y. is observed prior to 1.3 Ma. These cycles are also clearly defined by log data and correspond to clusters of decimeter-scale dark-colored sediment units alternating with clusters of light-colored units. Opal content varies between 3% and 22% between 0 and 1.3 Ma and from 3% to 43% between 1.3 and 2.6 Ma. Long-term opal accumulation rates average 1.8 g/cm**2/k.y. in the late Pliocene/early Pleistocene and decrease by about 60% at ~1.3 Ma. Rough calculations suggest that opal accumulation rates increased and terrigenous flux decreased during the Holocene relative to the last glacial period. Our age control is not yet sufficient to allow a similar analysis of the 41-k.y. cyclicity in opal content throughout the Pleistocene. Stable isotope results from planktonic foraminifers confirm previous suggestions of a strong surface-water freshening event during isotope stage 2; however, this episode appears to be unique during the Pleistocene. Benthic foraminifers are depleted in 18O during parts of glacial stages 2 and 6 relative to adjacent interglacials, suggesting unusual warming and/or freshening of deep waters. Collectively, the stable isotope and %opal data are consistent with continuing isolation of the Japan Sea during the Quaternary with important transitions occurring at 1.3, 0.7 to 1.0, and 0.2 to 0.3 Ma. Complex relationships among the stable isotope results, %opal data, and sediment characteristics such as color and organic and inorganic carbon content preclude development of a simple model to explain cyclical sedimentation. Opal maxima occur within both light and dark intervals and the processes that control surface-water productivity are at times decoupled from the factors that regulate deep-water dysaerobia. We suggest that water column overturn is controlled largely by regional atmospheric circulation that must also have an as yet poorly understood effect on surface-water fertility.

Formato

application/zip, 3 datasets

Identificador

https://doi.pangaea.de/10.1594/PANGAEA.776503

doi:10.1594/PANGAEA.776503

Idioma(s)

en

Publicador

PANGAEA

Direitos

CC-BY: Creative Commons Attribution 3.0 Unported

Access constraints: unrestricted

Fonte

Supplement to: Dunbar, Robert B; deMenocal, Peter B; Burckle, Lloyd H (1992): Late Pliocene-Quaternary biosiliceous sedimentation at Site 798, Japan Sea. In: Pisciotto, KA; Ingle, JCJr.; von Breymann, MT; Barron, J; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(1), 439-455, doi:10.2973/odp.proc.sr.127128-1.147.1992

Palavras-Chave #128-798; 128-798A; 128-798B; 128-798C; Acc rate opal; Acc rate terr; Accumulation rate, opal; Accumulation rate, sediment, mean; Accumulation rate, terrigeneous; Age, maximum/old; Age, minimum/young; Age max; Age min; Age model; Ageprof dat des; Ageprofile Datum Description; bSiO2; CaCO3; Calcium carbonate; Comment; COMPCORE; Composite Core; DBD; Density, dry bulk; Depth; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Depth bot; Depth top; DRILL; Drilling/drill rig; Event; Japan Sea; Joides Resolution; LAD = last appearance datum; Leg128; MAR; mbsf; Ocean Drilling Program; ODP; OM; Opal, biogenic silica; Organic matter; Rice = Hole 798A (+3.2-m correction); RiceB = Hole 798B (-4 m relative to Hole 798A, i.e., -0.8 m); RiceC = Hole 798C (0-m correction); Burckle Hole 798A (+3.2-m correction); Burckle2 = Hole 798B (-4 m relative to Hole 798A, i.e., -0.8 m); Pete798B = Hole 798B (-4 m relative to Hole 798A, i.e., -0.8 m.; Sedimentation rate; Sed rate
Tipo

Dataset