(Table T1) Strontium isotopic composition and ages of limestone samples from ODP Hole 180-1118A

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Main Authors: Allan, Tony, Robertson, Alastair H F, Sharp, Timothy R, Trotter, Julie
Format: Dataset Open Access
Language:en
Published: PANGAEA 2001
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author Allan, Tony
Robertson, Alastair H F
Sharp, Timothy R
Trotter, Julie
author_facet Allan, Tony
Robertson, Alastair H F
Sharp, Timothy R
Trotter, Julie
collection Datos científicos de ciencias marinas y ambientales
contents Limestone from Unit VI (857.1-859.15 meters below seafloor) collected at Site 1118 contains a planktonic foraminiferal fauna indicating a latest Miocene to early Pliocene age. Globorotalia tumida is recorded in Sample 180-1118A-68R-4, 46-48 cm, indicating an early Pliocene (N18) age at this level (J. Resig, pers. comm., 2000). Based on their known range in the western Papuan Basin, the presence of (rare) Lepidocyclina and common Amphistegina in some samples suggests that abundant shallow-water bioclastic debris present in these limestones may be reworked from older, possibly middle or early late Miocene sediments. Four samples were selected for whole-rock strontium isotopic analysis to further investigate this possibility. A petrographic examination of samples analyzed was also conducted.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_787037
institution PANGAEA
language en
publishDate 2001
publisher PANGAEA
record_format pangaea
spellingShingle (Table T1) Strontium isotopic composition and ages of limestone samples from ODP Hole 180-1118A
Allan, Tony
Robertson, Alastair H F
Sharp, Timothy R
Trotter, Julie
180-1118A; Age, dated; Age, strontium isotope, Oslick et al. (1994); DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
Limestone from Unit VI (857.1-859.15 meters below seafloor) collected at Site 1118 contains a planktonic foraminiferal fauna indicating a latest Miocene to early Pliocene age. Globorotalia tumida is recorded in Sample 180-1118A-68R-4, 46-48 cm, indicating an early Pliocene (N18) age at this level (J. Resig, pers. comm., 2000). Based on their known range in the western Papuan Basin, the presence of (rare) Lepidocyclina and common Amphistegina in some samples suggests that abundant shallow-water bioclastic debris present in these limestones may be reworked from older, possibly middle or early late Miocene sediments. Four samples were selected for whole-rock strontium isotopic analysis to further investigate this possibility. A petrographic examination of samples analyzed was also conducted.
title (Table T1) Strontium isotopic composition and ages of limestone samples from ODP Hole 180-1118A
topic 180-1118A; Age, dated; Age, strontium isotope, Oslick et al. (1994); DEPTH, sediment/rock; DRILL; Drilling/drill rig; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Strontium-87/Strontium-86 ratio; Strontium-87/Strontium-86 ratio, error
url https://doi.org/10.1594/PANGAEA.787037