Distribution of diatoms in Oligocene to Pleistocene sediments of the tropical Pacific

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Main Author: Radionova, E P
Format: Dataset Open Access
Language:en
Published: PANGAEA 1991
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author Radionova, E P
author_facet Radionova, E P
collection Datos científicos de ciencias marinas y ambientales
contents According to the drilling probes of the Deep Waier Drilling Project, Neogene sediments in a tropical area of the Pacific Ocean are divided into 15 zones based on diatoms. The author shows that a unique zonation may be applied for the entire region. Identification of diatoms zones boundaries was conducted through their direct correlation with nannoplancton, radiolarian and foraminiferal zonal sceals. Their ultra-structure and morphological relationship are being analysed. The mode of siliceous accumulation within the equatorial belt differed through the western central and eastern region since the early Miocene and the difference become more evident from the end of Middle Miocene. The distribution of Neogene diatomaceous silt in the tropical area is controlled by the character of gyre-water circulation and agrees with the modern geographical zonation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_758425
institution PANGAEA
language en
publishDate 1991
publisher PANGAEA
record_format pangaea
spellingShingle Distribution of diatoms in Oligocene to Pleistocene sediments of the tropical Pacific
Radionova, E P
7-63B; 7-66; 85-575; 86-578; Archive of Ocean Data; ARCOD; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg7; Leg85; Leg86; North Pacific/BASIN; North Pacific/FLANK; North Pacific Ocean
According to the drilling probes of the Deep Waier Drilling Project, Neogene sediments in a tropical area of the Pacific Ocean are divided into 15 zones based on diatoms. The author shows that a unique zonation may be applied for the entire region. Identification of diatoms zones boundaries was conducted through their direct correlation with nannoplancton, radiolarian and foraminiferal zonal sceals. Their ultra-structure and morphological relationship are being analysed. The mode of siliceous accumulation within the equatorial belt differed through the western central and eastern region since the early Miocene and the difference become more evident from the end of Middle Miocene. The distribution of Neogene diatomaceous silt in the tropical area is controlled by the character of gyre-water circulation and agrees with the modern geographical zonation.
title Distribution of diatoms in Oligocene to Pleistocene sediments of the tropical Pacific
topic 7-63B; 7-66; 85-575; 86-578; Archive of Ocean Data; ARCOD; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg7; Leg85; Leg86; North Pacific/BASIN; North Pacific/FLANK; North Pacific Ocean
url https://doi.org/10.1594/PANGAEA.758425