Age models for ODP Leg 172 sites

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Hauptverfasser: Gruetzner, Jens, Giosan, Liviu, Franz, Sven-Oliver, Tiedemann, Ralf, Cortijo, Elsa, Chaisson, William P, Flood, Roger D, Hagen, Sveinung, Keigwin, Lloyd D, Poli, Maria-Serena, Rio, Domenico, Williams, Thomas
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Sprache:en
Veröffentlicht: PANGAEA 2002
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author Gruetzner, Jens
Giosan, Liviu
Franz, Sven-Oliver
Tiedemann, Ralf
Cortijo, Elsa
Chaisson, William P
Flood, Roger D
Hagen, Sveinung
Keigwin, Lloyd D
Poli, Maria-Serena
Rio, Domenico
Williams, Thomas
author_facet Gruetzner, Jens
Giosan, Liviu
Franz, Sven-Oliver
Tiedemann, Ralf
Cortijo, Elsa
Chaisson, William P
Flood, Roger D
Hagen, Sveinung
Keigwin, Lloyd D
Poli, Maria-Serena
Rio, Domenico
Williams, Thomas
collection Datos científicos de ciencias marinas y ambientales
contents Ten ODP sites drilled in a depth transect (2164-4775 m water depth) during Leg 172 recovered high-deposition rate (>20 cm/kyr) sedimentary sections from sediment drifts in the western North Atlantic. For each site an age model covering the past 0.8-0.9 Ma has been developed. The time scales have a resolution of 10-20 kyr and are derived by tuning variations of estimated carbonate content to the orbital parameters precession and obliquity. Based on the similarity in the signature of proxy records and the spectral character of the time series, the sites are divided into two groups: precession cycles are better developed in carbonate records from a group of shallow sites (2164-2975 m water depth, Sites 1055-1058) while the deeper sites (2995-4775 m water depth, Sites 1060-1063) are characterized by higher spectral density in the obliquity band. The resulting time scales show excellent coherence with other dated carbonate and isotope records from low latitudes. Besides the typical Milankovitch cyclicity significant variance of the resulting carbonate time series is concentrated at millennial-scale changes with periods of about 12, 6, 4, 2.5, and 1.5 kyr. Comparisons of carbonate records from the Blake Bahama Outer Ridge and the Bermuda Rise reveal a remarkable similarity in the time and frequency domain indicating a basin-wide uniform sedimentation pattern during the last 0.9 Ma.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_742089
institution PANGAEA
language en
publishDate 2002
publisher PANGAEA
record_format pangaea
spellingShingle Age models for ODP Leg 172 sites
Gruetzner, Jens
Giosan, Liviu
Franz, Sven-Oliver
Tiedemann, Ralf
Cortijo, Elsa
Chaisson, William P
Flood, Roger D
Hagen, Sveinung
Keigwin, Lloyd D
Poli, Maria-Serena
Rio, Domenico
Williams, Thomas
172-1055; 172-1056; 172-1057; 172-1058; 172-1059; 172-1060; 172-1061; 172-1062; 172-1063; Blake-Bahama Outer Ridge, North Atlantic Ocean; Blake Outer Ridge, North Atlantic Ocean; Carolina Slope, North Atlantic Ocean; COMPCORE; Composite Core; Joides Resolution; Leg172; Ocean Drilling Program; ODP
Ten ODP sites drilled in a depth transect (2164-4775 m water depth) during Leg 172 recovered high-deposition rate (>20 cm/kyr) sedimentary sections from sediment drifts in the western North Atlantic. For each site an age model covering the past 0.8-0.9 Ma has been developed. The time scales have a resolution of 10-20 kyr and are derived by tuning variations of estimated carbonate content to the orbital parameters precession and obliquity. Based on the similarity in the signature of proxy records and the spectral character of the time series, the sites are divided into two groups: precession cycles are better developed in carbonate records from a group of shallow sites (2164-2975 m water depth, Sites 1055-1058) while the deeper sites (2995-4775 m water depth, Sites 1060-1063) are characterized by higher spectral density in the obliquity band. The resulting time scales show excellent coherence with other dated carbonate and isotope records from low latitudes. Besides the typical Milankovitch cyclicity significant variance of the resulting carbonate time series is concentrated at millennial-scale changes with periods of about 12, 6, 4, 2.5, and 1.5 kyr. Comparisons of carbonate records from the Blake Bahama Outer Ridge and the Bermuda Rise reveal a remarkable similarity in the time and frequency domain indicating a basin-wide uniform sedimentation pattern during the last 0.9 Ma.
title Age models for ODP Leg 172 sites
topic 172-1055; 172-1056; 172-1057; 172-1058; 172-1059; 172-1060; 172-1061; 172-1062; 172-1063; Blake-Bahama Outer Ridge, North Atlantic Ocean; Blake Outer Ridge, North Atlantic Ocean; Carolina Slope, North Atlantic Ocean; COMPCORE; Composite Core; Joides Resolution; Leg172; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.742089