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GlobSed: Updated total sediment thickness in the World’s oceans

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TLDR
In this article, a new global 5 arc-minute total sediment thickness grid for the world's oceans and marginal seas is presented, GlobSed, which provides a much needed update of the sediment thickness distribution of the world oceans and delivers a model for sedimentation rates on oceanic crust through time that agrees well with selected drill data used for comparison.
Abstract
We present GlobSed, a new global 5‐arc‐minute total sediment thickness grid for the world's oceans and marginal seas. GlobSed covers a larger area than previously published global grids and incorporates updates for the NE Atlantic, Arctic, Southern Ocean, and Mediterranean regions, which results in a 29.7% increase in estimated total oceanic sediment volume. We use this new global grid and a revised global oceanic lithospheric age grid to assess the relationship between the total sediment thickness and age of the underlying oceanic lithosphere and its latitude. An analytical approximation model is used to mathematically describe sedimentation trends in major oceanic basins and to allow paleobathymetric reconstructions at any given geological time. This study provides a much‐needed update of the sediment thickness distribution of the world oceans and delivers a model for sedimentation rates on oceanic crust through time that agrees well with selected drill data used for comparison.

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Journal ArticleDOI

A Global Data Set of Present-Day Oceanic Crustal Age and Seafloor Spreading Parameters

TL;DR: In this paper, an updated oceanic crustal age grid and a set of complementary grids including spreading rate, asymmetry, direction, and obliquity are presented. But they do not consider the distribution of spreading modes based on area of preserved crust.
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Reconstructions of Antarctic topography since the Eocene–Oligocene boundary.

TL;DR: In this article, a series of processes including ice sheet loading, volcanism, thermal subsidence, horizontal plate motion, erosion, sedimentation and flexural isostatic adjustment are considered.
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Global Cenozoic Paleobathymetry with a focus on the Northern Hemisphere Oceanic Gateways

TL;DR: In this paper, the authors re-evaluated the evolution of the Northern hemisphere oceanic gateways and embedded their tectonic histories in a new global paleobathymetry and topography model for the Cenozoic time.
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The evolving paleobathymetry of the circum-Antarctic Southern Ocean since 34 Ma – A key to understanding past cryosphere-ocean developments

TL;DR: In this paper, the authors used more than 40 years of seismic reflection data acquisition along the margins of Antarctica and its conjugate margins, along with multiple drilling campaigns by the International Ocean Discovery Program (IODP) and its predecessor programs to calculate oceanwide paleobathymetry grids via a backstripping method.
References
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Journal ArticleDOI

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Journal ArticleDOI

Age, spreading rates, and spreading asymmetry of the world's ocean crust

TL;DR: In this article, the authors present a digital model of the age, spreading rate, and asymmetry at each grid node by linear interpolation between adjacent seafloor isochrons in the direction of spreading.
Journal ArticleDOI

Global continental and ocean basin reconstructions since 200 Ma

TL;DR: In this paper, a new type of global plate motion model consisting of a set of continuously-closing topological plate polygons with associated plate boundaries and plate velocities since the break-up of the supercontinent Pangea is presented.
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