Evaluating marine dust records as templates for optical dating of Oldest Ice

The continuous ice core record extends 800,000 years into the past, covering the period of 100,000-year glacial cycles, but not the transition from 40,000-year glacial cycles (the Mid-Pleistocene Transition, 1.2–0.7 million years ago). A primary goal of the International Partnership in Ice Core Scie...

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Main Authors: Ng, Jessica, Severinghaus, Jeffrey, Bay, Ryan, Tosi, Delia
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/egusphere-2023-1342
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1342/
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spelling ftcopernicus:oai:publications.copernicus.org:egusphere112442 2023-09-05T13:13:48+02:00 Evaluating marine dust records as templates for optical dating of Oldest Ice Ng, Jessica Severinghaus, Jeffrey Bay, Ryan Tosi, Delia 2023-08-09 application/pdf https://doi.org/10.5194/egusphere-2023-1342 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1342/ eng eng doi:10.5194/egusphere-2023-1342 https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1342/ eISSN: Text 2023 ftcopernicus https://doi.org/10.5194/egusphere-2023-1342 2023-08-14T16:24:20Z The continuous ice core record extends 800,000 years into the past, covering the period of 100,000-year glacial cycles, but not the transition from 40,000-year glacial cycles (the Mid-Pleistocene Transition, 1.2–0.7 million years ago). A primary goal of the International Partnership in Ice Core Sciences is therefore to retrieve a 1.5-million-year-old continuous ice core, increasing our understanding of this major change in the climate system and thus of fundamental climate forcings and feedbacks. However, complex glacial processes, limited bedrock data, and surprisingly young basal ice in previous cores necessitate careful reconnaissance studies before extracting a full core. Ice borehole optical logging reflects the ice dust content and may be used to date ice quickly and inexpensively if a reference record is known. Here we explore the relationship between ice dust records and well-dated marine dust records from sediment cores in the southern Atlantic and Pacific Oceans, which lie along paths of dust sources to Antarctica. We evaluate how representative these records are of Antarctic dust both through the existing ice core record and during the older target age range, suggesting that a newly published 1.5 million year record from site U1537 near South America is likely the most robust predictor of the Oldest Ice dust signal. We then assess procedures for rapid dating of potential Oldest Ice sites, noting that the ability to detect dating errors is an essential feature. We emphasize that ongoing efforts to identify, recover, date, and interpret an Oldest Ice core should use care to avoid unfounded assumptions about the 40 kyr world based on the 100 kyr world. Text Antarc* Antarctic Antarctica ice core Copernicus Publications: E-Journals Antarctic Pacific
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The continuous ice core record extends 800,000 years into the past, covering the period of 100,000-year glacial cycles, but not the transition from 40,000-year glacial cycles (the Mid-Pleistocene Transition, 1.2–0.7 million years ago). A primary goal of the International Partnership in Ice Core Sciences is therefore to retrieve a 1.5-million-year-old continuous ice core, increasing our understanding of this major change in the climate system and thus of fundamental climate forcings and feedbacks. However, complex glacial processes, limited bedrock data, and surprisingly young basal ice in previous cores necessitate careful reconnaissance studies before extracting a full core. Ice borehole optical logging reflects the ice dust content and may be used to date ice quickly and inexpensively if a reference record is known. Here we explore the relationship between ice dust records and well-dated marine dust records from sediment cores in the southern Atlantic and Pacific Oceans, which lie along paths of dust sources to Antarctica. We evaluate how representative these records are of Antarctic dust both through the existing ice core record and during the older target age range, suggesting that a newly published 1.5 million year record from site U1537 near South America is likely the most robust predictor of the Oldest Ice dust signal. We then assess procedures for rapid dating of potential Oldest Ice sites, noting that the ability to detect dating errors is an essential feature. We emphasize that ongoing efforts to identify, recover, date, and interpret an Oldest Ice core should use care to avoid unfounded assumptions about the 40 kyr world based on the 100 kyr world.
format Text
author Ng, Jessica
Severinghaus, Jeffrey
Bay, Ryan
Tosi, Delia
spellingShingle Ng, Jessica
Severinghaus, Jeffrey
Bay, Ryan
Tosi, Delia
Evaluating marine dust records as templates for optical dating of Oldest Ice
author_facet Ng, Jessica
Severinghaus, Jeffrey
Bay, Ryan
Tosi, Delia
author_sort Ng, Jessica
title Evaluating marine dust records as templates for optical dating of Oldest Ice
title_short Evaluating marine dust records as templates for optical dating of Oldest Ice
title_full Evaluating marine dust records as templates for optical dating of Oldest Ice
title_fullStr Evaluating marine dust records as templates for optical dating of Oldest Ice
title_full_unstemmed Evaluating marine dust records as templates for optical dating of Oldest Ice
title_sort evaluating marine dust records as templates for optical dating of oldest ice
publishDate 2023
url https://doi.org/10.5194/egusphere-2023-1342
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1342/
geographic Antarctic
Pacific
geographic_facet Antarctic
Pacific
genre Antarc*
Antarctic
Antarctica
ice core
genre_facet Antarc*
Antarctic
Antarctica
ice core
op_source eISSN:
op_relation doi:10.5194/egusphere-2023-1342
https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1342/
op_doi https://doi.org/10.5194/egusphere-2023-1342
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