persistent millennial-scale link between greenland climate and northern pacific oxygen minimum zone under interglacial conditions
Clicks: 184
ID: 183279
2014
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Steady Performance
30.0
/100
184 views
41 readers
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #40 of 96 articles by views in proceedings - 16th ieee/acis international conference on computer and information science, icis 2017
Most read
Least read
Bar heights use a square-root scale.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
The intensity and/or extent of the northeastern Pacific Oxygen Minimum Zone
(OMZ) varied in-phase with the Northern Hemisphere high latitude climate on
millennial timescales during the last glacial period, indicating the
occurrence of atmospheric and oceanic connections under glacial conditions.
While millennial variability was reported for both the Greenland and the
northern Atlantic Ocean during the last interglacial period, the climatic
connections with the northeastern Pacific OMZ has not yet been observed
under warm interglacial conditions. Here we present a new geochemical
dataset, spanning the past 120 ka, for major components (terrigenous
fraction, marine organic matter, biogenic opal, and carbonates) generated by
X-ray fluorescence scanning alongside with biological productivity and redox
sensitive trace element content (Mo, Ni, Cd) of sediment core MD02-2508 at
23° N, retrieved from the northern limit of the modern OMZ.
Based on elemental ratios Si / Ti (proxy for opal), Cd / Al and Ni / Al, we
suggest that biological productivity was high during the last interglacial
(MIS5). Highly resolved opal reconstruction presents millennial variability
corresponding to all the Dansgaard-Oeschger interstadial events over the
last interglacial, while the Mo / Al ratio indicates reduced oxygenation
during these events. Extremely high opal content during warm interstadials
suggests high diatom productivity. Despite the different climatic and
oceanic background between glacial and interglacial periods, rapid
variability in the northeastern Pacific OMZ seems to be tightly related to
Northern Hemisphere high latitude climate via atmospheric and possibly
oceanic processes.
| Reference Key |
cartapanis2014climatepersistent
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;O. Cartapanis;K. Tachikawa;O. E. Romero;E. Bard |
| Journal | proceedings - 16th ieee/acis international conference on computer and information science, icis 2017 |
| Year | 2014 |
| DOI |
10.5194/cp-10-405-2014
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.