Regional Fluctuations in the Eastern Tropical North Pacific Oxygen Minimum Zone during the Late Holocene

This study presents a high-resolution record of δ 15 N sed , which serves as a proxy for water column denitrification and oxygen minimum zone (OMZ) intensity, from the Soledad Basin in the Eastern Tropical North Pacific OMZ. The Soledad Basin δ 15 N sed record is compared to the Pescadero Slope and...

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Bibliographic Details
Published in:Oceans
Main Authors: Caitlin E. Tems, Eric Tappa
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2024
Subjects:
Eastern Tropical North Pacific oxygen minimum zone
nitrogen isotopes
late Holocene climate
North American monsoon
paleoceanography
Oceanography
GC1-1581
Subarctic
Online Access:https://doi.org/10.3390/oceans5020021
https://doaj.org/article/16290cff4c0544248ba18d19ca264267
Description
Summary:This study presents a high-resolution record of δ 15 N sed , which serves as a proxy for water column denitrification and oxygen minimum zone (OMZ) intensity, from the Soledad Basin in the Eastern Tropical North Pacific OMZ. The Soledad Basin δ 15 N sed record is compared to the Pescadero Slope and Santa Barbara Basin (SBB) δ 15 N sed records to gain insight into regional variations in the ETNP OMZ. During the Medieval Climate Anomaly (MCA; 950–1250 CE), Soledad Basin, Pescadero Slope, and SBB records exhibit coherent trends suggesting that there was general water column oxygenation stability. During the Little Ice Age (LIA; 1350–1850 CE), Soledad Basin and SBB showed a similar decreasing trend in δ 15 N sed values while the Pescadero Slope δ 15 N sed exhibited an increasing trend until values abruptly declined between 1740 and 1840 CE. We suggest that increased δ 15 N sed variability and the different trends at the Pescadero Slope during the LIA are due to the influence of the North American monsoon (NAM), which can suppress upwelling when enhanced and result in OMZ contraction. The decoupling between the Soledad Basin, SBB, and the Pescadero Slope could also be due to the increased influence of enriched 15 NO 3 − subarctic waters in the California Current System. Since each site is influenced by local productivity, basin morphology, and regional atmospheric and ocean circulation patterns, we suggest that assessing OMZ fluctuations from multiple sites provides a more comprehensive view of regional OMZ dynamics in response to climate variations.

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