Article (Scientific journals)
Spatially contrasted response of Devonian anoxia to astronomical forcing
Gérard, Justin; Pohl, Alexandre; Sablon, Loïc et al.
2026In Climate of the Past, 22 (5), p. 1003-1021
Peer Reviewed verified by ORBi
 

Files


Full Text
110.2026 - Gérard_et_al_2026_SpatiallyContrastedDevonianAnoxia.pdf
Publisher postprint (6.35 MB) Creative Commons License - Attribution
Download

All documents in ORBi are protected by a user license.

Send to



Details



Abstract :
[en] Abstract. The Devonian period, spanning from 419 to 359 million years ago, was marked by a warmer-than-present climate and recurring ocean anoxic events, with evidence increasingly suggesting a link between these events and astronomical forcing. Here, we explore how astronomical forcing influences ocean oxygenation by modulating the continental weathering flux of phosphate within a Late Devonian climate framework. To investigate this, we performed transient simulations spanning 1.1 Myr, crossing a 2.4 Myr eccentricity node using the cGENIE Earth system model. These simulations were driven by spatially resolved fluxes of reactive phosphorus from continents, computed using the emulator developed by Sablon et al. (2025), trained on GEOCLIM and HadSM3 outputs. Our results provide new evidence supporting eccentricity maxima as a driver of Late Devonian anoxic events. Additionally, global analysis reveals that obliquity variations can leave an imprint on global ocean oxygen levels via their influence on biological productivity, suggesting a potential pathway for obliquity-driven anoxia under greenhouse conditions. Regional analysis revealed pronounced spatial heterogeneity in the biogeochemical response to astronomical forcing. Local ocean circulation emerged as a critical factor in shaping these patterns. The simulations indicate that astronomical forcing can, through its impact on continental weathering fluxes, exert a dominant influence on ocean oxygenation, with regional oxygen concentrations varying by up to 35 % and driving changes in regional anoxic volume of up to 19 %. Finally, these findings help explain why proxy records from different locations may show divergent expressions of astronomical signals, potentially leading to contrasting interpretations of their role in driving ocean anoxia.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Gérard, Justin 
Pohl, Alexandre 
Sablon, Loïc 
Huygh, Jarno  ;  Université de Liège - ULiège > Geology
Da Silva, Anne-Christine  ;  Université de Liège - ULiège > Département de géologie
Crucifix, Michel  ;  Université de Liège - ULiège > Département de géologie > Argiles, géochimie et environnements sédimentaires
Language :
English
Title :
Spatially contrasted response of Devonian anoxia to astronomical forcing
Publication date :
13 May 2026
Journal title :
Climate of the Past
ISSN :
1814-9324
eISSN :
1814-9332
Publisher :
Copernicus GmbH
Volume :
22
Issue :
5
Pages :
1003-1021
Peer reviewed :
Peer Reviewed verified by ORBi
Funders :
F.R.S.-FNRS - Fonds de la Recherche Scientifique
NSCF - National Natural Science Foundation of China
Available on ORBi :
since 22 May 2026

Statistics


Number of views
13 (1 by ULiège)
Number of downloads
8 (0 by ULiège)

Scopus citations®
 
0
Scopus citations®
without self-citations
0
OpenAlex citations
 
0

Bibliography


Similar publications



Contact ORBi