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Data · dataset · 2026

A nutrient effect on the TEX86 paleotemperature proxy

Listed in National Center for Atmospheric Research

The TEX 86 paleotemperature proxy is widely used to reconstruct ocean surface temperatures over the past 100 million years.

Description

However, archaeal culture experiments show that nutrient stress elevates TEX 86 values by increasing glycerol dialkyl glycerol tetraether (GDGT) cyclization. Here, we demonstrate that this “nutrient effect” is also recorded in sedimentary GDGTs.

Using an expanded core‐top database, we find a significant negative correlation between TEX 86 and nitrate concentrations (ρ = 0.31; P < 0.001) once the thermal effect is removed. There are stronger correlations (ρ 0.73 to 0.91; P < 0.001) in regions with steep nitrate gradients. Comparisons between TEX 86 and UKʹ37 ‐based reconstructions from the Arabian Sea and Tasman Sea suggest that nutrient stress influenced GDGT distributions during glacial‐interglacial cycles.

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Our findings underscore the need to account for nutrient effects when applying TEX86 paleothermometry.

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Provenance · 1 source records, 7 field assertions
SourceKeyLast seenRaw
National Center for Atmospheric Researchc553e924-1808-462d-a0df-ec674e59396912 d agoJSON v1
FieldAssertionExtractorEvidence
concepts[field].local:field:earth-environmentalmapping · data ucar educonnector:data_ucar_edu@1.0.0
concepts[field].local:field:ocean-atmosphericmapping · data ucar educonnector:data_ucar_edu@1.0.0
created_datesource · data ucar educonnector:data_ucar_edu@1.0.0
descriptionsource · data ucar educonnector:data_ucar_edu@1.0.0/notes
publication_datesource · data ucar educonnector:data_ucar_edu@1.0.0
titlesource · data ucar educonnector:data_ucar_edu@1.0.0/title
updated_datesource · data ucar educonnector:data_ucar_edu@1.0.0