A nutrient effect on the TEX86 paleotemperature proxy
<p>The TEX<sub>86</sub> paleotemperature proxy is widely used to reconstruct ocean surface temperatures over the past 100 million years. However, archaeal culture experiments show that nutrient stress elevates TEX<sub>86</sub> values by increasing glycerol dialkyl glycerol tetraether (GDGT) cyclization. Here, we demonstrate that this ânutrient effectâ is also recorded in sedimentary GDGTs. Using an expanded coreâtop database, we find a significant negative correlation between TEX<sub>86</sub> and nitrate concentrations (Ï = 0.31; P < 0.001) once the thermal effect is removed. There are stronger correlations (Ï 0.73 to 0.91; P < 0.001) in regions with steep nitrate gradients. Comparisons between TEX<sub>86</sub> and UKʹ37 âbased reconstructions from the Arabian Sea and Tasman Sea suggest that nutrient stress influenced GDGT distributions during glacialâinterglacial cycles. Our findings underscore the need to account for nutrient effects when applying TEX86 paleothermometry.</p>
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https://n2t.net/ark:/85065/d7qc07zw
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2016-01-01T00:00:00Z
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2025-06-28T00:00:00Z
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