Coupled response of rainfall and denitrification to solar forcing during the Holocene in Alfonso Basin.
The bulk sedimentary δ15N record of Alfonso Basin displayed changes both from a regional source possibly associated with changes in the isotopic signal of NO3– dissolved in Subsurface Subtropical Water and from a climate source governed by solar forcing (total solar irradiance) over the strength of...
Tallennettuna:
| Päätekijät: | , , |
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| Aineistotyyppi: | info:eu-repo/semantics/article |
| Kieli: | eng |
| Julkaistu: |
Iniversidad Autónoma de Baja California
2013
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| Linkit: | https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2224 |
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