Coupled response of rainfall and denitrification to solar forcing during the Holocene in Alfonso Basin.

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...

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Hlavní autoři: Ricaurte-Villota, Constanza, González-Yajimovich, Oscar, Sanchez, Alberto
Médium: info:eu-repo/semantics/article
Jazyk:eng
Vydáno: Iniversidad Autónoma de Baja California 2013
On-line přístup:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2224
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https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2224

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