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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主要な著者: Ricaurte-Villota, Constanza, González-Yajimovich, Oscar, Sanchez, Alberto
フォーマット: info:eu-repo/semantics/article
言語:eng
出版事項: Iniversidad Autónoma de Baja California 2013
オンライン・アクセス:https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/2224
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