Stable isotope paleoenvironmental record of a coral from Cabo Pulmo, entrance to the Gulf of california, mexico
A 17-year-long record of δ18O and δ13C from a Cabo Pulmo coral (Pavona gigantea) was analyzed. Although the coral δ18O signal is mainly temperature controlled (~70%), the seasonal arrival of surface water masses to the Gulf of California produces an isotopic effect in the opposite direction to that...
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Autores principales: | , |
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Formato: | Online |
Lenguaje: | eng |
Publicado: |
Iniversidad Autónoma de Baja California
2001
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Acceso en línea: | https://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/469 |
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