2009
DOI: 10.1016/j.marmicro.2009.06.009
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Palynological record (1483–1994) of Gymnodinium catenatum in Pescadero Basin, southern Gulf of California, Mexico

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Cited by 21 publications
(16 citation statements)
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“…There is general agreement that HABs have increased in recent years (Herná ndez-Becerril et al, 2007; Corté s-Altamirano and Sierra-Beltrá n, 2008) and G. catenatumrelated blooms are no exception (Band-Schmidt et al, 2010); however, the increase in G. catenatum blooms along the Mexican Pacific coast does not appear to be related to anthropogenic activities. For example, extensive aquaculture and agriculture activities are present on the east coast of the Gulf of California, but there is no clear evidence that PST-producing blooms have increased due to pollution or nutrient runoff from these activities (Flores-Trujillo et al, 2009). Blooms of G. catenatum in the Gulf of California appear to be related to other environmental forcing factors.…”
Section: Mexicomentioning
confidence: 99%
“…There is general agreement that HABs have increased in recent years (Herná ndez-Becerril et al, 2007; Corté s-Altamirano and Sierra-Beltrá n, 2008) and G. catenatumrelated blooms are no exception (Band-Schmidt et al, 2010); however, the increase in G. catenatum blooms along the Mexican Pacific coast does not appear to be related to anthropogenic activities. For example, extensive aquaculture and agriculture activities are present on the east coast of the Gulf of California, but there is no clear evidence that PST-producing blooms have increased due to pollution or nutrient runoff from these activities (Flores-Trujillo et al, 2009). Blooms of G. catenatum in the Gulf of California appear to be related to other environmental forcing factors.…”
Section: Mexicomentioning
confidence: 99%
“…Oceanographic conditions in the tropical northwestern Pacific respond with different frequency and intensity to the variability of tropical weather events (Barron et al 2003, Goni et al 2006, Barron and Bukry 2007, Flores-Trujillo et al 2009, Staines-Urías et al 2009, Marchitto et al 2010, Pérez-Cruz 2013, Ricaurte-Villota et al 2013. The variability of marine productivity in the northwestern Pacific during the Holocene has been linked to the following: (1) the position of the subtropical high pressure system (e.g., Goni et al 2006, Pérez-Cruz 2013; (2) the relative position of the Intertropical Convergence Zone (ITCZ) and the North American Monsoon (e.g., Goni et al 2006, Staines-Urías et al 2009, Pérez-Cruz 2013, Ricaurte-Villota et al 2013; and (3) solar activity, an exogenous factor responsible for El Niño/La Niña-like atmospheric and oceanographic conditions (e.g., Marchitto et al 2010).…”
Section: Introductionmentioning
confidence: 99%
“…The few existing late-Holocene paleorecords from the tropical northwestern region of Mexico are for Guaymas Basin (Barron et al 2003, Goni et al 2006, Barron and Bukry 2007, Alfonso Basin (Staines-Urías et al 2009, Pérez-Cruz 2013, Ricaurte-Villota et al 2013, and Pescadero Basin (Flores-Trujillo et al 2009, Staines-Urías et al 2009) in the Gulf of California, and for Soledad Basin (Marchitto et al 2010, Deutsch et al 2014 off the west coast of the Baja California peninsula. Changes in marine productivity and water-column conditions have been linked to changes in solar activity during the late Holocene.…”
Section: Introductionmentioning
confidence: 99%
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