Long Term Variability in the Structure of Kelp Communities in Northern Chile and the 1997–98 ENSO
By J. Vásquez, J. Vega, A. Buschmann. Journal of Applied Phycology, 2006
89 citations recorded by the source corpus.
Subfields: Ecology, Oceanography
View Paper: https://www.semanticscholar.org/paper/cd56ea4f086261d13cdf08ba74b2b1f8eca43429
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Citations in the corpus
- Sea urchin barrens as alternative stable states of collapsed kelp ecosystems (2014, unknown): “Conversely, in an 8 yr study of a kelp forest (Macrocystis integrifolia and Lessonia trabeculata) in northern Chile, Vásquez et al. (2006) documented a 3-fold increase in re - cruitment of sea urchins Tetrapygus niger and a sharp decline of kelp cover during a La Niña event in 1999.”
- Production and fate of kelp detritus (2012, unknown): “Large-scale kelp canopy loss is linked to warm water temperatures associated with the disruption of upwelling cycles during El Niño years (Gunnill 1985, Steneck et al. 2002, Martinez et al. 2003, Vasquez et al. 2006, Foster & Schiel 2010, Springer et al. 2010).”
- Stability, resilience, and phase shifts in rocky subtidal communities along the west coast of Vancouver Island, Canada (2011, background): “3 E-mail: Jane.Watson@viu.ca 215 facilitate disease outbreaks in grazers (Pearse and Hines 1979, Scheibling et al. 1999) or kill kelps outright (Vasquez et al. 2006), by longer term temperature changes (Dayton et al. 1992, Sutherland 1998), and by biotic factors such as grazing by sea urchins…”
- Genetic structure of the giant kelp Macrocystis pyrifera along the southeastern Pacific (2010, unknown): “Events such as the El Niño Southern Oscillation (ENSO) produce massive mortality of kelp in the Peruvian province and the northern part of the Intermediate area (Vega et al. 2005, Vasquez et al. 2006, Thiel et al. 2007).”
- Production, use and fate of Chilean brown seaweeds: re-sources for a sustainable fishery (2008, unknown): “Lessonia trabeculata: distribution and abundance of this species was evaluated using 160-m transects, perpendicular to the coastline and located between the intertidal zone and 20-m depth, according the methodology described by Vásquez et al. (2006).”