Composition, biomass and potential grazing impact of the crustacean and pelagic tunicates in the northern Humboldt Current area off Chile: differences between El Nino and non- El Nino years

By H. González, M. Sobarzo, D. Figueroa, E. Nöthig. 2000

88 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/4524caf12b694517cc5726e0a0c14c56882dd484

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. A. Calbet
2. H. González
3. Erasmo C. Macaya
4. W. Arntz
5. E. Acuña
6. J. Gili
7. M. Sobarzo
8. M. Thiel

In Oceanography

1. A. Calbet
2. W. Arntz
3. Erasmo C. Macaya
4. J. Gili
5. H. González
6. E. Acuña
7. M. Sobarzo
8. M. Thiel

Citations in the corpus

• The role of faecal material in the particulate organic carbon flux in the northern Humboldt Current, Chile (23°S), before and during the 1997–1998 El Niño (2000, methodology): “This might be due to (i) a strong seasonal signal with lower productivity in winter than summer (González et al., 1999) and (ii) the presence, during January 1998, of a restricted coastal area located near the mouth of large embayments, such as Mejillones Bay, where phytoplankton abundances and…”
• The humboldt current system of northern and central chile : Oceanographic processes, ecological interactions and socioeconomic feedback (2007, background): “This production also constitutes an important way of sequestering CO2 and supports a high rate of particulate organic matter (POM) exported to depth (González et al. 2000a, Pantoja et al. 2004).”
• Gelatinous zooplankton assemblages associated with water masses in the Humboldt Current System, and potential predatory impact by Bassia bassensis (Siphonophora: Calycophorae) (2001, methodology): “Values of individual carbon content for cyclopoid copepods in the length range 0.7 to 1.2 mm (3.5 µg C ind.–1) and small calanoids in the 0.8 to 1.5 mm length range (17.8 µg C ind.–1) (González et al. 2000) were used to calculate the total copepod biomass per station (Table 2).”
• Plankton community structure and carbon cycling in a coastal upwelling system. I: Bacteria, microprotozoans and phytoplankton in the diet of copepods and appendicularians (2004, background): “Gayana Oceanol 6:11–23 Grünewald AC, Morales CE, González HE, Sylvester S, Castro LR (2002) Grazing impact of copepod assemblages and gravitational flux in coastal and oceanic waters off central Chile during two contrasting seasons.”
• The trophic roles of microzooplankton in marine systems (2008, background): “The modest average contribution of mesozooplankton to total community grazing in upwellings and very productive systems, even if variable (Dagg and Turner, 1982; Dubischar and Bathman, 1997; Barquero et al., 1998; González et al., 2000), diverges from the traditional view of these ecosystems, which ”
• The relative importance of microbial and classical food webs in a highly productive coastal upwelling area (2007, methodology): “In the Peruvian and Chilean coastal upwelling systems, which are among the most productive coastal areas worldwide (4 to 20 g C m22 d21, Daneri et al. 2000), the upwelling of deep waters having relatively high CO2 content, low temperature, low oxygen concentration, and high concentration of nutrient”