2001
DOI: 10.3354/meps212053
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Short-term variability of photosynthetic parameters and particulate and dissolved primary production in the Alboran Sea (SW Mediterranean)

Abstract: d-1 at Stn C, with dissolved primary production ranging from 4 to 44% of total values. Integrated primary production was significantly correlated with surface chl a but not with integrated chl a. This finding has implications for the estimation of regional primary production based on remote sensing of near-surface pigments. Altogether, the results confirmed that the high hydrodynamism of the Alboran Sea was associated with marked biological variability and episodic high primary production events. KEY WORDS: Ph… Show more

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Cited by 97 publications
(76 citation statements)
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“…Any process inhibiting cell growth and division but still permitting carbon assimilation may result in an overflow of photoassimilated carbon, which might uncouple POCp and DOCp rates and increase the relative DOCp (Mague et al 1980, Wood & Van Valen 1990. Such an enhanced relative DOCp has been repeatedly ob served under very low light conditions (Thomas 1971, Berman & Holm-Hansen 1974, Morán & Estrada 2001, Marañón et al 2004, and was attributed by some authors to the presence of senescent or light -limited cells. DOCp could be also en hanced at low light levels as a consequence of the inability of cells to proceed with macromolecular synthesis at the same rates as carbon fixation, which would lead to an accumulation of photosynthates that would be released to the external environment (Harding et al 1985, Marañón & González 1997.…”
Section: Differences In Planktonic Carbon Dynamicsmentioning
confidence: 99%
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“…Any process inhibiting cell growth and division but still permitting carbon assimilation may result in an overflow of photoassimilated carbon, which might uncouple POCp and DOCp rates and increase the relative DOCp (Mague et al 1980, Wood & Van Valen 1990. Such an enhanced relative DOCp has been repeatedly ob served under very low light conditions (Thomas 1971, Berman & Holm-Hansen 1974, Morán & Estrada 2001, Marañón et al 2004, and was attributed by some authors to the presence of senescent or light -limited cells. DOCp could be also en hanced at low light levels as a consequence of the inability of cells to proceed with macromolecular synthesis at the same rates as carbon fixation, which would lead to an accumulation of photosynthates that would be released to the external environment (Harding et al 1985, Marañón & González 1997.…”
Section: Differences In Planktonic Carbon Dynamicsmentioning
confidence: 99%
“…Some evidence suggests that DOC release is essentially a physiological process that can be enhanced under suboptimal light levels or under nutrient limitation conditions (Zlotnik & Dubinsky 1989, Morán & Estrada 2001, Marañón et al 2004, López-Sandoval et al 2011. On the other hand, some other studies suggest that part of the recently-fixed photosynthetic carbon might be indirectly released in dissolved form as a consequence of trophic processes, such as grazing or cell lysis, ending in cell breakage (Nagata 2000, Teira et al 2001a.…”
Section: Introductionmentioning
confidence: 99%
“…As shown in Figure 1 (top), Atlantic water enters the investigated area at Gibraltar and proceeds eastward as Modified Atlantic Water (MAW, S < 36.5 and T > 20 °C, Millot, 1999). It continues as a jet along the Spanish coast following an anticyclonic circulation, gradually mixing with the resident waters and producing subsequent mesoscale structures (Rodriguez et al, 1998;Morán & Estrada, 2001). It then turns southward as the Almeria-Oran jet, lying on top of the Levantine Intermediate Water (LIW, S > 37.5 and T < 15°C, Millot, 1999).…”
Section: Introductionmentioning
confidence: 99%
“…She also helped to quantify the importance of plankton activity in biogeochemical fluxes under different conditions of nutrient and light availability. To address these questions she used a variety of approaches, ranging from experimental work (Estrada et al, 2003 to field work (Estrada 1979, and different biogeochemical methodologies: phosphorus nutrient deficient inputs (Berdalet et al 1996), biochemical relations with primary production (Berdalet et al 1993b, CO 2 links with frontal zones (Delgado and Estrada 1994), relationships of dissolved organic carbon with phytoplankton (Estrada and Morán 1996), DNA relative to biomass , excess of carbohydrate synthesis (Fraga et al 1999), variability of photosynthesis parameters (Morán and Estrada 2001) and enzyme kinetics principles (Packard et al 2004). …”
Section: Combining Different Approaches To Build a Reliable Conceptuamentioning
confidence: 99%