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MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 262:43-53 (2003) - doi:10.3354/meps262043 Alkaline phosphatase activities in the central Atlantic Ocean indicate large areas with phosphorus deficiency Montserrat Vidal1,*, Carlos M. Duarte2, Susana Agustí2, Josep M. Gasol3, Dolors Vaqué3 1Departament d¹Ecologia, Universitat de Barcelona, Avinguda Diagonal 645, 08028 Barcelona, Spain 2Institut Mediterrani d¹Estudis Avançats (CSIC-UIB), C/ Miquel Marqués 21, 07190 Esporles (Illes Balears), Spain 3Institut de Ciències del Mar (CMIMA-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Spain *Email: montsevidal@ub.edu ABSTRACT: The activity of the enzyme alkaline phosphatase (APA) was studied along 2 latitudinal transects in the central Atlantic (28°S to 28°N) and compared to the distribution of nutrient concentrations, planktonic biomass and other variables reflecting community P status. Using 3-0-methyl fluorescein phosphate (MF-P), APA was measured fluorometrically in 2 size fractions (<0.8 and <150 µm) and in the dissolved fraction (i.e. that fraction passing through 0.2 µm filters). Significant APA (p < 0.05) was recorded over extensive areas of the central Atlantic, ranging from 4 to 50 nmol MF-P l-1 h-1. Most activity arose from the free dissolved fraction, followed by the <0.8 µm size fraction. The relatively low APA in the central Atlantic is due to the low biomass that characterises most of the area covered by the transects. Nevertheless, the specific activity per unit biomass was high in both the north and south Atlantic subtropical gyres in this area. Along the transects, APA displayed an inverse relationship to the calculated upward turbulent nutrient fluxes. The results support the existence of persistent P-limited conditions in much of the central Atlantic Ocean. This is consistent with stoichiometric data and estimated rate processes and fluxes in the area, indicating that P regeneration from dissolved organic phosphorus may play an important role in the central Atlantic, allowing efficient utilisation of P in the biogenic layer and avoiding P loss through the diffusive vertical flux of dissolved organic matter that preferentially removes C and N. KEY WORDS: Alkaline phosphatase activity · Atlantic Ocean · Phosphorus deficiency · Enzyme activity Full text in pdf format Supplementary Appendix PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 262. Online publication date: November 07, 2003 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2003 Inter-Research.
Prochlorococcus and Synechococcus are pico-sized cyanobacteria that play a fundamental role in oceanic primary production, being particularly important in warm, nutrient-poor waters. Their potential response to nutrient enrichment is expected to be contrasting and to differ from larger phytoplankton species. Here, we used a metagenomic approach to characterize the responses to nutrient enrichment in the community of picocyanobacteria and to analyze the cyanophage response during a mesocosms experiment in the oligotrophic Red Sea. Natural picoplankton community was dominated by Synechococcus clade II, with marginal presence of Prochlorococcus (0.3% bacterial reads). Increased nutrient input triggered a fast Synechococcus bloom, with clade II being the dominant, with no response of Prochlorococcus growth. The largest bloom developed in the mesocosms receiving a single initial input of nutrients, instead of daily additions. The relative abundances of cyanophage sequences in cellular metagenomes increased during the experiment from 12.6% of total virus reads up to 40% in the treatment with the largest Synechococcus bloom. The subsequent collapse of the bloom pointed to a cyanophage infection on Synechococcus that reduced its competitive capacity, and was then followed by a diatom bloom. The cyanophage attack appears to have preferentially affected the most abundant Synechococcus clade II, increasing the evenness within the host population. Our results highlight the relevance of host-phage interactions on determining population dynamics and diversity of Synechococcus populations.
The fate of photosynthetic carbon in marine ecosystems dominated by different types of primary producers was examined by compiling published reports on herbivory, autotrophic respiration, decomposition, carbon storage, and export rates as fractions of net primary production (NPP) in ecosystems dominated by different types of autotrophs (i.e. oceanic and coastal phytoplankton, microphytobenthos, coral reef algae, macroalgae, seagrasses, marsh plants, and mangroves). A large fraction (>40%) of the NPP of marine ecosystems is decomposed within the system, except for microphytobenthos (decomposition, ∼25% of NPP). Herbivory tends to be highest for microalgae (planktonic and benthic, >40% of NPP) and macroalgae (33.6 ±4.9% of NPP) and is somewhat less for higher plants. Microphytobenthos export on average a much higher proportion of their NPP than do other microalgal communities, whereas marine macrophytes, except marsh plants, export a substantial proportion (24.3–43.5% on average) of their NPP. fraction of NPP stored in sediments is 4‐fold greater for higher plants (∼10–17% of NPP) than for algae (0.4–6% of NPP). On average, ∼90% of the phytoplankton NPP is used to support local heterotrophic metabolism (i.e. grazed or decomposed). This fraction is even higher in oceanic communities. Mangrove forests, and to a lesser extent seagrass meadows and macroalgal beds, produce organic carbon well in excess of the ecosystem requirements, with excess photosynthetic carbon (i.e. export rate plus storage) in these ecosystem representing ∼40% of NPP. Extrapolation of these results to the global ocean identifies marine angiosperms, which only contribute 4% of total ocean NPP, as major contributors of the NPP stored (30% of total ocean carbon storage) and subsequently buried in marine sediments. Consideration of burial of NPP from marine angiosperms should lead to estimates of total burial of marine NPP that exceed current estimates by 15–50%.
The Banc d′Arguin is a marine ecosystem of global conservation significance, the largest bird sanctuary of western Africa, supported by one of the most extensive seagrass beds in the world composed by three seagrass species, two temperate near their southern limit (Zostera noltei and Cymodocea nodosa) and one tropical at its northern limit (Halodule wrightii). Here we predict the fate of this seagrass ecosystem under climate change scenarios during the 21st century, using species distribution models and sea level rise estimates. We forecast a probable decline in total seagrass area of 3340 Km2 (78%) by 2100, involving the loss of both temperate seagrasses (Z. noltei, C. nodosa), the foundational ecosystem components. By 2050, only the tropical species (H. wrightii) would remain, which forms thin and sparse shallow stands functionally distinct from the previous tall dense meadows that span wider vertical ranges. Intertidal flats, the essential bird foraging habitats, would become unvegetated and also suffer a major reduction in area (114 km2 by 2050, 587 km2 by 2100). The large projected loss of foundational seagrass species portends a collapse of major ecosystem functions with profound impacts on biodiversity, fishery resources and ecosystem services.
The interannual changes in leaf formation and vertical growth rates and their correlation to the records available of environmental change (rainfall, mean sea level, water temperature, and transparency) were examined in 15 Posidonia oceanica meadows growing along the Spanish Mediterranean coast between 1967 and 1992. P. oceanica leaf production fluctuated interannually, but it did not exhibit any steady trend toward decline, indicative of nonhuman effects on changes in water quality in these areas. Conversely, the steady decline in vertical rhizome growth rate of P. oceanica observed in two sites suggests that shoreline erosion there could derive from human activities. In all meadows examined, interannual variability in vertical rhizome growth of P. oceanica showed clear oscillating trends, suggesting alternating episodes of sediment erosion and accretion every 7 yr and at least every 25 yr. Mean sea level and surface water temperature have been increasing for the last two decades, but water transparency has been declining. However, overall trends only accounted for 24–37% of the long‐term climatic variance. Rainfall interannual changes were dominated by time scales of 8 and 28 yr, whereas water transparency, temperature, and sea level showed dominant time scales in the oscillations of 4 and 15 yr, 6 and 20 yr, and 11 and 27 yr, respectively. In addition, 33% of P. oceanica vertical growth variability in the southern Spanish Mediterranean coast derived from variability in rainfall, suggesting a rise of erosive coastal conditions during rainy years. The similarity in the interannual changes of seagrass growth over a wide spatial scale (1,000 km), together with the significant coupling between seagrass growth and climate variability, points out climate change, and not widespread deterioration derived from anthropogenic pressure, as the main source of the observed changes in the Mediterranean littoral zone.