AME Aquatic Microbial Ecology Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials AME 36:41-52 (2004) - doi:10.3354/ame036041 Response of bacterial grazing rates to experimental manipulation of an Antarctic coastal nanoflagellate community Dolors Vaqué1,*, Susana Agustí2, Carlos M. Duarte2 1Institut de Ciències del Mar de Barcelona-CMIMA, CSIC, Departament de Biologia Marina i Oceanografia, Passeig Marítim de la Barceloneta, 37-49, 08003 Barcelona, Catalunya, Spain 2IMEDEA (CSIC-UIB), Institut Mediterrani d¹Estudis Avançats, Miquel Marquès, 21, 07190 Esporles, Mallorca, Illes Balears, Spain *Email: dolors@icm.csic.es ABSTRACT: We examined changes of bacterial losses related to heterotrophic nanoflagellate (HNF) size distribution in late spring/early summer (1998/1999) using 9 grazing experiments in a coastal Antarctic area (Johnson¹s Dock, Livingston Island, Bransfield Sector). Water samples were subjected to size fractionation through 50 and 5 μm pore sizes to obtain a truncation of the microbial food web. In each fraction, we estimated bacterial loss rates and abundance and biomass of HNF grouped into 4 size classes (≤2, 2 to 5, 5 to 10, 10 to 20 μm). We also investigated whether grazing on bacteria was mainly due to HNF, and which HNF size class had a major impact on bacteria. We expected that in the 50 μm fraction, large protists (ciliates, dinoflagellates) would prey preferentially on nanoprotists and relieve bacterial pressure from HNF. Bacterial grazing rates were estimated by disappearance of fluorescently labeled bacteria over 24 h. These showed similar values in both experimental treatments, although they were slightly higher for the 50 μm fraction. Average grazing rates were 4.8 × 105 ± 3.6 ×: 105 cells ml-1 d-1 in the 5 μm treatment and 6.9 ×: 105 ± 3.2 ×: 105 cells ml-1 d-1 for the 50 μm fraction. In the 5 μm fraction, HNF abundance (integrated over 24 h, HNFi) and bacterial grazing rates were significantly related. The best relationship was obtained with the smallest HNFi size classes (from ≤2 and 2 to 5 μm). In the 50 μm fraction, no relationships were found between bacterial loss rate and both total HNFi and any HNFi size class in terms of abundance and biomass. However, microozooplankton was negatively related to total bacteria and both HNFi abundance and biomass. The major contributor to this negative relationship was the HNFi size classes from ≤2 and 2 to 5 μm. Consequently, and against our expectations, large protists contributed to microbial food-web complexity by masking carbon fluxes from bacteria to HNF, and by feeding on both bacteria and nanoprotists. KEY WORDS: Antarctica · Johnson¹s Dock · Bacteria · Heterotrophic nanoflagellate size · Phagotrophic · Ciliates · Dinoflagellates · Grazing Full article in pdf format PreviousNextExport citation RSS - Facebook - Tweet - linkedIn Cited by Published in AME Vol. 36, No. 1. Online publication date: June 24, 2004 Print ISSN: 0948-3055; Online ISSN: 1616-1564 Copyright © 2004 Inter-Research.
The main purpose of this work is the inquiry and explanation of the determinants of the different forms of remuneration in Portugal. Although the existence o...
Recent changes in the editorial leadership, name, content, and publishing process for Estuaries and Coasts and looming changes in scientific publishing as technology advances have provided an opportunity to assess the health and examine the growth in size and reputation of the journal. Estuaries and Coasts has grown in size by about fourfold, with a concurrent decline in acceptance rate of about 1.5% per year to reach the present 65% acceptance rate. The number of paper downloads has increased exponentially to the current 4,000 downloads per month. Most (81%) of the published papers come from senior authors in the USA, with only 15% of the papers coming from senior authors based in non-English-speaking countries. The average number of authors per paper increased from an average of two in 1980 to three at present, and the impact factor has risen to 1.563 in 2006, at about the middle of the range in impact factors for related journals, from an average of 1.295 in the previous 10 years. Papers published in Estuaries and Coasts have a long citation half-life (8.4 years), resulting in very few (3.5%) published papers never receiving citations. All metrics assessed portray Estuaries and Coasts as a journal on the rise that stands up in comparisons of quality and citation rate with other journals in its field.
In oligotrophic ecosystems, bacterial production (BP) via the microbial loop and grazing processes plays a crucial role in carbon transfer (CT) to higher trophic levels. However, there studies quantifying CT from bacteria to the marine food web are limited. In this study, we used 13 C-isotope tracers and cavity ring-down spectroscopy to measure primary production (PP), BP, bacterial respiration (BR), and CT within the microbial food web in oligotrophic waters. Our results revealed that the BP rate, ranging from 0.02 to 4.93 μg C L −1 d −1 , was significantly lower than the total PP, which ranged from 2.69 to 16.71 μg C L −1 d −1 . Our findings indicate that grazing of bacteria in the Red Sea is substantial. The removal of grazers through prefiltration lead to a 9.5-fold increase in BP rates, rising from 0.37 ± 0.04 μg C L −1 d −1 to 3.52 ± 1.04 μg C L −1 d −1 at the stations analyzed. This significant increase suggests that a large portion of bacterial carbon is rapidly transfer to higher trophic levels via grazing. In addition, carbon transfer (CT) to the food web, measured in size fractions above picoplankton (>1.2 or > 3 μm), accounted for an average of 72.7 ± 4.0% of the net bacterial production (Net BP = BP + CT), underscore the crucial role of grazers in bacterial carbon cycling. This transfer increased significantly with increasing temperatures, highlighting the enhanced role of the microbial loop in CT during warmer conditions. We found that at some stations, a large proportion of the carbon assimilated by bacteria was used for respiration, averaging 1.37 ± 0.54 μg C L −1 d −1 . This high respiratory demand of bacterial cells in oligotrophic waters may explain the low bacterial growth efficiency (BGE) of 9.7% ± 1.0% observed in our study, along with the significant correlation between BP and BGE. Our findings demonstrated that BP effectively transfers carbon through the microbial loop to higher trophic levels in the oligotrophic and warm waters of the Red Sea.