Vertical biogenic particle flux during Austral summer in the Antarctic Peninsula area

被引:38
|
作者
Anadón, R [1 ]
Alvarez-Marqués, F
Fernández, E
Varela, M
Zapata, M
Gasol, JM
Vaqué, D
机构
[1] Univ Oviedo, Dept Biol Organismos & Sistemas, E-33071 Oviedo, Spain
[2] Univ Vigo, Dept Ecol & Biol Anim, Vigo 36200, Spain
[3] Univ Vigo, Dept Biol Vegetal & Ciencia Suelo, Vigo 36200, Spain
[4] Inst Espanol Ocenog, Lab La Coruna, La Coruna 15080, Spain
[5] CIMA, Conselleria Pesca, Xunta Galicia, Vilanova De Arousa 36620, Spain
[6] Inst Ciencias Mar, E-08039 Barcelona, Spain
关键词
D O I
10.1016/S0967-0645(01)00129-1
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
During both FRUELA cruises, we performed eight circum-diel stations in the Bellingshausen Sea (South of Drake Passage), and the Bransfield and Gerlache straits, where MULTITRAP sediment-traps were deployed for periods of 24 h in order to study carbon (C) and nitrogen (N) export from the photic layer. Two types of regions were visited: High chlorophyll a (Chl a) areas dominated by large-sized diatoms (> 10 mum), and low Chi a areas dominated by Cryptomonas sp. or micro flagellates. The vertical fluxes of C, N, and Chi a, and the number of fecal pellets (FP) were measured, and the taxonomic composition of the sedimented microplankton was analysed; the results compared to the standing stocks in the water column overlaying the sediment traps. We measured higher carbon export rates in the diatom-dominated regions (Gerlache Strait), than in the stations dominated by small phytoplankton (Bransfield Strait and Bellingshausen Sea), The measured C-fluxes ranged from 115 to 800 mg C m(-2) day(-1). Typical C:N ratio (by atoms) varied from 5.5 to 16.4. Nitrogen export, however, was not directly related to C export and, thus, we measured changes in the C: N ratio with stations having higher abundance of FP or detritus presenting higher C: N ratios, Variations in the vertical C-flux were related to biological variables such as FP number, algal community composition (quantitative counts and qualitative SEM observations), and photosynthetic and prokaryotic activity of the sedimented material. We calculated photic layer loss rates of C, N, Chl a (0.53-8.0% day(-1)) and of the different microplankton taxonomic entities (0.27-9.5% day 1). Some exceptionally high loss values were found for Cryptophyceae during Fruela 96. The obtained results are discussed within the conceptual framework set by the relationships between phytoplankton size and rood web structure, and concomitant carbon export from the photic layer. (C) 2001 Elsevier Science Ltd. All rights reserved.
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收藏
页码:883 / 901
页数:19
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