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Pelagic food web structure in high nutrient low chlorophyll (HNLC) and naturally iron fertilized waters in the Kerguelen Islands region, Southern Ocean
被引:10
|作者:
Hunt, Brian P., V
[1
,2
,3
]
Espinasse, Boris
[4
]
Pakhomov, Evgeny A.
[1
,2
,3
]
Cherel, Yves
[5
]
Cotte, Cedric
[6
]
Delegrange, Alice
[7
,8
]
Henschke, Natasha
[2
]
机构:
[1] Univ British Columbia, Inst Oceans & Fisheries, Vancouver, BC, Canada
[2] Univ British Columbia, Dept Earth Ocean & Atmospher Sci, Vancouver, BC, Canada
[3] Hakai Inst, Heriot Bay, BC, Canada
[4] UiT Arctic Univ Norway, Dept Arctic & Marine Biol, Tromso, Norway
[5] La Rochelle Univ, CNRS, UMR 7372, Ctr Etud Biol Chize CEBC, F-79360 Villiers En Bois, France
[6] Sorbonne Univ, CNRS, IRD,MNHN, Lab Oceanog & Climat Expt & Approches Numer LOCEA, Paris, France
[7] Acad Lille Hauts De France, Inst Natl Super Professorat & Educ INSPE, Site Outreau10,Rue H Adam, F-62230 Outreau, France
[8] Maison Rech Environm Nat, Lab Oceanol & Geosci LOG UMR CNRS 8187, 32 Ave Foch, F-62930 Wimereux, France
基金:
加拿大自然科学与工程研究理事会;
关键词:
Zooplankton;
Micronekton;
Food web;
Size structure;
Stable isotopes;
Southern Ocean;
Kerguelen plateau;
STABLE-ISOTOPE ANALYSIS;
PHYTOPLANKTON BLOOM;
SPECIES COMPOSITION;
TROPHIC POSITION;
SCOTIA SEA;
BODY-SIZE;
CARBON;
NITROGEN;
ZOOPLANKTON;
BIOMASS;
D O I:
10.1016/j.jmarsys.2021.103625
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
The Kerguelen Plateau is a region of natural iron fertilization in the Southern Ocean, within the typically iron limited High Nutrient Low Chlorophyll (HNLC) waters of the eastward flowing Antarctic Circumpolar Current. Between 26 February and 19 March 2018, the MOBYDICK expedition investigated pelagic ecosystem dynamics in the Kerguelen Island region on the northern plateau during the post-phytoplankton bloom period. The survey specifically targeted sampling at two stations in the HNLC waters to the west of the Kerguelen Plateau, and in the iron enriched waters on and to the east of the plateau. A combination of WP2, WP3 and Mesopelagos midwater trawl were used to sample the mesozooplankton (125 mu m to <= 10 mm), macrozooplankton (10-30 mm) and micronekton (> 30 to 200 mm) communities. Stable carbon (delta C-13) and nitrogen (delta N-15) isotopes were measured across representative samples of taxa from all stations. Trophic positions was estimated using a Bayesian isotope mixing model (tRophicPosition), that uses both the delta C-13 and delta N-15 values of baselines and consumers. Meso/ macrozooplankton trophic positions (TPs) were similar to 2.4 on the plateau and > 0.6 TPs higher at the upstream HNLC stations. This provides empirical evidence for shorter food chains on the diatom dominated plateau and longer food chains in the HNLC region dominated by pico and nanophytopklankon. Meso/macrozooplankton TPs were also elevated downstream of the plateau, though to a lesser extent than in the upstream region, likely reflecting the effect of downstream iron transport, supporting elevated phytoplankton production in the downstream re-gion. There was a consistent increase in trophic position between meso/macrozooplankton and micronekton of similar to 0.6 at all stations. Food chain length was therefore determined by the composition of and interactions between the trophic levels below micronekton. Similar trophic structure at the two upstream HNLC stations, on either side of the northern branch of the Polar Front, indicated that food chain length was robust to the differences in community composition, and supports the critical role of size structured trophic interactions in determining food web properties.
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