Benthic foraminifera as trophic links between phytodetritus and benthic metazoans: carbon and nitrogen isotopic evidence

Marine Ecology Progress Series

Takashi Toyofuku¹  Hisami Suga¹  Motohiro Shimanaga¹  Hiroshi Kitazato¹  Nanako O. Ogawa¹  Hidetaka Nomaki¹  Naohiko Ohkouchi¹  Takeshi Nakatsuka¹ 

关键词: Benthic foraminifera;    Metazoan meiobenthos;    Carbon isotopic composition;    Nitrogen isotopic composition;    Trophic level;    Deep-sea food web;    Foraminiferivory;   

DOI  :  10.3354/meps07309

学科分类：海洋学与技术

来源: Inter-Research

【 摘 要 】

ABSTRACT: We examined the trophic levels of deep-sea benthic foraminifera and metazoans based on stable carbon and nitrogen isotopic compositions of soft tissue to evaluate the role of foraminifera in deep-sea benthic ecosystems. Living benthic foraminifera and metazoans were collected from 2 bathyal sites in Sagami Bay, Japan (water depths 750 and 1430 m) on 3 occasions (April 2004, November 2004 and August 2005). Both carbon and nitrogen isotopic compositions significantly differed among the analysed foraminiferal species. At the deeper site δ¹⁵N of the benthic foraminifera ranged from 6.7 to 11.0‰ (typically 7 to 10‰) with considerable interspecies variations. This implies that most benthic foraminifera utilize primarily surface sediments (4.5‰) or particulate organic matter (6.4‰) as their food sources. Many metazoan meiobenthic organisms, in particular polychaetes of meiofaunal size, some harpacticoid copepods, and kinorhynchs (examined only at the shallower site), exhibited δ¹⁵N heavier than foraminifera, suggesting that they occupy higher trophic levels than benthic foraminifera. Macro- and megabenthos (spatangoids, ophiuroids and Dentalioida) exhibited δ¹⁵N of 10 to 14‰, suggesting they belong in trophic levels 1 to 2 steps higher than metazoan meiobenthos and benthic foraminifera. Similar isotopic trends were observed at the shallower site. Combining the isotopic evidences and the observations on gut contents of some metazoan meiobenthos, together with previous experimental results, the benthic foraminifera in the bathyal Sagami Bay are considered a bridge in the energy flow from phytodetritus and sediments to metazoans.

【 授权许可】

Unknown