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자료유형
학술저널
저자정보
이유리 (경북대학교) Hirofumi Asahi (한국해양과학기술원 부설 극지연구소) 우한준 (한국해양과학기술원) 김형직 (한국해양연구원) 이성주 (경북대학교) 김부근 (부산대학교)
저널정보
한국해양과학기술원 Ocean and Polar Research Ocean and Polar Research Vol.36 No.4
발행연도
2014.12
수록면
437 - 445 (9page)
DOI
http://dx.doi.org/10.4217/OPR.2014.36.4.437

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A time-series sediment trap was operated at a water depth of 4950 m from July 2003 to May 2004 at KOMO station (10o30'N, 131o20'W) in the northeastern equatorial Pacific, with the aim of understanding the temporal variation of planktonic foraminifera assemblages in response to the seasonal shift of Inter-Tropical Convergence Zone (ITCZ). A total of 22130 planktonic foraminifera specimens belonging to 30 species and 11 genera were identified, which shows a distinct seasonal variation with high values (125~288 specimens m?2 day?1) in the winter to spring (December-May) and low values (16~23 specimens m?2 day?1) in the fall (September-November). In addition, seasonal ecological differences of foraminifera assemblages are distinctly recognizable: omnivorous foraminifera occurred predominantlyduring the summer season, whereas herbivorous ones were dominant during the winter season. Such seasonal variations correspond to the seasonal shift of the ITCZ. Enhanced occurrence of herbivorous species during the winter-spring season seems a result of surface water mixing generated by the southward shift of the ITCZ. The increase in omnivorous species during the summer season may be due to the northward movement of the ITCZ caused by weakened wind speed, resulting in the intensification of water column stratification and nutrient-poor environment. A significant reduction of planktonic foraminifera specimens during the fall is attributed to heavy precipitation and reduction in light intensity.

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