• 제목/요약/키워드: Diplopsalis

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한국 연안해역의 미기록 Peridiniales 목 와편모조 시스트 (New Records of Dinoflgallate Cysts of Peridiniales from the Korean Coastal Waters)

  • 박종식;윤양호
    • 환경생물
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    • 제36권1호
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    • pp.82-89
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    • 2018
  • 남해 중앙부의 가막만 입구해역에 설치된 sediment trap의 와편모조 시스트 및 시스트에서 발아된 유영세포에서 국내 미기록 와편모조 시스트 9종을 관찰하였기에 형태적 특징을 고찰하였다. 미기록 와편모조 시스트는 모두 종속영양종으로 와편모조문 (Dinophyta), 와편모조강 (Dinophyceae), 페리디니움목 (Peridiniales)에 속하였다. 미기록 종은 Brigantedinium majusculum (Protoperidinium sinuosum), cyst of Diplopsalis lebourae, cyst of Protoperidinium excentricum, cyst of Pt. sp. cf. nudum, cyst of Pt. obtusum, cyst of Pt. ventricum, cyst of Protoperidinium sp.1, cyst of Protoperidinium sp.2 및 미동정된 cyst of Peridinales 등이었다.

New Records of Dinoflagellates in Five Genera of Peridiniales (Dinophyceae) from Korean Waters

  • Lee, Joon-Baek;Kang, Su-Min
    • 환경생물
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    • 제35권3호
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    • pp.251-264
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    • 2017
  • A study searching for unrecorded and taxonomically undescribed indigenous species has been conducted since 2006. Samples were collected from many sites in coastal waters and offshore in Korea as well as around Jeju Island. Since 2008 we have found 13 unrecorded species belonging to family Diplopsaliaceae, Heterocapsaceae, Kolkwitziellaceae, Protoperidiniaceae and Thoracosphaeraceae. The species are as follows, Preperidinium meunieri (2014), Heterocapsa ovata (2015), H. pseudotriquetra (2015), Diplopsalis lenticula (2008), Protoperidinium abei (2009), P. diabolus var. longipes (2010), P. depressum (synonym: P. parallelum (2008)), P. latispinum (2016), P. punctulatum (2010), P. solidicorne (synonym: P. spinosum (2010)), P. subpyriforme (2010), P. pacificum (2013), Scrippsiella hexapraecingula (2009) (note; The numbers in parenthesis refer to the year that the species was reported as unrecorded indigenous species by National Institute of Biological Resources, NIBR hereafter). Among these, 5 species were described as newly recorded species in Korean waters, and 8 were re-described in this study.

Modern Dinoflagellate Cysts Distribution off the Eastern Part of Geoje Island, Korea

  • Shin, Hyeon-Ho;Yoon, Yang-Ho;Matsuoka, Kazumi
    • Ocean Science Journal
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    • 제42권1호
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    • pp.31-39
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    • 2007
  • Distributional characteristics of dinoflagellate cysts in surface sediments were investigated in relation to environmental factors in the eastern part of Geoje Island, Korea. Samples were collected from 10 stations in February of 2004 and water temperature and salinity were measured in February, May, September and November of 2004. Total 30 taxa of dinoflagellate cysts were identified representing 19 genera, 28 species and 2 unidentified species. Among these dinoflagellate cysts, Brigantedinium spp. of which relative proportion in th e total dinoflagellate cysts was 23.5%, was the most abundant at all stations except St. 1, and was followed by Spiniferites bulloideus (8.6%), Lingulodinium machaerophorum (8.2%) and Diplopsalis lenticula (6.7%). In addition, ellipsoidal cysts of the genus Alexandrium (Alexandrium catenella - tamarense type) and Gymnodinium catenatum, known to be causative organisms for PSP, occurred with high concentrations. Scrippsiella trochoidea was also found; however, its cyst concentration was low. Generally, species composition in the study area was similar to these reported from Jinhae Bay and Busan Harbor and several dinoflagellate cysts reflected the eutrophic condition. Cyst distribution in th e eastern part of Geoje Island seems to be influenced by the Tsushima Warm Current flowing from the southwest. The mean water temperature was $12.0^{\circ}C$ in February, $14.7^{\circ}C$ in May, $20.9^{\circ}C$ in September and $17.2^{\circ}C$ in November, which was most favorable for Alexandrium spp. growth. The abundances of dinoflagellate cysts rang e d from 528 to 2,834 cysts/g dry sediment. Higher concentrations were recognized in sediments of west area of the Jisimdo than at other stations. The cyst composition of this area was closely related to these of Jinhae Bay and Busan Harbor from which currents flow into this area. Higher cyst concentration in the west area of Jisimdo might be due to formation of the gyre.