• 제목/요약/키워드: Sub-alpine conifer

검색결과 4건 처리시간 0.018초

One Unrecorded Endophytic Fungi from Sub-alpine Conifer, Rhizosphaera pini

  • Eo, Ju-Kyeong;Park, Eunsu
    • 한국균학회지
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    • 제47권2호
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    • pp.121-124
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    • 2019
  • An endophytic fungus, Rhizosphaera pini strain NIE7426, was isolated from the sub-alpine coniferous tree Abies nephrolepis in Mt. Nochu of Gangwon Province. It was characterized by macroscopic and microscopic features, as well as the internal transcribed spacer (ITS) 1, 2 and 5.8S sequences. All morphological and molecular features support the first recognition of this taxon in Korea. In addition, this study adds A. nephrolepis as a host plant R. pini.

청원 옥산 소로리 유적지 일대 유기질 니층의 화분분석에 의한 식생변천사에 관한 연구 (A Study on Vegetation History of Organic Muds of Sorori Archaeological Site, Oksan-myeon, Cheongwon-gun, Korea)

  • 김주용;양동윤;봉필윤;이융조;박지훈
    • 한국제4기학회지
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    • 제15권2호
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    • pp.75-81
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    • 2001
  • 한반도 내륙지역의 제4기 후기의 식생변천 과정을 밝히기 위하여, 충북 청원군 옥산면 소로리 유적지($36^{\circ}41'3"N$, $127^{\circ}24'49"E$)의 퇴적물을 대상으로 화분분석을 실시하였다. 그 결과, 이 지역 일대는 \circled1OS-1의 아고산성 침엽수림(만빙기;약 15,000yr.B.P.~10,000yr.B.P.)$\longrightarrow$\circled2OS-2의 침엽ㆍ낙엽 활엽수혼합림(후빙기 초기;약 10,000yr. B.P.경)$\longrightarrow$\circled3OS-3의 냉온대성 낙엽활엽수림(후정기 중기;약 10.000yr.B.P.~2,000yr.B.P.)$\longrightarrow$\circled4OS-4의 침엽수림(후빙기 후기;약 2,000yr.B.P.) 이후)로 변천하였음을 알 수 있었다.을 알 수 있었다.

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Post LGM Fluvial Environment and Palynological Changes of South Korea

  • Kim, Ju-Yong;Yang, Dong-Yoon;Bong, Pil-Yoon;Nahm, Wook-Hyun;Lee, Heon-Jong;Lee, Yung-Jo;Hong, Sei-Sun;Lee, Jin-Young;Kim, Jin-Wkan;Oh, Keun-Chang
    • 한국제4기학회지
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    • 제17권2호
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    • pp.17-23
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    • 2003
  • In Korea terrestrial fluvial sequences can be used as pedological and sedimentological markers indicating a millenium-scale environmental and climatic changes imprinted in fluvial sub-environments, which in turn are represented by the cyclicity of fluvial sands, backswamp organic muds, and flooding muds intercalations of frostcracked or dessicated brown paleosols. Post LGM and Holocene fluvial and alluvial sedimentary sequences of Korea are formed in such landscapes of coastal, floodplain, backswamp and hillslope areas. Among them, the most outstanding depositional sequences are fluvial gravels, sands and organic mud deposits in coastal, fluvial, or alluvial wetlands. The aim of this study is to explain the sedimentary sequences and palynofloral zones since the last 15,000years, on the basis of organic muds layers intercalated in fluvial sand deposits. Jangheung-ri site of Nam river, Soro-ri site of Miho river, Youngsan rivermouth site in Muan, Oksan-ri site of Hampyeong and Sanggap-ri site of Gochang are illustrated to interpret their sedimentary facies, radiocarbon datings, and palynofloral zonation. Up to the Middle to Late Last Glacial(up to 30-35Ka), old river-bed, flooding, and backswamp sequences contain such arboreal pollens as Pinus, Abies, and Picea, and rich in non-arboreal pollens like Cyperaceae, Gramineae, Ranunculaceae, and Compositae. During the LGM and post-LGM periods until Younger Dryas, vegetation has changes from the sub-alpine conifer forest(up to about 17-11Ka), through the conifer and broad-leaved deciduous forest, or mixed forest (formed during 16,680-13,010yrB.P), to the deciduous and broad-leaved forest (older than 9,500yrB.P). In the Earliest Holocene flooding deposits, fragments of plant roots are abundant and subjected to intensive pedogenic processes. During Holocene, three arboreal pollen zones are identified in the ascending order of strata; Pinus-Colyus zone(mixed conifer and deciduous broad-leaved forest, about up to 10Ka), Alnus-Quercus forest (the cool temperate deciduous broad-leaved forest, about 10Ka-2Ka), and Pinus forest (the conifer forest, about after 2Ka), as examplified in Soro-ri site of Cheonwon county. The palynological zonations of Soro-ri, Oksan-ri, Sanggap-ri, Youngsan estuary, and Gimhae fluvial plain have been recognized as a provisional correlation tool, and zonations based on fluvial backswamp and flooding deposits shows a similar result with those of previous researchers.

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백두대간 피재-도래기재구간의 능선부 식생구조 (Vegetation Structure of Mountain Ridge from Pijae to Doraegijae in the Baekdudaegan, Korea)

  • 오구균;박석곤
    • 한국환경생태학회지
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    • 제15권4호
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    • pp.330-343
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    • 2002
  • 백두대간상의 피재-도래기재구간 능선부에서 43개소 조사지(면적 500$m^2$)를 설정하여 식생구조를 파악하였다. TWINSPAN분석에 의하여 조사지의 식물군집을 분류한 결과, 아고산대 혼효림, 신갈나무-당단풍군집, 신갈나무-소나무군집, 신갈나무군집, 일본잎갈나무림으로 분리되었다. 백두대간 피재-도래기재구간의 능선부는 대부분 신갈나무가 우점하고 있었으며, 국지적으로 분비나무, 주목 등의 한대 기후대 침엽수와 낙엽수종들이 혼효하고 있었다. 조사지의 산림군집의 종다양성지수(면적 1,000$m^2$)는 2.0149~3.0139로서 백두대간에 위치한 국립 공원들의 능선부 식생구조와 유사하였다.