• 한국제4기학회지
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• 제15권2호
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• pp.93-99
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• 2001

동북 일본 오우산맥 중앙부의 제4기 후기의 식생변천 과정을 밝히기 위하여, 암수현 탕전정 탕천소(북위 $39^{\circ}15'$, 동경 $140^{\circ}45'$, 표고 590m)의 퇴적물을 대상으로 화분분석을 실시하였다. 그 결과, 탕천소 일대는 Y-I대의 Pinus-Picea-Betula림(최종빙기 최성기 말) $\longrightarrow$ Y-II대의 Betula림(만빙기 $\longrightarrow$ Y-III대의 Quercus-Betula림(후빙기 초기) $\longrightarrow$ Y-IV대의 Fagus림(후빙기 중기) $\longrightarrow$ Y-V대의 Fagus-Quercus-Cryptomeria림 (후빙기 후기)으로 변천하였음을 알 수 있었다. 그리고 Y-I대와 Y-II대는 아한대성 침엽수림 시대, Y-III대는 아한대성 침엽수림 시대에서 냉온대성 낙엽활엽수림 시대로의 이행기, Y-IV대는 냉온대성 낙엽활엽수림 시대, Y-V대는 침엽.낙엽활엽혼합림 시대에 대비되는 것도 알 수 있었다.

• 한국환경복원기술학회지
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• 제9권2호
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• pp.45-58
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• 2006

This study was aimed to propose the plan of creating a biotope reflecting an ecological education as well as its function as the habitats of amphibian in Namsan Urban Natural Park in Seoul. There were Cheonil mineral spring area which was located on the southern side of Namsan, wetlands which was already created on the east valley(800$m^2$) and a buffer area of the circumference(1,100$m^2$) as the biotope sites. Major fields of this study include a survey of the staus, a basic plan, a master plan; a survey of this site was focused on topography, water system, existing vegetation, wildbird, amphibian, trail; a detailed plan was focused on flow plan, planting plan, facility plan. Existing vegetation was classified into 8 types; Pinus densiflora forest, Pinus densiflora planted area, Prunus sargentii-Quercus spp. forest, Pinus rigida forest, Robinia pseudoacacia forest, artificial green space, wetlands, south beltway. There were Pinus densiflora planted area and Prunus sargentii-Quercus spp. forest as major vegetations of this site. 14 species and 33 individuals of wildbirds appeared, Rana temporaria ornativentris and Hynobius leechi were investigated in the wetlands.In particular, habitats of amphibian were divided eco-zone, buffer-zone and restore-zone, and habitats and facilities which would be suitable for the characteristics of each space were planned. As a result, environment elements of good habitats including spawn wetlands of amphibian, harbor of amphibian, water plant of wetland, wild shrubs forest, ecological landscape forest, wetland observation trail, fence of wetland protection and ramp by pebble and log were created at the site. The amphibian biotope of Namsan is rated high as an important space for conserving biodiversity. Accordingly, continuous monitoring of this biotope as a urban habitat is required as the environment changes.

• 한국제4기학회지
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• 제13권1호
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• pp.1-23
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• 1999

경기도 화성군 안녕리 지역의 충적층 시추 시료로부터 화분분석이 처음으로 수행되었다. 그 결과 2개의 화분대: 제 1 화분대(Pollen Zone I : Ainus-Quercus-Pinus)와 제 2 화분대(Pollen Zone II : Pinus)가 설정되었다. 제 1 화분대는 약 3,500 yr. B.P.~2,000 yr. B.P.동안 침엽-낙엽 활엽수 혼합림(mixed coniferous and deciduous broadleaved vegetation), 제 2 화분대는 2,000 yr. B.P.이후의 침엽-상록활엽수림 (coniferous vegetation and evergreen broadleaved vegetation)으로 각각 특징지워진다. 제 1 화분대는 저지대 하호성(fluvio-lacustrine)환경으로 호수가 형성되기 시작하는 시기이며, 제 2 화분대는 완전한 호수 혹은 저수지환경이 형성된 시기이다. 화분 분석결과에 의하면 약 3,500 yr. B.P.부터 2,000 yr. B,P.까지는 식물의 서식분포는 주로 자연 환경조건에 지배를 받은 반면에, 2,000 yr. B.P.이후는 소나무림으로 특징지워지면서 인간의 정착생활 시작으로 농경지 확대와 자연림 파괴가 시작되어 자연림에서 인공림으로 바뀌어진 것으로 해석된다. 결과적으로, 화분분석을 통하여 이 연구지역의 고환경과 인간간섭시기를 밝힐 수가 있었으며, 또한 담수조류의 분석으로 과거 존재했던 호수의 규모를 규명할 수가 있었다.

• The Korean Journal of Ecology
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• 제21권5_1호
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• pp.427-433
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• 1998

The standing crop and net production were estimated in Moojaechi on Mt. Jungjok. By using the decay model of organic carbon, absolute year of bog peat was calculated. Pollen analysis to bog peat revealed vegetational history and climate change around Moojaechi. The time required for amount of the accumulated peat in the bog was estimated in terms of the balance of the accumulation and decay of organic carbon of the deposit peat. Absolute year of the peat surveyed in this study was about 314 years. Pollen of Pinus was predominant in all the pollen zone, Geamineae and Cyperaceae increased in lower pollen zone while Pinus in upper pollen zone. This showes that climate of the past was probably more humid than that of present. In addition, middle pollen zone showed warming trend which is suggested by high pollen concentration of Quercus, Juglans, Carpinus and Corylus. It suggests that overall environment and vegetation were changed from warmer and more humid to dry condition in Moojaechi and it is considered as the course of boggy ground formation by retrogressive successions.

• 한국지형학회지
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• 제17권1호
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• pp.39-48
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• 2010

충남 온양천 유역의 후빙기 환경변화를 밝히기 위한 사례연구로서 온양천의 지류인 금곡천의 상류부(이하 조사지역)에 분포하는 선상지 퇴적층을 대상으로 화분분석을 실시하였다. 시료채취지점은 해발고도 약 67.5m로 현재 냉온대 중부 식생대에 속한다. 분석결과는 다음과 같다. 조사지역 일대는 약 3,000yrB.P. 이후 크게 SC-I기(期)(Pinus가 우점하는 침엽수림시대) → SC-II기(期)(Quercus·Castanea가 우점하는 낙엽활엽수림시대) → ③ SC-III기(期)(Pinus-Quercus-Ulmus/Zelkova가 우점하는 침활혼효림시대)로 변천했다. 각 시대의 연대는 SC-I기(期)와 SC-II기(期)가 약 3,000~2,000yrB.P., SC-III기(期)가 약 2,000yrB.P.~현재로 수렴된다. 전국적 후빙기 화분대와 대비하면, SC-I기(期)와 SC-II기(期)는 RIIIa 그리고 SC-III기(期)는 RIIIb에 대비된다. 그리고 약 2,000yrB.P. 이후 조사지역 일대는 삼림파괴에 따른 소나무림의 분포역이 확대되었으며, 또한 메밀화분의 출현율이 높은 점 등을 고려할 때, SC-III기(期)는 인간간섭의 시대로서 이 시대에 들어서면서부터 삼림파괴가 본격화되었고, 당시 거주민들은 농경생활을 했었을 것으로 추정된다.

• 환경생물
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• 제22권1호
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• pp.127-132
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• 2004

본 연구는 계룡산 국립공원내 해발 650 m이상의 산림식생을 대상으로 식물사회학적 방법_으로_ 산림군락을 분류하여 계룡산 국립공원 관리에 필요한 기초자료를 제공하고자 수행되었다. 계룡산 상부지역의 총 51개 조사구를 분석한 결과, 산림군락은 신갈나무군락, 서어나무군락, 소나무군락 및 굴참나무군락으로 구분되었다. 신갈나무군락은 29개 조사구에서 나타났으며, 군락 구분종은 신갈나무, 좁은단풍, 천남성, 용수염, 은분취이다. 서어나무군락은 10개 조사구에서 나타났으며, 군락 구분종은 서어나무, 까치박달, 층층나무, 대사초, 산수국이다. 소나무군락은 7개 조사구에서 나타났으며, 군락 구분종은 소나무, 조록싸리, 산딸기, 참억새, 이삭여러, 맑은대쑥, 큰기름새 이다. 굴참나무군락은 5개 조사구에서 나타났으며, 군락 구분종은 굴참나무이다.

• Journal of Plant Biology
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• 제30권4호
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• pp.267-276
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• 1987

A pollen analytical study was carried out on the accumulated humus samples collected from 27 sites under the different plant communities of Mt. Seolag. These pollen spectra were then compared with the actual vegetation. The aboreal pollen(AP) and non-abnoreal pollen(NAP) were 1 Family 25 Genus and 5 Family 5 Genus, respectively. Among the aboreal pollen identified, the pollen of Pinus, Quercus, Betula and Acer were appeared in abundance and the coniferous pollen of Pinus was occupied at least 20%-65% through all the sites studied. The pollens of Abies, Betula, accer, Quercus, Carpinus, Corylus, Fraxinus, Styrax, Prunus and Ericaceae were in accordance with the present vegetation but the other pollens were inconsistent with the actual vegetaton. It suggests that it was caused by the difference between Wehseolag and Namseolag of subalpine zone in Mt. Seolag was 200 m by pollen spectra. Quercus was distributed at the lower part of Namseolag and the subalpine boreal elements were increased with increasing altitudes. The pollen spectra of each site was put together into 5 groups of pollen assemblage by cluster analysis and the community coefficient (CC) was over 60% between all sites studied.

• The Korean Journal of Ecology
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• 제13권4호
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• pp.311-320
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• 1990

This paper deals with pollen analysis of a 190cm core collected from the Chollipo Arboretum sedimentary basin($N36^{\circ}47$ 43", $E1269^{\circ}$ 7") in southwestern Korea in order to know the change of the climate and vegetation. In this research it is found that the pollen zones are divided into two layers. Pollen zone, I, the lower layer, is flourished with broadleaved trees such as Quercus, Alnus, Corylus, Betula, Carpinus and Castanopsis, and about 30~40% of pollen of those trees consist of that of Q. acuta/glauca and Castanopsis which are evergreen trees. And pollen of Trapa, Typhaceae and Nymphaceae living in wet habitat, is dominant among the nonarboreal pollen. Therefore we can conclude that it ould be warmer and more humid than present in this area of the past. In pollen zone, the upper layer, pollen of Pinus is dominant and those of Artemisia, Gramineae, Compositae and spore are increased in quantity, while pollen of Quercus, Belula and Nymphaceae decreased. It it supposed that the climate of this zone was drier than that zone.that zone.

• Journal of Plant Biology
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• 제2권2호
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• pp.1-21
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• 1959

1. The plant communities on Mt. Sulak, a typical alpine mountain in central Korea was researched from the standpoint of ecological survey. 2. The plant on this mountain can largely be classified into 2 categories, the warm zone (below 1100m) and the frigid zone. The former is again classified into a broad-leaved tree formation and a needle-leved tree formation, and the latter is calssified into a broad-leaved tree formation and needle-leaved tree formation, and shrub formation. 3. The broad-leaved tree formation in the warm zone can largely be classified into a Carpinus laxiflora-syringa Palibiniana var. kanibayashi association(1), a Carpinus erosa-Acer Pseudo-sieboldianun association(2), and a Quercus mongolica- Tripterygium Regelii association(3). 4. The needle-leaved tree formation in the warm zone can also largely ben classified into a Pinus densiflora- Miscanthus sinensis association(4), Abies holophylla- Tripterygium regelii association(5), Pinus kordiensis- Rhododendron schlippenbachii association(6) In the association(4), the canopy of the Pinus densiflora is gradually being occupied by the Quercus mongolica which is one kind of broad-leaved trees. 5. We can fully see a DryoPteris type of the flour layer plant type in the association (3) and also see a Sasamorpha type in the association (5). 6. The broad-leaved tree formation in the frigid zone can largely be classified into Quercus mongolica- Rhododendron schlippenbachii association (8). The constituents of tree and subtree layers in (7) and (8) associations are similar to those association (3), but the constituents of the shrub layer are different from those of associtation (3) due to the difference in height. 7. The needle-leaved formation in the frigid zone can largely be classified into Thuja koraiensisRodgersia podophylla var. viritis association (9) and Abies nephrolepis-Acer tschonoskii var. rubripes asscciation (10). The species of alpine plants or subalpine plants are gradually increased in this formation. 8. The shrub formation can also largely be classified into a Rhododendron mucronulatum- Patrinia saniculaefolia association (11) and Pinus pumila associatio (12). Association (12) has largely developed on the windy place. Association (12) was burned due to the bombing during the Korean war, but now we recoginized there occurred an invasion of Tripterygium Regelii in such a place. 9. The herb layer species which constitute the shrub formation are mostly alpine or subalpine plants of small size, and their kinds are also very few. 10. The growth of the Moss layer is especially good because of the varied conditions of the habitat. The kinds which can easily be seen are the genus of Thunidium, Haplocladium, Brachythecium, Macromitrium, Holonitrium, Atrichum, Schwstchkeopsis, Grimmia, Hedwigia, Rhynchostegium and Mnium. 11. The genus of the Sphagnum densly grows like a mat at the acid and moisturous place above 1100m. The authors should express their thanks to father. Yang Kisup, Dean of Catholic Medical College, Prof. Yoon Doksuen, from their valuable advice. Thanks arealso due to Prof. Numata, Chiba University, Prof. Takagi, Nagoya University and Prof. Ando, Hiroshima University in Japan for his kind help and identification of Bryophytes.

• 한국지형학회지
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• 제23권3호
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• pp.1-11
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• 2016

This study estimated vegetation environment and agricultural activity during the late Holocene inferred from pollen analysis of peat on floodplain of Wangpo-cheon around Neungsan-ri, Buyeo-gun, South Korea. By result of pollen analysis of 28 horizons from Trench NS 1 and NS 4, vegetation environment during 2,300 to 1,700 yr BP was divided into Pollen Zone I (Quercus-Alnus), Pollen Zone II (Quercus-Alnus-Gramineae) and Pollen Zone III (Pinus-NAP-Gramineae). The pollen analysis suggests that agricultural activity in the Buyeo area was widely spread from the early time of the Pre-Iron Age to the late Samhan Age and buckwheat field seem to be built to substitute paddy field during the early time of the Pre-Iron Age.