• The Korean Journal of Food And Nutrition
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• v.23 no.2
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• pp.212-217
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• 2010

To enhance the quality of traditional Dasik, pollen Dasik containing brown rice flour fortified with 5, 10, 15 and 20% pollen powder were prepared, and their physicochemical properties were evaluated. Pollen Dasik possessed higher amount of mineral such as K and Ca than brown rice Dasik. The L value of pollen Dasik decreased with increasing pollen powder compared to brown rice Dasik, while the b value of pollen Dasik was increased with increasing pollen powder compared to brown rice Dasik(p<0.05). Hardness of pollen Dasik decreased with increasing amounts of pollen compared to the brown rice Dasik(p<0.05). Sensory evaluation on pollen Dasik preparewd with over 10% pollen showed the highest sensery evaluation value in overall preference.

• Journal of The Geomorphological Association of Korea
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• v.17 no.2
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• pp.53-61
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• 2010

In this study, pollen analysis and a dating were performed on the alluvial deposits in the Tangjeong Plains in Asan-Si, Chungcheongnam-Do. Specimens were collected at the altitude of about 12m, which belongs to the mid-forest belt in the cool temperate zone. The followings show the results. In general, the target zone passed through TJ-I (the coniferous forest age in which the Pinus forest was dominant), TJ-II (the mixed conifer and deciduous broad-leaved forest age in which Pinus and Quercus were dominant) and TJ-III (the coniferous forest age in which the Pinus was dominant) respectively. TJ-II was subdivided into TJ-IIa and TJ-IIb. TJ-I is presumed to be between about 2,810 and 1,500yrB.P.; TJ-IIa to be between about 1,500 and 1,370yrB.P.; and TJ-IIb to be between about 1,370 and 770yrB.P. As for TJ-III, it is presumed to begin after about 770yrB.P. In comparison with the nationwide pollen zone during the Postglacial, TJ-I and TJ-II are contrasted with the R-IIIa period and also TJ-III is contrasted with RIIIb (so-called human interference age). It is also presumed that Pinus luxuriated there after about 770yrB.P. as forests began to be markedly destroyed in the Tangjeong Plains.

• Proceedings of the Korean Quaternary Association Conference
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• 2004.11a
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• pp.75-76
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• 2004

일산 이산포 BH-4 발굴단면의 퇴적물 시료로부터 화분 포자 및 담수성과 해양성조류화석이 다양하고 풍부하게 산출되었다. 산출된 식물기원 미화석 중, 목본화분 $25{\sim}60%$, 초본화분 $15{\sim}70%$ 그리고 포자 $4{\sim}30%$ 각각 구성 되었다. 또한 담수성 조류(freshwater algae)는 전체 단면구간에서 산출된 반면, 와편모류(dinoflagellate), 아크리타치(acritarch)와 같은 해양성조류(marine algae)는 하부단면구간(절대고도: 3.31-2.74 m)에서만 산출되었다. 산출된 화분 포자 및 통계처리기법(CONISS)을 이용하여 2개의 지역화분대 (local pollen a assemblage zone) 및 4개의 아화분대(local pollen assemblage subzone)가 설정되었다. 제I화분대(시료 $Al-2{\sim}A6-1$, 고도 $2.70{\sim}3.31\;m$)는 다시 제Ia아화분대(시료 $Al-2{\sim}A3-1$, 고도 $2.70{\sim}3.00\;m$)와 제Ib아화분대(시료 $A4-2{\sim}A6-1$, 고도 $3.01{\sim}3.31\;m$)로 세분되었으며; 제II화분대(시료 $A7-2{\sim}A10-1$, 고도 $3.32{\sim}3.72\;m$) 역시 두개의 아화분대인 제IIa(시료 $A7-2{\sim}A8-1$, 고도 $3.32{\sim}3.51\;m$)와 제lIb(시료 $A9-2{\sim}A10-1$, 고도 $3.53{\sim}3.72\;m$)로 이루어졌다. 화분군집조성에 의하면, 미화석들이 퇴적되었던 시기동안에 2개의 산림(forest)형태가 발달했던 나타났다. 제I화분대(고도, $3.31{\sim}2.74\;m$)의 시기동안에는 침엽수와 낙엽활엽수로 이루어진 혼합림으로, 주요 식생은 2엽소나 무(Diploxylon), 가문비((Picea), 낙엽송(Larix)의 침엽수와 참나무(Quercus), 자작나무(Betula), 개암나무(Corylus), 중국굴피 나무속(Pterocarya)의 낙엽활엽수 등이 산악-구릉지에서 주로 서식하였던 것으로 나타났다. 또한 습생나무인 오리나무(Alnus), 버드나무(Salix)등과 해안가 등지에서 잘 서식하는 양치식물과 사초과(Cyperaceae), 명아주과(Chenopodiaceae) 같은 풀들이 하구언(estuary)의 해안가에 주로 서식하였던 것으로 나타났다. 이 시기동안에 해양성조류인 와편모류와 담수성 조류가 동시에 다양하게 산출되는 것은 하구언 퇴적환경이었음을 잘 지시해 준다. 제II화분대(고도, 43.72{\sim}3.36\;m$)가 시작되면서 혼합림은 침엽수림으로 바뀌었으며, 낙엽활엽수들의 서식지가 2엽소나무로 대치되면서 침엽수가 주요 수종을 이루었던 것으로 나타났다. 아마도 이런 산림형태는 자연 기후환경변화 뿐만 아니라 인간간섭에 의해 나타난 결과로 생각된다. 이 시기에 경작식물인 벼과(Gramineae), 옥수수(Zea), 메밀(Fagopyrum)과 논밭의 뚝 등지 에서 서식하는 돼지풀(Ambrosia) 등이 처음으로 산출되는 것으로 보아 인간간섭이 행해졌음을 잘 뒷 받침해준다. 또한 담수성 조류는 변함없이 산출되는 반면, 해양성조류인 와편모류가 산출되지 않는 것으로 보아 해안환경에서 다소 멀 어진 저지대의 습윤한 충적대지환경으로 변하였던 것으로 판단된다.

• The Korean Journal of Quaternary Research
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• v.15 no.2
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• pp.83-91
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• 2001

The environmental change during the upper Holocene was restored at Kimpo alluvial plain on the left bank of Han-river near the Yellow Sea according to the results of pollen analysis and carbon dating, based on the sea-level change from Ilsan area. Pollenzone I (5.8~7.0 m.a.s.l.) was the period of AP-dominance, including mostly Alnus. Study area was under the lagoon or swamp environment influenced by Flandrian transgression during 5,000~3,200 BP. Pollenzone II (7.0~7.4 m.a.s.l.) was the period of Spore & NAP-dominance. It represents that the vegetational environment was changed to drier condition by falling underwater surface caused by sea-level regression, and influenced by human activity during 3,200~2,300 BP. Subzone I a represented the characteristics of the climax of transgression. During subzone I b, herbs with the dominant Alnus were increased gradually, and it was correlated to the stagnation of high sea-level. Subzone II a was the dominant period of Spore by the gradual falling of sea-level. After that, the study area in swamp was emerged to the lowland by the fallen sea-level and herbs, especially Gramineae increased suddenly during Subzone II b. The sudden increase of NAP such as Artemisia, Chenopodiaceae and Umbelliferae with Gramineae during this period indicates the beginning of agriculture at this study area.

• Journal of Korean Society of Forest Science
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• v.80 no.2
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• pp.151-161
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• 1991

I tried to specify the taxa of Fagaceae in Korea by the character of their pollen grains. The light microscope(LM) and the Scanning electron microscope(SEM) were used to examine the pollen grains of 19 taxa, 5 genera. The result are as follows. 1. The pollen of Fagaceae in Korea could be grouped into four types and 4 subtypes. 1) Fagus type 2) Castanea type 3) Lithocarpus, Castanopsis type 4) Quercus type (1) Cyclobalanopsis subtype (2) Prinus subtype (3) Dentatae subtype (4) Cerris subtype. 2. The morphology of the granula on the pollen of Quercus was closely related to the differantiation of the shape of the cup scales. 1) The uniformity of branching granula on the pollen grain surface corresponds to the morphological features of the concentric arrangement of cup scales. 2) The morphological features of the pollen grain surface intermingled with large or small granula, simple-granula and tuber granula which have small points of circular prominence, corresponded to those of short cup scales. 3) The morphological features of the polllen grain surface intermingled with large or small granula, simple-granula and tuber granula with an apex of amoeba type corresponded to those of Q. dentata Thunb, with thin, fine and long cup scales. 4) The morphological features of the pollen grain surface intermingled with large of small granula of with only simple-granula, corresponded to those of Q. acutissima carr. with thick, fine and long cup scales. 3. The result of cluster analysis by coding the sculpture pattern of the pollen grain surface, the existence and nonexistence of surface perforate, the grain size and granula type were coincident with the system of classification of plants and showed an intimated relationship even under th level of species.

• Proceedings of the Plant Resources Society of Korea Conference
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• 2010.10a
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• pp.3-3
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• 2010

GM 들잔디의 환경위해성평가는 유전자변형생물체의 국가간이동등에 관한 법률 (2008년)에 안전관리 및 시험평가가 수행되었다. 일반적으로 GM 작물의 환경위해성평가는 도입 유전자의 안정적 발현여부, 일반적으로 사용되어온 식물과의 실질적 동등성, 화분비산에 의한 유전자이동성 검정, GM재배작물 주변 환경에 미치는 영향, GM작물 및 유전자의 인체 및 동물에 대한 안전성 평가, 위해성 관리 등이 있다. 본 발표에서는 제초제저항성 GM 들잔디를 실용화 하기위한 환경위해성평가의 내용을 소개하기 위하여 GM 들잔디의 안전성평가를 수행한 포장시험에 대해서 간략히 발표하고자 한다. GM 들잔디는 제초제저항성 유전자가 식물체내에 1개의 복제수를 갖으며, 후세대에서도 안정적으로 발현되었다. 또한 TAIL PCR을 통한 도입 유전자의 삽입 부위를 확인하였고, 주변염기서열을 이용한 JG21 들잔디 만의 특이적 염기서열을 얻었다. GM 들잔디의 실질적 동등성검정은 격리온실 수준과 격리포장 수준에 생물학적, 화학적 특성을 조사하였고, 일반 들잔디와 큰 차이가 없음을 확인하였다. GM 들잔디의 화분은 일광조건하에서 약 1시간 이내에 불활성 되었고, 실내의 실온조건에서는 3시간까지 활성이 유지되었다. GM 들잔디 재배포장 ($12m{\times}6m$ 크기)으로부터 화분비산 밀도는 3 m 이내에서 높게 나타났고, 9 m 이상의 거리에서는 낮은 빈도로 일정하게 나타났다. 화분비산에 의한 GM 들잔디 유전자이동성은 근접거리에서 약 15%가 관찰되었고, 반경 3 m 이내에서 거리에 따라서 2 ~ 0.12%의 유전자이동성이 관찰되었다. 각각의 시험모형에 따른 GM 들잔디와 일반들잔디 간의 교잡율을 조사한 결과 들잔디 교잡율은 GM 잔디의 면적과 거리에 의존적이었고, GM 들잔디 면적에 따라서 6-21%의 교잡율이 나타났다. GM들잔디의 인체위해성평가는 독성 및 알레르기 반응성을 검정하였고, 도입유전자 산물인 PAT 단백질은 독성 및 알레르기 반응성이 없음이 알려져 있다. 본 연구에서는 GM들잔디의 독성 및 알레르기 반응성을 검토한 결과 아플라톡신 등의 독성은 검출되지 않았으나, GM과 일반 들잔디 모두에서 화분 알레르기 반응성이 양성으로 나왔다. 그러나 GM들잔디에 도입된 유전자에 의한 알레르기 반응이 아닌 일반들잔디 화분에 가진 알레르겐에 의한 반응성이라 할 수 있다. GM들잔디의 비의도적 방출가능성을 조사하기위하여 시험포장외부의 자연환경에 대해서 환경모니터링을 수행한 결과 GM 들잔디의 유출 및 유전자이동 의한 제초제저항성 들잔디는 나타나지 않았다.

• Journal of Ecology and Environment
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• v.29 no.3
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• pp.287-293
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• 2006

We carried out pollen analysis and radiocarbon dating from sediments of Wangdeungjae moor (960 m a.s.l.) to clarify vegetation history of temperate broad-leaved deciduous forest zone of Mt. Jiri. Three local pollen zones and two sub-zones were recognized on the basis of variation in the palynofloral assemblage: I. Quercus zone (150-114 cm), II. Quercus-Pinus zone (114-43 cm): IIa. Quercus-Pinus subzone (114-83 cm), IIb. Quercus-Pinus-Herbs subzone (83-43 cm), III. Pinus-Quercus zone (43-27 cm). Radiocarbon date from sediment depth 111-116 cm was estimated $1,160{\pm}40yr$ B.P. From these results, overall vegetation around of Wangdeungjae moor and Mt. Jiri have changed from Q. mongolica dominant to steady decrease of Q. mongolica whereas steady increase of P. densiflora, finally abrupt increase of P. densiflora. 'Medieval Warm Period (MWP)' and 'Little Ice Age (LIA)' have not had an effect on change of vegetation around, at least, Mt. Jiri. But at maximum period of LIA, extension of grassland and steady increase of Pinus were recognized around the moor. After then, an abrupt increase of Pinus is supposed that vegetation change is reflected in human impact surging around foothills.

• Journal of Ecology and Environment
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• v.29 no.6
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• pp.573-580
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• 2006

A sediment core from the Cheollipo arboretum ($36^{\circ}$ 47' 57'N, $126^{\circ}$ 09' 04') was studied for pollen analysis in order to reconstruct postglacial vegetational change and environmental changes around the central western region of the Korean Peninsula. The record shows four pollen assemblage zones: Zone CHL-I, Quercus stage (ca. 9,300$\sim$6,200 yr BP): zone CHL-II, Quercus-Pinus stage (ca. 6,200$\sim$4,600 yr BP); zone CHL- III, Pinus-Quercus stage (ca. 4,600$\sim$1,160 yr BP): zone CHL-IV and Pinus stage (ca. 1,160 yr BP-present). During the 9,300$\sim$8,500 yr BP, the early Holocene, researchers have guessed a piece of cool-temperate norihern/altimontane mixed coniferous and deciduous broad-leaved forest. Between 8,500$\sim$4,600 yr BP the Quercus dominated the landscape of study area and the established dates of this typical cool-temperate central/montane deciduous broad-leaved forest vegetation might be ca. 6500 yr BP, and then the Pinus developed around the site at ca. 5,700 yr BP. The abrupt increase of Pinus and NAP (non-arboreal pollen) after ca. 1,100 yr BP indicates the vegetation changes due to human activities. From the dynamics of the Chenopodiaceae pollen indicating salt marsh and freshwater pollen flora such as Typha, Trapa, Nymphoides and so forth, we suggest that the tidal flat was altered into freshwater lake around 6,500 yr BP.

• Journal of the Korean Geographical Society
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• v.47 no.5
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• pp.641-653
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• 2012

We analyzed two radiocarbon-dated lagoonal sediment cores from Cheonjinho and Ssangho using various biogeochemical methods. As a result, the start times of rice agriculture are estimated to be AD 780 for Cheonjinho and 100 BC for Ssangho. There is a large temporal difference in the beginning of rice agriculture between two study sites even though they are closely located on the coast. This result indicates that pollen records are not sufficient to approximate the start time of rice agriculture accurately. A temporal lag seems to exist between the time when rice agriculture was first introduced and the time when full-scale rice agriculture began in the Yeongdong region, probably because of low agricultural productivity. In both study sites, rice agriculture intensified and slope erosion increased 250 years after full-scale agriculture began. This suggests that intensified rice agriculture resulted in an increased number of inhabitants, settlement expansion to hilly areas, and the consequent deforestation.

• The Korean Journal of Ecology
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• v.28 no.1
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• pp.37-43
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• 2005

This study presents the Mid-Lateglacial vegetation history of southwestern Korea. From the result of AMS dating and pollen analysis, four local pollen assemblage zones(BS) were recognized. The four local pollen assemblage zones are BS 1. 12,222cal BC$\sim$9,160cal BC: cool-temperate northern/altimontane mixed coniferous & deciduous broad-leaved forest, BS 2. 9,160cal BC$\sim$ 4,210cal BC: cool-temperate central/montane deciduous broad-leaved forest, BS 3. 4,210cal BC$\sim$125cal BC: cool-Temperate southern/submontane mixed coniferous & deciduous broad-leaved forest. BS 4. BC125cal ${\sim}$present: warm-temperate/cool-temperate southern/submontane coniferous forest. Pine forest expanded since 4,210cal BC and full-scale rice cultivation might started since 2,120cal BC. A radical expansion of Pinus densiflora forest after postglacial stage might be caused by human impacts including full-scale agriculture.