• 대한수의학회지
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• 제36권4호
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• pp.757-761
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• 1996

The animal bone-remains excavated with earthwares at Cheju Kimnyungri cave site were investigated morphologically and osteometrically. The number of bone remains were 1706 pieces by morphological criteria. Based on the classification of bony pieces excavated in the cave site, the important animal species in Cheju island during the early Tamra period (presumably between A.D.0 - A.D. 500) was as follows; wild boar(75%), deer(17%), cattle(6%), and horse in small percentage. The excavated bone remains imply that the major fauna of animal species are composed of three species, including Sus scrofa, Cervus nippon and Bos taurus. These data suggests that the archaeological remains such as bone pieces are good indicators of the fauna animals, and of zoological entity in the island.

• 한국제4기학회지
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• 제17권2호
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• pp.145-148
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• 2003

The Kunang cave paleolithic site is located at Tanyang [$N37^{\circ}2'$, $128^{\circ}21'E$], Chungbuk Province, which is in the Central part of the Korean peninsula. The cave is developed at 312 amsl in a karstic mountainous area. The South Han River flows across this region and other caves can also be found near the river. The site was discovered in 1986 and excavated 3 times by the Chungbuk National University Museum until now. The cave was wellpreserved from modem human activities until the first discovery. The full length of the cave is estimated to be ca. 140 m. However, a spacious part up to 11 m from the entrance has been excavated. Eight lithological units are divided over the vertical profile at a depth of 5 m. Each unit is deposited in ascending order as follow: mud layer (Unit 9), lower complex (Unit 8) which is composed of angular blocks and fragments with a muddy matrix, lower travertine layer (Unit 7； flowstone), middle complex (Unit 6; cultural layer) which is composed of fragments with a muddy matrix, middle travertine layer (Unit 5； flowstone), yellowish muddy layer (Unit 4), upper complex (Unit 3； cultural layer) which has a similar composition to Unit 8. the upper travertine layer (Unit 2； flowstone), and finally surface soil layer (Unit 1). The most abundant vestiges in the cultural layers are the animal bones. They are small fractured pieces and mostly less than 3 cm in length. About 3,800 bone pieces from 25 animal species have been collected so far, 90 percent of them belonging to young deers. Previous archaeological study of these bone pieces shows thatprehistoric people occupied the cavenot for permanent dwelling but for temporary shelter during their seasonal hunting activity. More extensive studies of these bones together with pollen analysis are in progress to reconstruct the paleoenvironment of this cave. Only a single date (12,500 BP) obtained from a U-Th measurement of the upper travertine layer was previously available. In spite of the importance of the cave stratigraphy, there was no detail chronological investigation to establish the depositional process of the cultural layers and to understand the periodic structure of the cave strata, alternating travertine floor and complex layers. We have measured five 14C age dating (38900+/-1000, 36400+/-900, 40600+/-1600, more than 51000 and 52000 14C BP) using Seoul National University 14C AMS facility, conducted systematic process of the collagen extraction from bone fragments samples. From the result, we estimate that sedimentation rate of the cave earth is constant, and that the travertine layers, Unit 2 and Unit 3, was formed during MIS 5a(ca. 80 kBP) and MIS 5c (ca. 100 kBP) respectively. The Kunang Cave site is located at Yochonli of the region of Danyang in the mid-eastern part of Korea. This region is compased of limestones in which many caves were found and the Nam-han river flows meanderingly. The excavations were carried out three times in 1986, 1988, and 1998.

• 동굴
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• 제88호
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• pp.7-25
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• 2008

치악산에 위치한 원주 신림면 성남2리에 있는 회옥굴의 동굴생물 종의 분포와 생태적 특성을 알기위해 2004년 11월부터 2005년 6월까지 현장조사 연구를 통해 동굴생물의 보전과 관리를 위한 자료를 얻고자 본 연구를 시행하였으며, 다음과 같은 결과를 얻었다. 조사된 회옥굴의 동굴생물 분포는 8강 18목 28과 34종이었으며, 곤충강이 7목 11과 14종(41.2％)이었다. 회옥굴 내의 서식 생물을 생태적 특성에 따라 구분하면 진동굴성은 8종(23.5％), 호동굴성은 7종(20.6％), 외래성이 19종(55.9％)으로 나타났으며, 동굴에의 적응율은 44％로 외래성 생물의 분포가 높은 것으로 나타났다.

• Animal Systematics, Evolution and Diversity
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• 제3권2호
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• pp.165-174
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• 1987

동남아시아의 열대지역 동굴에서 톡토기를 채집하기 위해 Luzon(필리핀), 파푸아뉴기니아, Sulawesi(인도네시아), 말라야, 타이랜드에 수차 원정을 실시하였다. Acherontiella, Pseudosinella, Sinella, Oncopodura, Arrhopalites 등 속들이 조사지역의 모든 동굴에서 서식하고 있었다. 그러나 수개 속은 분포상 매우 제한되어 있었다. Troglopedetes는 동남아시아 대륙에서는 현저한 분화상을 보였으나 다른곳에서는 볼 수 없었다. Coecoloba는 파푸아 뉴기니아에서만 관찰될 뿐이고 멀리 떨어져 한국과 일본지역에서 다시 나타나고 있다. 대개의 종들은 토양산 계통으로 현재까지 유존종으로 생각되는 것은 발견되지 않았다.

• Animal Systematics, Evolution and Diversity
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• 제2권1호
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• pp.11-20
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• 1986

동굴산 어리톡토기과 (Onychiuridae)의 3 신종이 강원도 정선군 북면의 " 산호동굴"에서 채집 확인되어 Onychiurus polychaetosus . n.sp., O.longisetosus n.sp 및 O.oblogngatus n.sp.로 명명 기재하였다. 아울러 삼척군 신령굴에서 보고되었던 O.izurruensis 도 재기재 하였다. 강원도 영월군 고씨굴에서 신속으로 보고된 이후 (Yosii, 1966) 그 동안 멸종된 것으로 생각되었던 Gulgastruura reticulosa Yosii , 1966 이 본 동굴 입구에서 다시 발견된 사실도 아울러 보고한다. 아울러 보고한다.

• Animal Systematics, Evolution and Diversity
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• 제20권1호
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• pp.79-85
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• 2004

한국 고수동굴 입구지대에서 채집된 유령거미과 1신종, 고수유령거미(Pholcus gosuensis sp. nov,)를 기재한다. 본 신종은 매우 발달된 후측면부배엽(procursus)와 위턱의 전변과 측면 돌기, 퇴화된 구보조돌기(appendix)그리고 바깥자궁(uterus externus)에 있는 경질화된 알키스(arches)를 가지고 있다. 또한 비슷한 구돌기(uncus)와 삽입기를 보유한 한국 고유종인 부채유령거미와 목이유령거미를 닮았으나 수컷 후측면부배엽에 있는 큰 돌기들과 강하게 경질화된 켈로시티(callosity) 그리고 바깥자궁에 있는 경질화된 무늬들의 구조로 구별할 수 있다.

• Animal cells and systems
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• 제2권4호
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• pp.427-434
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• 1998

Canthocamptus morimotoi Miura, a cave-dwelling harpacticoid species belonging to C. mirabilis species group, is fully redescribed and illustrated on the basis of the material newly collected from the type locality, Simpigul Cave, South Korea. C. morimotoi is the only genuine subterranean species in the C, mirabilis group, and claimed to be a relict species restricted to its type locality. The sexually isomorphic ornamentation of the outer terminal seta on the distal exopodal segment of male leg 4 and the well-developed spines on the disteromedial corner of anal somite are the most significant features differentiating this species from ther members of the mirabilis-group.

• Animal Systematics, Evolution and Diversity
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• 제11권4호
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• pp.435-445
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• 1995

한국의 동굴산 가시톡토기과 5종을 기재, 논의한다. 이들 종은 Tomocerus(Monodontocerus) odongnyeoensis. T.(s. str.) liliputanus. T.(s. str.) kinoshitai kinoshitai, T.(Aphaenomurus) interpositus 및 T.(Plutomurus) diversispinus이다. 이 중에서 T.(M.) odongnyeoensis는 신종이며, T.(s. str.) liliputanus는 한국의 동굴에서는 처음으로 보고되는 종이다. 이로써 한국의 동굴산 가시톡토기는 8종이 되며, 한국의 동굴산 톡토기는 총 8과 9속 23종(또는 아종)에 이른다.

• Animal Systematics, Evolution and Diversity
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• 제23권2호
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• pp.155-167
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• 2007

As a result of the faunistic study on the subterranean cyclopoid copepods, four species of three genera in the family Cyclopidae are reported from nine limestone caves and a lava tube in South Korea: Megacyclops magnus (Marsh, 1920), Acanthocyclops orientalis Borutzky, 1966, A, robustus (Sars, 1863) and Diacyclops suoensis Ito, 1956, all of them new to Korean fauna. This paper deals with the taxonomic accounts and illustrations of the four species with the redescription of A. orientalis. This is the first taxonomic study on the cave-dwelling cyclopoid copepods from Korea.

• 한국동물위생학회지
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• 제35권3호
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• pp.251-254
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• 2012

Pectus excavatum (PE) is a ventral chest wall deformity, also known as funnel chest, sunken chest, chondrosternal depression or koilosternia. The 4 months old, 1.3 kg intact-female Pekingese dog was evaluated for acute semicoma and convulsion. The client reported that this patient have had chronic loss of appetite, intermittent dyspnea and palpable sunken breast. The other littermates did not show any abnormalities. On physical examination, cachexia (BCS 1/5), concave sternum, flatten thoracic cavity and cardiac murmur were observed. On radiographic study, the caudal sternum cave to vertebrae and narrowing thoracic cavity. The severities of thoracic deformity were evaluated by deformation indices such as-Frontosagittal index (FSI) and vertebral index (VI). Moderate to severe PE was founded by the radiological measurements.