Kor J Fish Aquat Sci 46(6),886-891,2013 한수지 46(6), 886-891, 2013
Original Article
886 서 론
Stichopus japonicus는우리나라에서수산자원으로활용되는
해삼종으로순수목(Aspiodchirotida), 돌기해삼과(Stichopodi- dae), 돌기해삼속(Stichopus)에속하며, 우리나라전해역에걸 쳐서식한다. 해조류가서식하는암반이나돌무더기지역, 또
는모래, 펄분포지역등다양한환경에서서식하며(Uthicke,
1999), 퇴적물에 포함된 미세조류(micro-algae)와 박테리아
(bacteria), 유기쇄설물(detritus) 등을먹이로취하는퇴적물식 자(deposit feeder)로섭식에의한생교란작용(bioturbation)을 통해저서생태계에산소와유기물을공급하고영양염을순환시 키는생태학적으로중요한역할을한다(Bakus, 1973; Yingst,
1976; Massin, 1982). 또한, 국제적인자원관리위기종으로보 호받고있으나최근웰빙수산물로인식되면서전세계적으로 소비량이꾸준히증가하고있어산업적으로도매우중요한종 이다.
우리나라의해삼생산량은 1990년에 2,491톤을기록한이래 로지속적으로감소하다가인공종묘생산에의한소규모의씨
뿌림양식이도입된이후 2010년에 2,687톤으로빠르게회복되
고있지만, 아직까지는수출수요에비해생산량이크게부족한 실정이다. 씨뿌림양식은삼면이바다이고광활한갯벌이발달 한우리나라의천혜의지형적조건에서최적의해삼양식방법 으로화석연료를사용하지않은자연의존형양식방법으로녹 색성장산업으로서의가치또한매우크다. 그러나지금까지우
Article history;
Received 4 March 2013; Revised 1 October 2013; Accepted 25 October 2013
*Corresponding author: Tel: +82. 61. 452. 0361 Fax: +82. 61. 452. 0362 E-mail address: [email protected]
Kor J Fish Aquat Sci 46(6) 886-891, December 2013 http://dx.doi.org/10.5657/KFAS.2013.0886 pISSN:0374-8111, eISSN:2287-8815
ⓒ The Korean Society of Fishereis and Aquatic Science. All rights reserved
한국 서해안 돌기해삼(Stichopus japonicus)의 서식지 기질 특성
박광재·류상옥1*·백영숙1·김윤설2·강희웅3·한현섭4
국립수산과학원 갯벌연구소, 1연안관리기술연구소, 2해양수산과학원 국제갯벌연구소,
3국립수산과학원 서해수산연구소, 4국립수산과학원 사료연구센터
Substrate Characteristics of Sea Cucumber Stichopus japonicus Habitats in the West Coast of Korea
Kwang-Jae Park, Sang-Ock Ryu1*, Young-Sook Baek1, Yeun-Seol Kim2, Hee-Woong Kang3 and Hyon-Sob Han4
Tidal-Flat Research Center, National Fisheries Research & Development Institute, Gunsan 573-882, Korea
1Institute of Coastal Management & Technology, Muan 534-830, Korea
2Internatioal Tidal Flat Research Institute, Fisheries Research and Department Institute, Sinan 535-802, Korea
3West Sea Fisheries Research Institute, National Fisheries Research & Development Institute, Incheon 400-420, Korea
4Aquafeed Research Center, National Fisheries Research & Development Institute, Pohang 791-923, Korea
We analyzed surface sediments to explain the substrate characteristics of sea cucumber Stichopus japonicus habitat. The analyses included grain-size determination, water content (WC), loss on ignition (IL), chemical oxygen demand (COD), and acid volatile sulfide (AVS) content. We obtained data on sea cucumber density, weight, and length at each station in a marine farming area in the middle of Korea's Taean coast on the West (Yellow) Sea in May, 2012. The apparent density of S. japonicus was high in coarse and bimodal sediments, whereas it was low in fine and unimodal sediments. The mass of S. japonicus was greater in fine than in coarse sediments, showing a different trend from sea cucumber density. The values for WC, IL, COD, and AVS in surface sediments were higher in areas with high densities of S. japonicus than in areas with low sea cucumber densities. In particular, the concentration of AVS was much higher than the value proposed in Japanese criteria for areas with high S. japonicus density.
Key words: Stichopus japonicus, Grain sizes, Geochemical parameters, Substrate characteristics, Taean coastal zone
해삼 서식지 기질 887
리나라의기술수준은종묘생산과해삼의생리적특성에관한 일부연구만있을뿐씨뿌림양식의근간이되는기질등서식지 환경특성에대한연구는전무한실정이다(Lee and Park, 1999;
Park et al., 2007). 기질특성에관한지금까지의연구는주로미 국과영국, 일본등을중심으로활발하게수행되어왔다. 그러 나이들선행연구의대부분은해삼의생교란작용(bioturbation)
에의한통기현상(aeration)과영양염순환, 해삼서식지와생
물풍부도사이의관계를규명하는물질순환연구에국한되었
을뿐서식적지조건규명을위한연구는보고된바없다(Mas-
sin, 1982; Uthicke, 1999; Yamada et al., 2009; Bellchambers et al., 2011).
본연구는해삼씨뿌림양식의근간이되는기질특성을파악 하여서식적지조건을규명하는데주요목적이있으며, 연구결 과는정부의해삼섬개발사업이나인공종묘방류를통한씨뿌 림양식산업을위한기초자료로활용될것으로기대된다.
재료 및 방법
해삼서식지의기질특성을파악하기위하여 2012년 5월에태
안군해삼양식어장으로허가가난해역의 19개정점에서해삼 을포획하고, 퇴적물시료를채취하였다(Fig. 1). 조사지역의정 점별수심은 4-17 m 범위이다. 해삼은직경 6 m의원안에서식 하는모든해삼을직접잠수하여포획하였으며, 퇴적물시료는 주로선상에서채니기(La-bond type grab sampler)를사용하여 채취하였다. 잔자갈이상의굵은퇴적물이분포하여채니기를 이용하여채취가불가능한일부정점에서는직접잠수하여시 료를채취하였으며, 채취정점의위치는 GPS (Garmin GPS V, USA)를이용하여측정하였다.
퇴적물의 입도분석은 Ingram (1971)의 표준입도분석 방법 에의거하여체분석및피펫법을병행하여실시하였다. 퇴적물 유형은자갈, 모래, 실트, 점토의함량비를기준으로분류하는
Folk (1968)의삼각다이아그램을이용하여구분하였고, 퇴적
물의조직표준치는 Folk and Ward (1957)의계산식에의해구
하였다. 또한 10 Ø보다세립한입자의질량은외삽법에의한균
등분배방식을이용하여구분하였고, 조립구간은 -3 Ø (8 mm, pebble) 까지분석되었다.
퇴적물의함수율(WC), 강열감량(IL), 화학적산소요구량(COD) 및산휘발성황화물(AVS)은해양환경공정시험기준 (국토해양부,
2010)에의거하여분석하였다.
결 과
해삼 출현양상
태안군해삼양식어장에서 2012년 5월에출현한해삼(Sticho- pus japonicus)의밀도(density)는 0.00-3.39개체/m2 범위(평균 0.53개체/m2)로지역에따라다양한출현양상을보였다(Table
1). 모항과방포항주변해역에서는 2개체/m2이상으로높은출 현밀도를보인반면, 이원방조제와신두리, 근소만, 몽산포주 변해역에서는 1개체도출현하지않았다. 해삼의체장(length) 은 8.8-21.5 cm 범위(평균 15.2 cm)로대부분의조사해역에
서 15 cm 이상의크기를보였으나안면도북서측과남서측일
부해역에서는 10 cm 미만으로상대적으로작은크기를보였 다. 예외적으로, 높은출현밀도를보인모항에서는체장의크기 가작은데이는어민들이수시로일정크기이상의해삼을포획 하기때문이다. 체폭(width)은 3.2-10.5 cm 범위(평균 6.3 cm)
로모항주변을제외한대부분해역에서 7 cm 내외의크기를보
였으나천수만해역에서는 10 cm 이상으로큰크기를보였다. 체중(weight)은 49.7-470.0 g 범위(평균 195.5 g)로체폭의분
포와동일하게모항주변을제외한대부분해역에서 200 g 내외
를보였으나천수만해역에서는 400 g 이상으로큰체중을보였 다(Table 1) (Fig. 3).
Fig. 1. A map showing the study area and the sampling sites.
Bathymetry is related to approximate lowest low water level.
36˚45´N36˚30´N
8 Mean grain size (Unimode)
Mean grain size (Bimode) Density
Weight
Mean grain size WCIL 6
4 2 0
1 2 3 4 5 6 7 8 9 10111213141516171819 -2
8 6 4 2 0 -2
50 40 30 20 10 0
5 500
400 300 200 100 0 4 3 2 1
Mean grain size (phi)Mean grain size (phi) 0 2Density (ind./m) COD (mg O/g-dry)Weight (g)WC (%)2
Station No.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Mean grain size
WCIL 8
6 4 2 0 -2
50 40 30 20 10 0
Mean grain size (phi)Density (ind./m2)
COD (mgO2/g-dry)
1 2 3 4 5
y = 0.08x-0.21 r = 0.45 4
3
2
1
0
0 5 10 15 20
6 7 8 9 10 11 12 13 14 15 16 17 18 19
Density (ind./m2)
AVS (mg S/g-dry)
y = 3.34x+0.17 r = 0.46 4
3
2
1
0
0.0 0.1 0.2 0.3 0.4
박광재ㆍ류상옥ㆍ백영숙ㆍ김윤설ㆍ강희웅ㆍ한현섭 888
해삼 서식지 기질 특성
퇴적물 입도
태안군해삼양식어장의퇴적물은모래질실트(sandy silt)에
서자갈(gravel)에이르기까지다양한유형을보였다. 자갈과
모래, 실트, 점토의함량은각각평균 17.4%, 42.1%, 28.5%,
12.0%로모래가가장우세한분포를보였다(Table 2). 퇴적물
의평균입도는 -1.6-6.5 Ø 범위(평균 3.3 Ø)로방포항과천수만 입구에서뚜렷하게조립하였고, 신두리와모항남측, 안면도서
측, 천수만에서뚜렷하게세립한경향을보였다. 분급은 0.3-5.1
Ø 범위(평균 2.7 Ø)로매우양호한것에서극단적으로매우불
량한것에이르기까지다양한분포를보였다(Table 2).
퇴적물의구간별함량분포를살펴보면 19개정점중 9개정
점의퇴적물이복모드(bimode) 분포를보이는반면, 10개정점
의퇴적물은단모드(unimode) 분포를보였다. 지역적으로는모
항주변과방포항주변의안면도서측및남측퇴적물은복모드 분포를보인반면, 그밖의지역의퇴적물은단모드분포를보 였다(Fig. 2).
저질
태안군해삼양식어장퇴적물의함수율(WC)은 15.6-42.1%
범위(평균 30.3%)로다양한분포범위를보였다(Table 3). 강 열감량(IL) 또한 1.4-7.1% 범위(평균 3.3%)로다양한분포범 위를보였으며, 함수율의함량비에영향을받기때문에함수율 이높은곳에서높은유기물함량비를나타내었다. 화학적산소 요구량(COD)은 3.3-18.0 mgO2/g-dry 범위(평균 9.0 mgO2/g- dry)로이원방조제와신두리주변해역에서낮았고모항주변 과안면도남서해역에서상대적으로높았으나, 모든조사정점
에서일본의수산환경퇴적물기준치인 20 mgO2/g-dry보다낮
은농도분포를보였다(Table 3). 산휘발성황화물(AVS)의농도 는 0.007-0.369 mgS/g-dry 범위(평균 0.110 mgS/g-dry)로대 부분의정점에서는낮은농도분포를보였으나, 모항주변등일 Table 1. Appearance aspect of sea cucumber Stichopus japonicus
at each station
* The sea cucumber Stichopus japonicus in station 5 (Mo Harbor) has been frequently captured to be a certain size by fishermen.
Station Density
(ind./m2) Length
(cm) Width
(cm) Weight
(g) Water depth (m) 12
34 5* 67 89 1011 1213 1415 1617 1819
0.390.00 0.000.07 3.390.46 0.000.00 0.850.39 0.112.12 0.490.39 1.060.11 0.210.04 0.04
17.8- 13.5- 15.39.5 -- 15.914.7 13.68.8 19.415.6 10.013.6 17.321.5 21.5
5.8- 6.5- 3.28.3 -- 5.65.5 5.05.8 6.46.1 4.04.1 10.57.4 10.5
146.4 -- 175.0 294.249.7
-- 164.8 173.6 149.695.0 170.0 180.0 70.785.0 239.2 470.0 470.0
5.58.9 9.37.4 11.36.3
6.26.5 4.04.7 11.59.4 14.26.4 7.65.1 4.04.2 10.9
Fig. 2. The distribution of the mean grain size expressed uni or bi- mode, and the density and weight of the sea cucumber Stichopus japonicus on each station.
Table 2. The textural parameters and types of the surface sediment at each station
Station Gravel(%) Sand (%) Silt
(%) Clay (%) Mean
(Ø) Sorting
(Ø) Sediment type (Folk, 1968) 12
34 56 78 109 1211 1314 1516 1718 19
0.0 0.2 0.0 0.0 57.7
0.60.0 0.0 0.0 46.7 0.0 80.7 25.9 20.4 1.1 25.4 70.4 1.1 0.8
83.1 83.2 20.6 88.6 22.6 18.3 56.4 13.8 100 86.4 30.5 11.8 30.0 13.9 35.6 36.8 17.2 30.8 20.1
12.2 10.3 53.8 11.8 7.5 52.6 30.5 76.3 0.0 16.3 9.1 31.04.8 57.0 27.7 28.3 9.2 47.3 55.8
4.7 25.6 6.3
3.9 7.9 28.5 13.1 9.9 0.0 4.5 6.5 13.12.7 28.0 16.3 9.5 3.2 20.8 23.3
3.2 2.5 6.3 3.2 0.2 6.4 4.5 5.1 3.0 3.1 0.9 -1.6 2.6 6.5 2.9 2.3 -0.6 5.7 6.1
1.2 2.1 2.8 1.1 4.0 3.0 2.6 1.7 0.3 1.1 3.9 2.6 4.82.9 5.1 4.1 3.1 2.7 2.9
(g) mSzS mSsZ (g) MmsG
zSsZ mSS msGG (g) MgM gMgM (g) MmsG (g) M
36˚45´N36˚30´N
8 Mean grain size (Unimode)
Mean grain size (Bimode) Density
Weight
Mean grain size WCIL 6
4 2 0
1 2 3 4 5 6 7 8 9 10111213141516171819 -2
8 6 4 2 0 -2
50 40 30 20 10 0
5 500
400 300 200 100 0 4 3 2 1
Mean grain size (phi)Mean grain size (phi) 0 2Density (ind./m) COD (mg O/g-dry)Weight (g)WC (%)2
Station No.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Mean grain size
WC IL 8
6 4 2 0 -2
50 40 30 20 10 0
Mean grain size (phi)Density (ind./m2)
COD (mgO2/g-dry)
1 2 3 4 5
y = 0.08x-0.21 r = 0.45 4
3
2
1
0
0 5 10 15 20
6 7 8 9 10 11 12 13 14 15 16 17 18 19
)
y = 3.34x+0.17 r = 0.46 4
3
해삼 서식지 기질 889
부정점에서는일본의수산환경퇴적물기준치인 0.20 mgS/g- dry보다높은농도분포를보였다(Table 3).
고 찰
해삼(Stichopus japonicus)은해저표면에서미세조류와박테 리아, 유기쇄설물등을주요한먹이로섭취하는것으로알려져 있다(Bakus, 1973; Yingst, 1976; Massin, 1982). 표층퇴적물 의입도와퇴적물내에존재하는유기물함량등의기질특성 은해삼의서식및분포를결정하는중요한요인으로작용한다 (Conand and Chardy, 1985; Uthicke and Karez, 1999; Bell- chambers et al., 2011).
태안군해삼양식어장에서해삼의출현밀도가높은지역과낮 은지역의표층퇴적물입도분포특성을비교한결과, 출현밀도 가높은지역의퇴적물은주로평균입도가조립하고분급이불 량한반면, 출현밀도가낮은지역의퇴적물은상대적으로평균
입도가세립하고분급이양호한경향을보였다(Fig. 2). 또한출
현밀도가높은지역의퇴적물구성은주로조립구간의함량이 뚜렷하게높지만조립구간과세립구간에서각각최빈값을갖는 복모드분포를보이는반면, 출현밀도가낮은지역에서는조립 구간이나세립구간에서최빈값을갖는단모드분포를보여퇴 적물의입도및분포특성이해삼의출현밀도를결정하는중요
한요인임을확인할수있었다(Fig. 2). 해삼의체폭과밀접한상
관관계를갖는체중은퇴적물의모드특성와무관하게평균입 도가세립한퇴적물에서높게나타난반면, 평균입도가조립한 퇴적물에서는상대적으로낮게나타나출현밀도특성과는다른 양상을보였다(Fig. 2).
저질분석결과퇴적물의함수율(WC)과강열감량(IL) 값은퇴
적물의평균입도가세립한정점에서높고조립한정점에서낮 아평균입도와밀접한상관관계를보였다(Fig. 3). 화학적산소
요구량(COD)과산휘발성황화물(AVS) 농도는두변수간에유
사한변화패턴을보이며평균입도가세립한정점에서높은농 도를보였으나함수율, 강열감량과는다르게평균입도와밀접 한상관관계는보이지않았다(Fig. 3). 유기물등의오염물질을 산화제로산화·분해시켜정화하는데소비되는산소량을나타 내는척도인화학적산소요구량은해삼의출현밀도가높은지역 에서낮은지역보다높은농도를보이는정(+)의상관관계를보 였으나모든정점에서일본의유기물오염기준인 20 mgO2/g-
dry를초과하지않아건강한서식지가유지되고있음을확인할
수있었다(Fig. 4). 퇴적물내산소의고갈및결핍정도를나타
내는산휘발성황화물(AVS)의농도또한해삼의출현밀도가높 은지역에서낮은지역보다높은농도를보이는정(+)의상관관 계를보였으나, 화학적산소요구량의농도분포와는달리일부 정점에서일본의유기물오염기준인 0.2 mgS/g-dry를크게초 Table 3. The concentrations of water content (WC), ignition loss (IL), chemical oxygen demand (COD), and acid volatile sulfide (AVS) at each station in the surface sediments
Station WC
(%) IL
(%) COD
(mgO2/g-dry) AVS (mgS/g-dry) 12
34 56 78 109 1211 1314 1516 1718 19
37.9 31.6 41.2 24.1 42.1 32.3 28.3 26.9 25.1 31.9 23.9 21.6 32.4 29.8 35.3 22.1 15.6 35.9 38.2
3.2 1.7 3.3 1.4 4.2 7.1 2.9 2.9 1.7 2.1 2.9 2.6 3.3 6.5 4.1 2.5 2.5 3.6 3.7
5.0 3.9 3.3 15.5 3.4 18.0 9.3 12.0
5.1 7.0 8.4 10.6 16.0 8.4 16.5 7.6 3.9 7.9 9.5
0.022 0.007 0.033 0.013 0.342 0.369 0.139 0.055 0.013 0.220 0.013 0.101 0.022 0.028 0.246 0.064 0.012 0.154 0.239 Fig. 3. The correlation of water content (WC), ignition loss (IL),
chemical oxygen demand (COD), and acid volatile sulfide (AVS) with mean grain size on each station.
36˚45´N36˚30´N
8 Mean grain size (Unimode)
Mean grain size (Bimode) Density
Weight
Mean grain size WCIL 6
4 2 0
1 2 3 4 5 6 7 8 9 10111213141516171819 -2
8 6 4 2 0 -2
50 40 30 20 10 0
5 500
400 300 200 100 0 4 3 2 1
Mean grain size (phi)Mean grain size (phi) 0 2Density (ind./m) COD (mg O/g-dry)Weight (g)WC (%)2
Station No.
1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 Mean grain size
WC IL 8
6 4 2 0 -2
50 40 30 20 10 0
Mean grain size (phi)Density (ind./m2)
COD (mgO2/g-dry)
1 2 3 4 5
y = 0.08x-0.21 r = 0.45 4
3
2
1
0
0 5 10 15 20
6 7 8 9 10 11 12 13 14 15 16 17 18 19
Density (ind./m2)
AVS (mg S/g-dry)
y = 3.34x+0.17 r = 0.46 4
3
2
1
0
0.0 0.1 0.2 0.3 0.4
Station No.
박광재ㆍ류상옥ㆍ백영숙ㆍ김윤설ㆍ강희웅ㆍ한현섭 890
과하는경향을보였다(Fig. 4). 이에반해개인적으로분석한모
든시료에서해삼내장속퇴적물의산휘발성황화물농도는불 검출된반면, 화학적산소요구량의농도는서식지표층퇴적물 의농도보다두드러지게높게나타났다. 일반적으로해삼은표 면하수 mm 이내에서구강촉수(buccal tentacles)를이용하여
먹이를섭취하는퇴적물식자로알려져있다(Massin, 1982). 이
들의생태계에서주요역할은생교란작용을통해통기효과를 증대시키고용존된유기물질을수계내로공급하여저서환경을 개선시키는것으로알려져있다(Massin, 1982; Uthicke, 1999;
Yamada et al., 2009; Bellchambers et al., 2011). 이러한현상을 고려할때해삼출현밀도가높은지역에서산휘발성황화물의 농도가뚜렷하게높게나타나는현상이산휘발성황화물의농도 가높은지역을해삼이서식지로선호하기때문인지또는해삼 에의한다량의배설물등에의해농도가높아진것인지, 그렇 지않으면두경우와무관하게지역적인특성에의한것인지에 대해서는명확한판단을내릴수없으며, 이에대해서는추후보 다면밀한조사가이루어져야할것으로판단된다.
사 사
본연구는국립수산과학원수산생물종보존및복원연구와 태안군 해삼양식장적지조사 과제의일환으로 추진되었습니 다. 이연구의현장조사및시료채취에도움을준연안관리기술 연구소연구원들에게감사를드립니다.
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36˚45´N36˚30´N
8 Mean grain size (Unimode)
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8 6 4 2 0 -2
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Mean grain size (phi)Mean grain size (phi) 0 2Density (ind./m) COD (mg O/g-dry)Weight (g)WC (%)2
Station No.
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WCIL 8
6 4 2 0 -2
50 40 30 20 10 0
Mean grain size (phi)Density (ind./m2)
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y = 0.08x-0.21 r = 0.45 4
3
2
1
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Density (ind./m2)
AVS (mg S/g-dry)
y = 3.34x+0.17 r = 0.46 4
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1
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0.0 0.1 0.2 0.3 0.4
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