南方水产科学
南方水產科學
남방수산과학
South China Fisheries Science
2015年
5期
38-46
,共9页
戴明%巩秀玉%刘华雪%廖秀丽%齐占会%黄洪辉
戴明%鞏秀玉%劉華雪%廖秀麗%齊佔會%黃洪輝
대명%공수옥%류화설%료수려%제점회%황홍휘
南沙海域%网采浮游植物%水团%冗余分析
南沙海域%網採浮遊植物%水糰%冗餘分析
남사해역%망채부유식물%수단%용여분석
Nansha area%net phytoplankton%water masses%redundancy analysis
根据2013年春季调查资料研究了南沙海域不同水团中网采浮游植物的群落特征。共鉴定网采浮游植物4门62属222种,其中硅藻门和甲藻门种类数分别占67.1%和31.1%。浮游植物平均丰度为(16655±36570)个· m-3,硅藻门平均丰度占93.6%。浮游植物多样性指数( H′)和均匀度指数( J′)平均分别为4.43和0.85。巴拉巴克海峡西侧混合水受苏禄海表层入侵水及冷涡影响,跃层浅,营养盐浓度高,浮游植物种类数和丰度均最高。巽他陆架北缘沿岸混合水受局部上升流的影响,浮游植物丰度次之。中南半岛沿岸混合水中无机氮( DIN)浓度最低,浮游植物种类数和丰度均低,而固氮蓝藻的丰度比例却最高。南沙中央表层水受陆源物质影响小,跃层深且薄,75 m以浅水层硅酸盐浓度最低,浮游植物丰度较低,但甲藻门丰度比例最高, J′最高,浮游植物丰度最低值出现在暖涡区域。
根據2013年春季調查資料研究瞭南沙海域不同水糰中網採浮遊植物的群落特徵。共鑒定網採浮遊植物4門62屬222種,其中硅藻門和甲藻門種類數分彆佔67.1%和31.1%。浮遊植物平均豐度為(16655±36570)箇· m-3,硅藻門平均豐度佔93.6%。浮遊植物多樣性指數( H′)和均勻度指數( J′)平均分彆為4.43和0.85。巴拉巴剋海峽西側混閤水受囌祿海錶層入侵水及冷渦影響,躍層淺,營養鹽濃度高,浮遊植物種類數和豐度均最高。巽他陸架北緣沿岸混閤水受跼部上升流的影響,浮遊植物豐度次之。中南半島沿岸混閤水中無機氮( DIN)濃度最低,浮遊植物種類數和豐度均低,而固氮藍藻的豐度比例卻最高。南沙中央錶層水受陸源物質影響小,躍層深且薄,75 m以淺水層硅痠鹽濃度最低,浮遊植物豐度較低,但甲藻門豐度比例最高, J′最高,浮遊植物豐度最低值齣現在暖渦區域。
근거2013년춘계조사자료연구료남사해역불동수단중망채부유식물적군락특정。공감정망채부유식물4문62속222충,기중규조문화갑조문충류수분별점67.1%화31.1%。부유식물평균봉도위(16655±36570)개· m-3,규조문평균봉도점93.6%。부유식물다양성지수( H′)화균균도지수( J′)평균분별위4.43화0.85。파랍파극해협서측혼합수수소록해표층입침수급랭와영향,약층천,영양염농도고,부유식물충류수화봉도균최고。손타륙가북연연안혼합수수국부상승류적영향,부유식물봉도차지。중남반도연안혼합수중무궤담( DIN)농도최저,부유식물충류수화봉도균저,이고담람조적봉도비례각최고。남사중앙표층수수륙원물질영향소,약층심차박,75 m이천수층규산염농도최저,부유식물봉도교저,단갑조문봉도비례최고, J′최고,부유식물봉도최저치출현재난와구역。
Based on the samples collected in Nansha area in spring,2013,we investigated the net phytoplankton community in order to de-termine the effects of water masses on their distribution. A total of 222 species,belonging to 62 genera of 4 phyla,were identified. Bacillari-ophyta and Pyrrophyta accounted for 67. 1% and 31. 1% in species number,respectively. The average abundance of net phytoplankton was (16 655 ± 36 570)cell·m-3. Bacillariophyta accounted for 93. 6% in abundance. The average diversity index and evenness index of net phy-toplankton were 4. 43 and 0. 85. The species number and abundance of net phytoplankton were the highest in the mixed waters in the west of Balabac Strait,characterized by shallow thermocline and high nutrient concentrations resulting from the intrusion of Sulu Sea waters and the appearance of a clod eddy. In the mixed waters in the north edge of the Sunda Shelf,the abundance of net phytoplankton was sub-high due to the influence of upwelling. In the mixed waters from coast of the Indo-China Peninsula with low inorganic nitrogen,the species number and abundance of net phytoplankton were low,but the percentage of Cyanophyta increased to the maximum. In the Nansha central surface waters with less terrigenous matter,deep and thin thermocline,the lowest silicate concentration occurred at 0~75 m,the average abun-dance of net phytoplankton was low,but the percentage of Pyrrophyta increased to the maximum,and the average evenness index of net phy-toplankton was the highest,while the lowest abundance of net phytoplankton appeared in the warm eddies.