Lu Songhui, Ou Linjian, Dai Xinfeng, Cui Lei, Dong Yuelei, Wang Pengbin, Li Dongmei, Lu Douding
Research Center of Harmful Algae and Marine Biology, Jinan University, Guangzhou 510632, China; Southern Marine Science and Engineering Guangdong Laboratory, Zhuhai 519000, China.
Research Center of Harmful Algae and Marine Biology, Jinan University, Guangzhou 510632, China.
Harmful Algae. 2022 May;114:102207. doi: 10.1016/j.hal.2022.102207. Epub 2022 Feb 24.
Prorocentrum donghaiense Lu (also identified as Prorocentrum shikokuense Hada and Prorocentrum obtusidens Schiller) is a bloom-forming dinoflagellate species distributed worldwide. Blooms of P. donghaiense occur annually in adjacent waters of the East China Sea (ECS), especially in the waters near the Changjiang River Estuary. Blooms of this species have also been reported in nearby Japanese and Korean waters. There has been an apparent bloom-forming species succession pattern in the ECS since 2000, with diatom blooms in the early spring, shifting to long-lasting and large-scale dinoflagellate blooms dominated by P. donghaiense during the spring, and finally ended by diatom and/or Noctiluca scintillans blooms in summer. These bloom succession patterns were closely correlated with changes in environmental factors, such as temperature increase and anthropogenic eutrophication. Decreasing silicate by the construction of the Three Gorges Dam and increasing dissolved inorganic nitrogen flux were mainly influenced by high intensity human activities in the Changjiang River watershed, resulting in low Si/N ratio and high N/P ratios, possibly accelerating outbreak of P. donghaiense blooms. Phosphorous deficiency might be the most critical factor controlling the succession of microalgal blooms from diatoms to dinoflagellates. Prorocentrum donghaiense is a nontoxic species, but it can disrupt marine ecosystem by decreasing phytoplankton biodiversity and changing the structure of the food chain. Prorocentrum donghaiense blooms in the ECS have been intensively studied during the last two decades. Several possible mechanisms that contribute or trigger the annual blooms of this species have been proposed, but further research is required particularly on the aspect of nutrient budget, ecosystem impacts, as well as social-economic impact assessment.
东海原甲藻(也被鉴定为四国原甲藻和钝顶原甲藻)是一种能形成水华的甲藻物种,分布于全球。东海原甲藻水华每年在东海邻近海域出现,尤其是在长江口附近海域。在日本和韩国附近海域也有该物种水华的报道。自2000年以来,东海明显存在一种水华形成物种演替模式,早春为硅藻水华,春季转变为以东海原甲藻为主的持久且大规模的甲藻水华,最终在夏季以硅藻和/或夜光藻水华结束。这些水华演替模式与环境因素的变化密切相关,如温度升高和人为富营养化。三峡大坝建设导致硅酸盐减少以及溶解无机氮通量增加,主要受长江流域高强度人类活动影响,导致硅氮比低和氮磷比高,可能加速了东海原甲藻水华的爆发。磷缺乏可能是控制微藻水华从硅藻向甲藻演替的最关键因素。东海原甲藻是无毒物种,但它可通过降低浮游植物生物多样性和改变食物链结构来破坏海洋生态系统。在过去二十年中,对东海原甲藻水华进行了深入研究。已经提出了几种促成或引发该物种年度水华的可能机制,但尤其在营养收支、生态系统影响以及社会经济影响评估方面还需要进一步研究。