CSIR-National Institute of Oceanography, Regional Centre, Visakhapatnam, India.
CSIR-National Institute of Oceanography, Regional Centre, Kochi, India.
Environ Monit Assess. 2024 Jan 12;196(2):143. doi: 10.1007/s10661-023-12290-7.
This study investigates phytoplankton functional group variations in the western Bay of Bengal (WBoB) during the Spring Intermonsoon. Samples were collected from four cross-shore transects: Mahanadi (MN), Vamsadhara (VD), Godavari (GD), and Krishna (KS). East India Coastal Current and warm gyre influenced the southern transects (KS, GD), VD was experiencing moderate upwelling and MN was characterized by low salinity and oligotrophic conditions due to freshwater input. In response to hydrography, phytoplankton biomass and functional types differed within and between the transects. Chlorophyll-a (Chl-a) was spatially high in VD and low in MN. The subsurface Chlorophyll-a maxima (SSCM) was prominent and shallow in the MN and VD, compared to the southern transects. Total diagnostic pigments concentration was high in VD, followed by GD, KS and MN. Phytoplankton functional groups and each groups contribution to Chl-a was calculated through CHEmical Taxonomy (CHEMTAX). Diatoms and cyanophytes were the dominant functional types in the surface layers. Progressive shift from diatoms in the nearshore region to cyanophytes in the offshore was observed. The low saline and low-nutrient conditions were conducible for the growth of cyanophytes, while nutrient-rich optimum light layer of SSCM and upper layer of VD were favorable for diatoms. Cryptophytes contribution to Chl-a was higher in southern transects compared to the north. Prymnesiophytes and prasinophytes were high in the subsurface and deep layers could be due to their adaptions to light and nutrients. The present study highlights the significance of physical processes associated hydrography in structuring the phytoplankton functional types.
本研究调查了春季季风期间孟加拉湾西部(WBoB)浮游植物功能群的变化。样品取自四个沿岸横切带:马哈纳迪(MN)、瓦斯达哈(VD)、戈达瓦里(GD)和克里希纳(KS)。东印度沿岸流和暖旋流影响南部横切带(KS、GD),VD 经历中度上升流,MN 则因淡水输入而具有低盐度和贫营养条件。根据水文学特征,浮游植物生物量和功能类型在横切带内和之间存在差异。VD 区的叶绿素 a(Chl-a)空间分布较高,MN 区则较低。MN 和 VD 区的次表层叶绿素 a 最大值(SSCM)较为明显且较浅,而南部横切带则不然。VD 区的总诊断色素浓度较高,其次是 GD、KS 和 MN。浮游植物功能群及其对 Chl-a 的贡献通过 CHEmical Taxonomy(CHEMTAX)计算得出。在表层,硅藻和蓝藻是主要的功能类型。从近岸区域的硅藻到离岸区域的蓝藻逐渐占主导地位。低盐度和低营养条件有利于蓝藻的生长,而 SSCM 的富营养最佳光照层和 VD 的上层则有利于硅藻的生长。与北部相比,南部横切带的隐藻对 Chl-a 的贡献更高。在次表层和深层,颗石藻和甲藻的含量较高,这可能是由于它们对光和营养的适应。本研究强调了与水文学相关的物理过程在浮游植物功能类型结构中的重要性。