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Variations of colored dissolved organic matter in the Mandovi Estuary, Goa during spring inter-monsoon: A comparison with COVID-19 outbreak imposed lockdown period
Frontiers in Marine Science ( IF 2.8 ) Pub Date : 2021-04-29 , DOI: 10.3389/fmars.2021.638583
Albertina Dias , Siby Kurian , Suresh Thayapurath , Anil K. Pratihary

Colored dissolved organic matter (CDOM) is one of the important fractions of dissolved organic matter (DOM) that controls the availability of light in water and plays a crucial role in the cycling of carbon. High CDOM absorption in the Mandovi Estuary (Goa) during spring inter-monsoon (SIM) is largely driven by both in-situ production and anthropogenic activities. Here we presented the CDOM variation in the estuary during SIM of 2014 to 2018 and compared it with that of 2020 when the COVID-19 outbreak imposed lockdown was implemented. During 2020, low CDOM absorption was observed at the mid-stream of the estuary as compared to the previous years, which could be attributed to low autochthonous production and less input from anthropogenic activities. On the other hand, high CDOM observed at the mouth during 2020 is linked to the autochthonous production, as seen from the high concentrations of chlorophyll a. High CDOM in the upstream region could be due to both autochthonous production and terrestrially derived organic matter. Sentinel- 2 satellite data was also used to look at the variations of CDOM in the study region which is consistent with in-situ observations. Apart from this, the concentration of nutrients (NO3-, NH4+ and SiO44-) in 2020 was also low compared to the previous reports. Hence, our study clearly showed the impact of anthropogenic activities on CDOM build-up and nutrients, as the COVID-19 imposed lockdown drastically controlled such activities in the estuary.

中文翻译:

春季季风之间果阿曼多维河口有色溶解有机物的变化:与COVID-19爆发施加的锁定期比较

有色溶解有机物(CDOM)是溶解有机物(DOM)的重要组成部分之一,它控制水中的光的利用率,并在碳循环中起关键作用。春季季风(SIM)期间,曼多维河口(Goa)对CDOM的高吸收很大程度上是由原位生产和人为活动共同驱动的。在这里,我们介绍了2014年至2018年SIM在河口的CDOM变化,并将其与2020年实施COVID-19暴发实施封锁的2020年进行了比较。在2020年期间,与前几年相比,河口中游观测到的CDOM吸收较低,这可能归因于本地生物产量低和人为活动投入少。另一方面,从高浓度的叶绿素a可以看出,在2020年期间在口中观察到的高CDOM与本地生产有关。上游地区的高CDOM可能是由于自生产物和陆生有机质造成的。Sentinel-2卫星数据还用于查看研究区域中CDOM的变化,这与原位观测一致。除此之外,与以前的报告相比,2020年的营养素(NO3-,NH4 +和SiO44-)浓度也很低。因此,我们的研究清楚地表明了人为活动对CDOM积累和养分的影响,因为COVID-19施加的锁定作用在河口大幅度地控制了此类活动。上游地区的高CDOM可能是由于自生产物和陆生有机质造成的。Sentinel-2卫星数据还用于查看研究区域中CDOM的变化,这与原位观测一致。除此之外,与以前的报告相比,2020年的营养素(NO3-,NH4 +和SiO44-)浓度也很低。因此,我们的研究清楚地表明了人为活动对CDOM积累和养分的影响,因为COVID-19施加的锁定作用在河口大幅度地控制了此类活动。上游地区的高CDOM可能是由于自生产物和陆生有机质造成的。Sentinel-2卫星数据还用于查看研究区域中CDOM的变化,这与原位观测一致。除此之外,与以前的报告相比,2020年的营养素(NO3-,NH4 +和SiO44-)浓度也很低。因此,我们的研究清楚地表明了人为活动对CDOM积累和养分的影响,因为COVID-19施加的锁定作用在河口大幅度地控制了此类活动。与以前的报告相比,2020年的NH4 +和SiO44-)也较低。因此,我们的研究清楚地表明了人为活动对CDOM积累和养分的影响,因为COVID-19施加的锁定作用在河口大幅度地控制了此类活动。与以前的报告相比,2020年的NH4 +和SiO44-)也较低。因此,我们的研究清楚地表明了人为活动对CDOM积累和养分的影响,因为COVID-19施加的锁定作用在河口大幅度地控制了此类活动。
更新日期:2021-04-29
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