Tseng CM, Shen PY, Liu KK (2014) Synthesis of observed air-sea COTseng Y-F, Lin J, Dai MH et al (2013) Joint effect of freshwater plume and coastal upwelling on phytoplankton growth off the Changjiang River. Between late 1997 and mid-2008, satellites observed that warmer-than-average temperatures (red line) led to below-average chlorophyll concentrations (blue line) in these areas. Geophys Res Lett 33:L07610Gong G-C, Liu K-K, Chiang K-P et al (2011) Yangtze River floods enhance coastal ocean phytoplankton biomass and potential fish production. $E}k���yh�y�Rm��333��������:� }�=#�v����ʉe Estuar Coast Shelf Sci 71:3–12Li XA, Yu ZM, Song XX et al (2011) The seasonal characteristics of dissolved oxygen distribution and hypoxia in the Changjiang Estuary. Sci Total Environ 407(13):4012–4021Wang K, Chen JF, Jin HY et al (2011) The four seasons nutrients distribution in Changjiang River Estuary and its adjacent East China Sea (in Chinese with English abstract).
Sellner KG, Sellner SG, Lacouture RV et al (2001) Excessive nutrients select for dinoflagellates in the stratified Patapsco River estuary: Margalef reigns. In high latitudes, blooms peak in the spring and summer, when sunlight increases and the relentless mixing of the water by winter storms subsides. All our watersports: If its above water, on the water, or underwater, we do it. 0000002154 00000 n Wang WL, Chen JF, Jin HY et al (2009) The distribution characteristics and influence factors of some species phosphorus in waters of the Changjiang River Estuary in summer (in Chinese with English abstract). Zhou M-J, Shen Z-L, Yu R-C (2008) Responses of a coastal phytoplankton community to increased nutrient input from the Changjiang (Yangtze) River. Acta Oceanol Sin 26:96–106Office of Integrated Oceanographic Survey of China (OIOSC) (1964a) Dataset of the national integrated oceanographyic survey (in Chinese). Water Res 54:1–11Jiang ZB, Chen JF, Zhou F et al (2017) Summer distribution patterns of Jiang ZB, Li HL, Zhai HC (2018) Seasonal and spatial changes in Keeling RF, Körtzinger A, Gruber N (2010) Ocean Deoxygenation in a Warming World. J Mar Syst 154:15–27Liu SM, Zhang J, Chen HT et al (2003) Nutrients in the Changjiang and its tributaries. Ocean and seas or trees and plants? Mar Pollut Bull 125(1–2):440–450Chou W-C, Gong G-C, Cai W-J et al (2013) Seasonality of CODai ZJ, Du JZ, Zhang XL et al (2010) Variation of riverine material loads and environmental consequences on the Changjiang (Yangtze) Estuary in recent decades (1955–2008). Certain species of phytoplankton produce powerful biotoxins, making them responsible for so-called “red tides,” or harmful algal blooms.
Phytoplankton, like land plants, require nutrients such as nitrate, phosphate, silicate, and calcium at various levels depending on the species. Prog Oceanogr 159:237–254. Those conditions likely set the stage for large and persistent blooms of phytoplankton in the waters around the United Kingdom and Ireland. The Research and Media Team at Scotty's. Disclaimer: Phytoplankton can grow explosively over a few days or weeks. 0000001962 00000 n
Ocean Dynam 60:1293–1306Hsueh Y, Wang J, Chern CS (1992) The intrusion of the Kuroshio across the continental shelf northeast of Taiwan. If you want to know more about Oceans and Oxygen, take a look at some of our references below. Wu B, Jin HY, Gao SQ et al (2019) Nutrient Budgets and Recent Decadal Variations in a Highly Eutrophic Estuary: Hangzhou Bay. EndNote
Am Sci 46:205–221Rabouille C, Conley DJ, Dai MH et al (2008) Comparison of hypoxia among four river-dominated ocean margins: The Changjiang (Yangtze), Mississippi, Pearl, and Rhône rivers. As surface waters warm up through the summer, they become very buoyant. Hydrobiologia 563:313–328Chang KI, Zhang C-I, Park C et al (2015) Oceanography of the East Sea (Japan Sea). The most common kind of phytoplankton is the Hypoxia is relatively sporadic and patchy before 2013. Cont Shelf Res 28:1483–1489Zhu Z-Y, Zhang J, Wu Y et al (2011) Hypoxia off the Changjiang (Yangtze River) Estuary: oxygen depletion and organic matter decomposition. J Geophys Res 104(C9):20675–20686. (Illustration ©2010 Phytoplankton samples can be taken directly from the water at permanent observation stations or from ships.
Survey report of Chinese coastal plankton, BeijingRedfield AC (1958) The biological control of chemical factors in the environment.
E. huxleyi is an abundant species of coccolithophore. When the algae die, they become biomass for bacteria, which can lower the oxygen levels in an area of the ocean (or lake, as we witnessed in the Great Lakes this past summer), making it uninhabitable for other marine life.
J Coast Res 32:1081–1091Li MT, Xu KQ, Watanabe M et al (2007) Long-term variations in dissolved silicate, nitrogen, and phosphorus flux from the Yangtze River into the East China Sea and impacts on estuarine ecosystem. For example, excessive blooms can cause oxygen depletion at night and result in massive plankton and aquatic life die-offs. Mendeley He XQ, Bai Y, Pan DL et al (2013) Satellite views of the seasonal and interannual variability of phytoplankton blooms in the eastern China seas over the past 14 years (1998–2011).
They are abundant in cold, nutrient rich waters where they form the base of the food web, and are an extremely diverse and varied group of organisms. (Illustration adapted from Worldwide, this “biological carbon pump” transfers about 10 gigatonnes of carbon from the atmosphere to the deep ocean each year. (Graph adapted from Over the past decade, scientists have begun looking for this trend in satellite observations, and early studies suggest there has been a small decrease in global phytoplankton productivity. 0000001405 00000 n
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