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Cultural eutrophication is the result of releasing large amounts of nutrients into rivers and lakes. doi: 10.5194/bg-15-3975-2018, Jørgensen, B. Although these episodes tend to occur following increases in river runoff, and mucilage production occurs during diatom blooms (McKinney, 2007), anthropogenic nutrient enrichment may not be directly responsible (Degobbis et al., 2005). Syst. Impacts of increasing dissolved inorganic nitrogen discharged from Changjiang on primary production and seafloor oxygen demand in the East China Sea from 1970 to 2002. Global nitrogen and phosphate in urban wastewater for the period 1970 to 2050. Chin. Jr, Degobbis, D., and Precali, R. (1999). (2012). Mar. Water residence time in Chesapeake Bay for 1980–2012. Since 1983, annual riverine inputs of DIN have fluctuated between ∼ 0.6 × 109 kg yr–1 in 2000 and ∼ 1.8 × 109 kg yr–1 in 1993. doi: 10.1016/j.hal.2008.08.017, Anderson, D. M., Glibert, P. M., and Burkholder, J. M. (2002). Environ. 148, 1–13. “Dead zones: Oxygen depletion in coastal ecosystems,” in World Seas: An Environmental Evaluation, ed. Biogeosciences 8, 1881–1899. 20, 452–457. Estuar. Examples include the following: (i) Recycle animal manure to cropland within watersheds has been shown to be an effective BMP that substantially reduces nutrient runoff (Strokal et al., 2020); (ii) Restore critical habitats (seagrass meadows, coral reefs, oyster reefs, mangrove forests and salt-marshes) to remove nutrients, increase sequestration of organic matter in benthic sediment, and increase rates of denitrification; (iii) Establish sustainable macroalgal and bivalve aquaculture systems to remove excess N and P (Burkholder and Shumway, 2011; Kellogg et al., 2014; Duarte and Krause-Jensen, 2018; Theuerkauf et al., 2019a, b; Kotta et al., 2020); and. Estuar. It is generally agreed that N is the primary cause of eutrophication in most coastal ecosystems2 (Howarth and Marino, 2006; Paerl, 2018). (Ed.) doi: 10.1016/j.jmarsys.2014.08.001, Dong, Z., Liu, D., and Keesing, J. K. (2010). Where can the world’s purest water be found? 15, 1303–1317. Bottom water hypoxia now covers > 15% of the ECS making it one of the largest coastal hypoxic zones in the world (Chen et al., 2007; Wang et al., 2016; Zhu et al., 2016). Dugdale, R. C., and Goering, J. J. A., Waters, T. J., Wickliffe, L. C., Alleway, H. K., and Jones, R. C. (2019b). Acad. 214, 1–14. doi: 10.1016/j.jmarsys.2015.05.002, Zhu, Z.-Y., Zhang, J., Wu, Y., Zhang, Y.-Y., Lin, J., and Liu, S.-M. (2011). doi: 10.1016/b978-0-12-805052-1.00021-8, Altieri, A. H., and Gedan, K. B. A conceptual framework for selecting environmental indicator sets. The high phytoplankton biomass (red – high, blue – low) footprint of the coastal plume of the Po River in the northern Adriatic Sea. Lakes receive inputs of nutrients and silt from the surrounding land basin as a result of natural erosion and runoff. 19, 1975–1988. in the East China Sea – Potential role of Taiwan Warm Current in bloom initiation. Francé, J., and Mozetič, P. (2006). (2009). For the most part, summer blooms are confined to the euphotic zone and there is relatively little sedimentation to the benthos. doi: 10.1073/pnas.1619575114, Goldewijk, K. K., Beusen, A., van Drecht, G., and de Vos, M. (2011). ecosystem to survive and respire. Rev. 128. Harding, L. W. Jr., Mallonee, M. E., Perry, E. S., Miller, W. D., Adolf, J. E., Gallegos, C. L., and Paerl, H. W. (2019). Reconstructing the development of Baltic Sea eutrophication 1850–2006. Has eutrophication promoted forage fish production in the Baltic Sea? 38, 129–145. Shen, J., and Wang, H. V. (2007). The first detection of bivalves contaminated by toxins produced by a bloom of Alexandrium minutum that cause paralytic shellfish poisoning (PSP) was in 1994 (Honsell et al., 1996). (2019). (2011). The framework is conceptualized in terms of (1) anthropogenic pressures on ecosystem support services that (2) are uniquely modulated by each ecosystem as they perturb (3) ecosystem support services (states), changes in which impact (4) regulating and provisioning services. The hypoxic region north of 30° N is dominated by Changjiang inputs, with its N loads supporting 74% of oxygen consumption; south of 30°N, oceanic nitrogen sources become more important, supporting 39% of oxygen consumption during the hypoxic season, but the Changjiang remains the main control on hypoxia formation also in this region (Große et al., 2020). doi: 10.3354/meps009203, O’Higgins, T., Tett, P., Farmer, A., Cooper, P., Dolch, T., Friedrich, et al. Harmful Algae 4, 525–531. Data 9, 181–192. Nature 490, 388–392. Mills, C. E. (2001). Educate the masses and raise awareness regarding cultural Selman, M., and Greenhalgh, S. (2010). 1, 349–360. Biogeosciences 17, 2701–2714. 5, 243–264. have restrictions regarding the concentration of phosphates that should be in doi: 10.1016/j.ecss.2015.05.032. In 2013, southern Asia accounted for 71% of global fertilizer use, followed by North America (11%), Europe (7%), and South America (6%) (Lu and Tian, 2017). Shelf Sci. J. Mar. Earth Syst. Interannual variations (1998–2007) in the spatial extent of high Chl are driven by variations in river discharge (Xiuren et al., 1988; Kim et al., 2009). Pollut. Pollut. A number of water filtration systems could help you out in Oceans 121, 8395–8416. Ambio 41, 534–548. Ser. Glibert, P. M., Manager, R., Sobota, D. J., and Bouwman, L. (2014). Cultural eutrophication is the Earth's most widespread water quality problem. Overview of Cultural Eutrophication. Coastal upwelling centers represent an extreme case of natural new nutrient inputs and are expected to exhibit equally extreme blooms of both benign and toxic phytoplankton (Kudela et al., 2010). Phytoplankton biomass is correlated with the riverine supply of N (Fennel et al., 2011), and the annual cycle of phytoplankton biomass is characterized by a spring maximum and an autumn minimum (Bode and Dortch, 1996; Gomez et al., 2018). Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge: Cambridge University Press. 94, 239–252. Cultural eutrophication is the process that speeds up natural eutrophication because of human activity. doi: 10.1016/j.csr.2011.08.010, Crutzen, P. J. European Assessment of Eutrophication Abatement Measures Across Land-Based Sources, Inland, Coastal and Marine Waters. Ecol. BioScience 56, 987–996. It is important to emphasize that these impacts should be viewed in the context of their spatial extent relative to the size of the ecosystem as a whole. Mar. A comparison of 30 coastal ecosystems worldwide shows that when the spatial extent of bottom water hypoxia is < 20% of the ecosystem’s area, fish landings per unit N loading (kg wet weight per kg N) range between 0.1 and 2.1, but when spatial extent was > 20%, landings per N loading were consistently < 0.5 (Breitburg et al., 2009). (2019). B., and Icely, J. Summer bottom water hypoxia has been documented in the mesohaline salinity zone throughout the twentieth century and, while interannual variability is substantial, the volume of hypoxia has increased significantly since WWII as anthropogenic N loading to the Bay increased (Brush, 2009; Murphy et al., 2011; Li et al., 2016; Testa et al., 2017). Phytoplankton production is both the foundation of most marine food webs that support provisioning services and a source of excess organic matter that often leads to coastal eutrophication. These nutrients are needed for photosynthesis. (2019), made the following recommendations to address the ongoing eutrophication problem: (i) Changes in ecological status must be monitored and assessed more effectively; (ii) Management actions must account for the effects of multiple stressors; (iii) Management targets of the Water Framework Directive (WDF)35 need to acknowledge long-term recovery time-scales; (iv) Water resource protection must be mainstreamed into other policy instruments; and. The ECS has an area of ∼750,000 km2, 75% of which is < 200 m deep. Environ. doi: 10.5194/essd-9-667-2017, Zhang, F., Cui, Z., Chen, X., Ju, X., Shen, J., Chen, Q., et al. Change Biol. Influence of river flow and nutrient loading on selected ecosystem processes: A synthesis of Chesapeake Bay data, in Estuarine Science: A Synthetic Approach to Research and Practice, Ed. At its maximum extent, the spatial extent of hypoxia is the largest anthropogenically enhanced hypoxic zone in the world (Schmale et al., 2016). Current state, scales of variability and decadal trends of biogeochemical properties in the Northern Adriatic Sea. J. Oceanogr. 68, 159–169. Change Biol. Ser. Atmospheric deposition is distributed over the entire ECS (Zhang et al., 2019). J. Plankton Res. photosynthetic organisms, but the species which depend on them for oxygen. 24, 115–139. J. “Bloom dynamics and physiology of Gymnodinium breve, with emphasis on the Gulf of Mexico,” in Physiological Ecology of HarmfulAlgal Blooms, eds E. M. Anderson, A. D. Cembella, and G. M. Hallengraff (New York, NY: Springer), 135–153. being carried out, no oxygen is being produced that may help the fishes of the Although N supply typically limits the magnitude of seasonal phytoplankton blooms in coastal ecosystems, both P and N inputs should be managed since P has been found to be the primary limiting nutrient in some coastal ecosystems (e.g., the NA), and managing only N without managing P inputs can lead to decreases in N:P ratios, increases in N-fixation, and toxic blooms of cyanobacteria (Conley et al., 2009; Glibert et al., 2014; Paerl et al., 2016; Glibert and Burford, 2017). 150, 143–155. N input via N-fixation by cyanobacteria is estimated to be ∼ 0.40 × 109 kg N yr–1 (Olofsson et al., 2020), nearly equivalent to riverine inputs. Agroecosyst. Ambio 39, 49–58. (ii) Combustion of Fossil Fuels – Emissions from the combustion of fossil fuels release an estimated 25–40 × 109 kg N yr–1 (Penuelas et al., 2013) with Asia, Europe, North America and Sub-Saharan Africa accounting for 30, 20, 17, and 12% of emissions, respectively (Lamsal et al., 2011). Report 96:4113. doi: 10.3133/wri964113, Eero, M., Andersson, H. C., Almroth-Rosell, E., and MacKenzie, B. R. (2016). Hoagland, P. and Scatasta, S. (2006). 31, 1881–1893. Serv. J. Mar. Alerts due to the presence of biotoxins in the Gulf of Trieste increased steadily from 10 yr–1 in 2005 to 60 yr–1 in 2010 and then declined to 1 yr–1 in 2013 and 2014 (Lipizer et al., 2017). Oceanogr. A progressive increase in eutrophication began in the early 20th C, continued to ∼ 1978, and subsequently began to decrease (Sangiorgi and Donders, 2004). An indication of the significance of the latter is the observation that dissolved oxygen in nearshore bottom water (within 10 km of the shoreline) has declined by up to four times faster than reported for more offshore waters over the last 15 years (Booth et al., 2014). 66, 1528–1537. doi: 10.1016/j.gca.2012.12.038, Dalsgaard, T., Thamdrup, B., and Canfield, D. E. (2005). Ambio 44 (Suppl. “Dead zones: a future worst-case scenario for Northern Adriatic biodiversity,” in CIESM Workshop Monographs, No. Ecol. 353, 126–138. The HYDE 3.1 spatially explicit database of human-induced global land-use change over the past 12,000 years. Most scientists agree that it is largely caused by increasing inputs of phosphorus and nitrogen . unfortunate demise. (2012). Estuaries 24, 875–883. Nat. (2004). Estuaries 24, 481–490. Stratification has strengthened in the Baltic Sea – An analysis of 35 years of observational data. Spatial and temporal distribution of sea surface salinity in coastal waters of China based on Aquarius. Millennium Ecosystem Assessment. doi: 10.1007/978-3-319-70069-4_12, Glibert, P. M., and Burford, M. A. Direzione Regionale dell’ Ambiente Trieste 0, 178. In the other 90%: phytoplankton responses to enhanced nutrient availability in the Great Barrier Reef Lagoon. Recent trends towards oligotrophication of the northern Adriatic: evidence from chlorophyll a time series. Microbiol. Proc. As a result, it is estimated that the spatial extent of seagrass decreased by 46% between the 1930s and the 1990s (Kemp et al., 2005). doi: 10.1007/bf02804899, Paerl, H. W., Hall, N. S., Hounshell, A. G., Luettich, R. A. Jr., Rossignol, K. L., Osburn, C. L., et al. These poisonous substances include hydrogen sulfide and However, the relative magnitude of direct atmospheric deposition to coastal ecosystems varies from ∼5% in waters most heavily impacted by river borne inputs (e.g., the northern Gulf of Mexico) to ≥ 30% in waters with relatively low river borne inputs (e.g., Baltic, western Mediterranean, mid-Atlantic and northeast U.S.-Canadian Atlantic coastal regions) (Paerl et al., 2002; Spokes and Jickells, 2005). Res. Factories are essential for countries to consistently produce consumer products for local…, The Tasmanian devil (Sarcophilus harrisii) belongs to the family of Dasyuridae. Bull. doi: 10.1007/bf02179829, Seitzinger, S. P., Mayorga, E., Bouwman, A. F., Kroeze, C., Beusen, A. H. W., Billen, G., et al. It is mainly caused by increased nutrient input into a water body. doi: 10.1007/s13280-016-0788-3, Ekstrom, J. HELCOM (2018b). Human-induced eutrophication of freshwaters, also called cultural eutrophication, is largely a result of increased phosphorus inputs from sources such as agricultural fertilizers or partially treated sewage. Ser. The cultural eutrophication process consists of a continuous increase in the contribution of nutrients, mainly nitrogen and phosphorus (organic load) until it exceeds the capacity of the water body (i.e. doi: 10.1007/s10750-015-2320-3, Swaney, D. P., Hong, B., Ti, C., Howarth, R. W., and Humborg, C. (2012). Nat. Prog. M. L. Pace & P. M. Groffman (Editors), Springer Verlag, NY. Intergovernmental Oceanographic Commission. Coasts 30, 791–801. Sci. Portugal. doi: 10.1016/j.ecss.2014.05.027, Wang, B., and Wang, X. Diaz, R. J., and Rosenberg, R. (1995). doi: 10.1371/journal.pone.0118571. 115:C08028. 5, 451–456. The jellyfish joyride: causes, consequences and management responses to a more gelatinous future. doi: 10.1029/2007GL030474, Hieronymus, J., Eilola, K., Hieronymus, M., Meier, H. E. M., Saraiva, S., and Karlson, B. doi: 10.1093/plankt/18.12.2251. Sci. Nutrients, eutrophication and harmful algal blooms along the freshwater to marine continuum. 1, 329–349. Biogeogr. Today, agriculture is responsible for over 75% of the NH3 emissions in the United States and Canada, with animal production accounting for > 70% (Aneja et al., 2001; Bittman and Mikkelsen, 2009). Estuar. eutrophication. doi: 10.1021/acs.est.6b02575, Parsons, M. L., and Dortch, Q. Special Publ. USA: long-term observations suggest a regime shift. Copyright © 2020 Malone and Newton. Mar. Bergström, L., Karlsson, M., Bergström, U., Pihl, L., and Kraufvelin, P. (2019). Mar. Populations of red tide forming dinoflagellate Noctiluca scintillnas (McCartney): a comparison between the Black Sea and the northern Adriatic Sea. 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