Human impact on marine life

Different activities carried out and caused by human beings such as global warming, ocean acidification, and pollution affect marine life and its habitats.

[4] With coral producing materials such as carbonate rock and calcareous sediment, this creates a unique and valuable ecosystem not only providing food/homes for marine creatures but also having many benefits for humans too.

[13] Significant habitat loss is occurring particularly in seagrass meadows, mangrove forests and coral reefs, all of which are in global decline due to human disturbances.

[14][15] Coral reefs are microbially driven ecosystems that rely on marine microorganisms to retain and recycle nutrients in order to thrive in oligotrophic waters.

However, these same microorganisms can also trigger feedback loops that intensify declines in coral reefs, with cascading effects across biogeochemical cycles and marine food webs.

[17] The most pressing threat to kelp forests may be the overfishing of coastal ecosystems, which by removing higher trophic levels facilitates their shift to depauperate urchin barrens.

The invasive freshwater zebra mussels, native to the Black, Caspian, and Azov seas, were probably transported to the Great Lakes via ballast water from a transoceanic vessel.

[21] Meinesz believes that one of the worst cases of a single invasive species causing harm to an ecosystem can be attributed to a seemingly harmless jellyfish.

Mnemiopsis leidyi, a species of comb jellyfish that spread so it now inhabits estuaries in many parts of the world, was first introduced in 1982, and thought to have been transported to the Black Sea in a ship's ballast water.

[23] Marine pollution occurs when substances used or spread by humans, such as industrial, agricultural and residential waste, particles, noise, excess carbon dioxide or invasive organisms enter the ocean and cause harmful effects there.

Air pollution is also a contributing factor by carrying off iron, carbonic acid, nitrogen, silicon, sulfur, pesticides or dust particles into the ocean.

Nutrients and fertilizers from residential properties and impervious surfaces can be picked up in stormwater, which then runs into nearby rivers and streams that eventually lead to the ocean.

[34] Larger plastic waste can be ingested by marine species, filling their stomachs and leading them to believe they are full when in fact they have taken in nothing of nutritional value.

Ship and boat propellers and engines, industrial fishing, coastal construction, oil drilling, seismic surveys, warfare, sea-bed mining and sonar-based navigation have all introduced noise pollution to ocean environments.

[55] The Antarctic oscillation (also called the Southern Annular Mode) is a belt of westerly winds or low pressure surrounding Antarctica which moves north or south according to which phase it is in.

[66] The IPCC (2019) says marine organisms are being affected globally by ocean warming with direct impacts on human communities, fisheries, and food production.

[68] A 2020 study reports that by 2050 global warming could be spreading in the deep ocean seven times faster than it is now, even if emissions of greenhouse gases are cut.

[74] Coral, important for bird and fish life, also needs to grow vertically to remain close to the sea surface in order to get enough energy from sunlight.

[78][79] Human activities, such as dam building, can prevent natural adaptation processes by restricting sediment supplies to wetlands, resulting in the loss of tidal marshes.

Research in the past decade has transformed this view, demonstrating the existence of uniquely adapted microbial communities, high rates of biogeochemical/physical weathering in ice sheets and storage and cycling of organic carbon in excess of 100 billion tonnes, as well as nutrients.

The release of nitrogen oxides (N2O, NO) from anthropogenic activities and oxygen-depleted zones causes stratospheric ozone depletion leading to higher UVB exposition, which produces the damage of marine life, acid rain and ocean warming.

Pteropods are severely affected because increasing acidification levels have steadily decreased the amount of water supersaturated with carbonate which is needed for the aragonite creation.

[109] Likewise corals,[110] coralline algae,[111] coccolithophores,[112] foraminifera,[113] as well as shellfish generally,[114] all experience reduced calcification or enhanced dissolution as an effect of ocean acidification.

The dominance of non-siliceous phytoplankton due to anthropogenic nitrogen and phosphorus loading and enhanced silica dissolution in warmer waters has the potential to limit silicon ocean sediment export in the future.

[128] Marine environments are the blue frontier of a strategy for novel carbon sinks in post-Paris climate governance, from nature-based ecosystem management to industrial-scale technological interventions in the Earth system.

Wetlands, coasts, and the open ocean are being conceived of and developed as managed carbon removal-and-storage sites, with practices expanded from the use of soils and forests.

According to the study: "A third of fish stocks are operated beyond biologically sustainable levels and an estimated 30–50% of critical marine habitats have been lost owing to human industrialization".

When the data was added to previously existing information about ships that were publicly tracked, this led to several discoveries including: The study discovered a significant increase in offshore wind turbins which had overpassed oil platforms by number already in 2021.

But the unintended consequences of these well-intentioned actions — climate change, biodiversity loss, inadequate water supplies, and much else — could well make tomorrow the worst of times."

Areas that swarmed with a particular species hundreds of years ago may have experienced long-term decline, but it is the level a few decades previously that is used as the reference point for current populations.

Global cumulative human impact on the ocean [ 1 ] [ 2 ]
Fishing down the foodweb . Overfishing of high trophic fish like tuna can result in them being replaced by low trophic organisms, like jellyfish .
Relationship between annual trend and current cumulative impacts for different marine ecosystems [ 1 ]
A cargo ship pumps ballast water over the side.
Mnemiopsis leidyi
Microorganisms and climate change in marine and terrestrial biomes [ 47 ]
Overview of climatic changes and their effects on the ocean [ 48 ]
Global mean land-ocean temperature change from 1880 to 2011, relative to the 1951–1980 mean. Source: NASA GISS .
Most heat energy from global warming goes into the ocean. [ 49 ]
Global heat accumulation data, from Nuccitelli et al. (2012) [ 54 ] [ 50 ]
Between 1993 and 2018, the mean sea level has risen across most of the world ocean (blue colors). [ 71 ]
Thermohaline circulation , the ocean conveyor belt
Surface salinity changes measured by the NASA Aquarius satellite instrument from December 2011 to December 2012. Blue: low salinity, red: high salinity.
Potential impacts of ocean acidification. An overview of the potential upcoming ecological and biogeochemical consequences, linking different environmental drivers, processes, and cycles related to acidification in the future ocean. [ 87 ]
Estimated change in sea water pH caused by human created CO
2
from the start of the industrial revolution to the end of the twentieth century
Climate change causes sea ice to melt, transforming the Arctic from an icy desert into an open ocean. Polar bears and seals may lose their habitats, phytoplankton growth may increase and fuel the Arctic food web , which may lead to higher carbon burial rates and possibly decrease the amount of CO 2 in the atmosphere. [ 103 ]
Carbon stores and fluxes in present-day ice sheets (2019), and the predicted impact on carbon dioxide (where data exists). Estimated carbon fluxes are measured in Tg/a (megatonnes of carbon per year) and estimated sizes of carbon stores are measured in Pg C (thousands of megatonnes of carbon). DOC = dissolved organic carbon , POC = particulate organic carbon . [ 105 ]
Anthropogenic effects on the marine nitrogen cycle [ 106 ]
Video summarizing impacts of ocean acidification – Source: NOAA
Anthropogenic changes in the global carbon cycle 2009–2018. Schematic representation of the overall perturbation of the global carbon cycle caused by anthropogenic activities, averaged globally for the decade 2009–2018. See legends for the corresponding arrows and units. The uncertainty in the atmospheric CO2 growth rate is very small (±0.02 GtC yr−1) and is neglected for the figure. The anthropogenic perturbation occurs on top of an active carbon cycle, with fluxes and stocks represented in the background [ 123 ] for all numbers, with the ocean gross fluxes updated to 90 GtC yr−1 to account for the increase in atmospheric CO2 since publication. The carbon stocks in coasts are from a literature review of coastal marine sediments. [ 124 ] [ 125 ]
Nitrogen–carbon–climate interactions. Shown are the main interacting drivers during the Anthropocene. Signs indicate an increase (+) or a decrease (−) in the factor shown; (?) indicate an unknown impact. Colors of the arrow indicate direct anthropogenic impacts (red) or natural interactions (blue, many of which also modified by human influence). Strength of the interaction is expressed by the arrow thickness. [ 126 ] [ 127 ]
Proposed marine carbon dioxide removal options [ 128 ]
Ecosystem impacts amplified by ocean warming and deoxygenation. Drivers of hypoxia and ocean acidification intensification in upwelling shelf systems. Equatorward winds drive the upwelling of low dissolved oxygen (DO), high nutrient, and high dissolved inorganic carbon (DIC) water from above the oxygen minimum zone . Cross-shelf gradients in productivity and bottom water residence times drive the strength of DO (DIC) decrease (increase) as water transits across a productive continental shelf . [ 131 ] [ 132 ]
Multiple stressors acting on coral reefs [ 141 ]
Drivers of change in marine ecosystems [ 146 ]