Climate change is turning coastal lagoons into ‘salty soup’

The impacts of human activity and climate change are coalescing to make coastal lagoons saltier, changing the microbial life they support and the function they play in their ecosystems, according to new University of ޲Ʊ research.

Birds flocking beneath the dunes of the Coorong, a coastal lagoon in South Australia. Darcy Whittaker CC-BY

Birds flocking beneath the dunes of the Coorong, a coastal lagoon in South Australia. Credit: Darcy Whittaker, CC-BY.

Coastal lagoons are critical ecosystems that provide essential habitats and ecosystem services, including carbon sequestration, nutrient cycling, and fisheries support.

“Under normal conditions, lagoons act as nurseries for fish and crustaceans, they are internationally important feeding grounds for migratory birds, and they protect coasts from storm surges,” says the University’s Dr Chris Keneally.

“Their microbial makeup is what makes this happen, recycling nutrients and fostering this high productivity, allowing diverse plant and animal life to flourish.

“However, a single hot, dry summer, like the one we have recently experienced, can completely shift this important habitat into a salty, green soup, leading to the microbes becoming less diverse and those that are salt-tolerant becoming more dominant.

“Key processes, such as nitrification, de-nitrification, and carbon cycling are then disrupted, altering nutrient retention, organic matter decomposition, and greenhouse gas emissions.”

The trend of hypersalinity in coastal lagoons is global, occurring most often in arid and semi-arid coastal lagoons, such as those in Australia, the Mediterranean and the Persian Gulf. The phenomenon has accelerated in Australia over the last 40 years.

A global map of representative coastal lagoons with salinity above seawater. Background colours depict the Köppen-Geiger climate classification between 1991 and 2020

A global map of representative coastal lagoons with salinity above seawater. Background colours depict the Köppen-Geiger climate classification between 1991 and 2020. ().

“The rise in salinity can be attributed to elevated temperatures, enhanced evaporation, reduced rain and freshwater inputs, and rising sea levels,” says Dr Keneally, whose recent study was published in .

“Human factors such as upstream water diversions, urbanisation and development, and groundwater depletion also reduce freshwater inflow to coastal lagoons.

“We can mitigate the impacts of these activities by restoring environmental flows. Allocating water for the environment can maintain lagoon flushing, and nutrient runoff can be reduced by upgrading wastewater plants, re-establishing wetlands, and increasing efforts to retain nutrients in our agricultural lands throughout catchments worldwide.

“To buffer the effects of drought or sea‑level rise, we could also re-open closed tidal inlets to improve mixing, or improving salt tolerant vegetation coverage to trap sediment and slow evaporation.”

A lagoon can bounce back surprisingly fast when appropriately flushed. After the record 2022 Murray–Darling floods, South Australia’s Coorong Lagoon’s microbiome within months, demonstrating that timely freshwater inputs can rapidly reverse ‘salty soup’ conditions.

Addressing high salinity and nutrient pollution in lagoons benefits the ecosystems they serve while mitigating human health impacts.

“Fish kills hurt local fisheries, algae blooms may produce toxins or airborne irritants, and lost seagrass can weaken coastal flood protection,” says Dr Keneally.

“Emerging research also suggests degradation can make these ecosystems a source of potent greenhouse emissions, adding to climate impacts felt well beyond the shoreline.”

Tagged in featured story, coastal lagoons, climate change