Ensemble projections of global ocean animal biomass with climate change. (A) Multimodel mean change in total biomass without fishing for historical and four future emission scenarios (RCPs) relative to 1990–1999 with 1 SD (±SD, n = 10); thin vertical line indicates target year for achieving SDGs. (B) Individual model projections for RCP8.5 without fishing showing the spread across different ecosystem model and ESM combinations. (C) Projected biomass declines for three size groups in 2090–2099 relative to 1990–1999 under low (RCP2.6) and high (RCP8.5) emissions without fishing (n = 10). (D) Projected climate change effect (RCP8.5 vs. RCP2.6) in 2090–2099 for three size groups with and without fishing (n = 6). (E) Variability in biomass projections (expressed as SD of % change) due to different ESMs and different MEMs under RCP2.6 and RCP8.5 without fishing for three size groups (n = 10). Box plots display the median (horizontal line), mean (x), and interquartile range (boxes). Graphic: Lotze, et al., 2019 / PNAS
Ensemble projections of global ocean animal biomass with climate change. (A) Multimodel mean change in total biomass without fishing for historical and four future emission scenarios (RCPs) relative to 1990–1999 with 1 SD (±SD, n = 10); thin vertical line indicates target year for achieving SDGs. (B) Individual model projections for RCP8.5 without fishing showing the spread across different ecosystem model and ESM combinations. (C) Projected biomass declines for three size groups in 2090–2099 relative to 1990–1999 under low (RCP2.6) and high (RCP8.5) emissions without fishing (n = 10). (D) Projected climate change effect (RCP8.5 vs. RCP2.6) in 2090–2099 for three size groups with and without fishing (n = 6). (E) Variability in biomass projections (expressed as SD of % change) due to different ESMs and different MEMs under RCP2.6 and RCP8.5 without fishing for three size groups (n = 10). Box plots display the median (horizontal line), mean (x), and interquartile range (boxes). Graphic: Lotze, et al., 2019 / PNAS

By Alison Auld
11 June 2019

(Dal News) – Populations of large fish and other marine species will decline steadily if little is done to stem the effects of climate change, according to a study led by Dalhousie University researchers that shows how greenhouse gas emissions could cause widespread global stock losses and habitat shifts.

The paper by a team of 35 international scientists and published Tuesday (11 June 2019) in the Proceedings of the National Academy of Sciences presents a stark view of what will happen to the global biomass — the total weight of marine animals, such as fish, invertebrates and mammals — if measures aren’t taken to reduce emissions.

Derek Tittensor, an adjunct professor in the Department of Biology at Dalhousie who co-authored the report, says it provides a more comprehensive assessment of climate change because it is one of the first to use a combination of multiple climate and marine ecosystem models, rather than individual ones used in previous forecasts.

The innovative approach reveals that global marine animal biomass will decline under all emission scenarios, due largely to increasing water temperatures and a decrease in primary production.

Trophic amplification of marine biomass declines. Shown is the magnitude of projected mean changes in 2090–2099 relative to 1990–1999 (percent, ±SD) for NPP, phytoplankton, and zooplankton biomass derived from ESMs (n = 2) and higher trophic levels from MEMs across four RCPs (n = 10 for RCP2.6 and RCP8.5; n = 8 for RCP4.5 and RCP6.0). All ecosystem models use either NPP or phytoplankton biomass as forcing variables, and some also use zooplankton biomass. Graphic: Lotze, et al., 2019 / PNAS
Trophic amplification of marine biomass declines. Shown is the magnitude of projected mean changes in 2090–2099 relative to 1990–1999 (percent, ±SD) for NPP, phytoplankton, and zooplankton biomass derived from ESMs (n = 2) and higher trophic levels from MEMs across four RCPs (n = 10 for RCP2.6 and RCP8.5; n = 8 for RCP4.5 and RCP6.0). All ecosystem models use either NPP or phytoplankton biomass as forcing variables, and some also use zooplankton biomass. Graphic: Lotze, et al., 2019 / PNAS

“We found that with every degree of warming you’re seeing about a 5-per-cent drop in the total amount of biological materials in the oceans, which is quite a significant decline and gets more serious as we move up the food chain,” says Dr. Tittensor (pictured), who is also a senior marine biodiversity scientist with the UN Environment World Conservation Monitoring Centre in Cambridge, UK.

“There are substantial consequences for marine ecosystems on a global scale. The oceans are changing quite significantly, but if we focus on what we have control over we still have a chance to alter our trajectory.”

Mitigating the impact

The study projects that if rigorous measures are not put in place to curb greenhouse gas emissions, the biomass decline could soar to 17 per cent by the end of the 21st century.

The losses can be constrained significantly if strong mitigation measures are adopted, the report says.

“Reduction of greenhouse gas emissions will undoubtedly help to safeguard marine life as much as possible against further losses” says lead author Heike Lotze of Dalhousie.

The report, which was written by three Dalhousie researchers and 32 scientists from 12 countries, also found that the magnitude of the climate-change effect was similar in areas with and without fishing pressure.

The analysis suggests that climate-change impacts may be more severe at higher food-web levels, meaning that larger fish and marine mammals may suffer more severe declines than smaller species like phytoplankton.

Dr. Tittensor says that could cause a dangerous domino effect when it comes to species declines.

Researchers caution that biomass will decline in many temperate to tropical ocean regions, where people are highly dependent on the seafood supply and where marine biodiversity is already affected by human activity.

Projected biomass trends in relation to global air temperature changes. Shown is the relationship of the change in marine animal biomass to increasing global surface air temperature since preindustrial times (1860s). Each dot represents an annual ensemble mean (n = 10) relative to 1990–1999 across historical and future emission scenarios (RCPs) in the absence of fishing. Vertical lines frame expected changes between 1.5 °C and 2 °C of warming. Graphic: Lotze, et al., 2019 / PNAS
Projected biomass trends in relation to global air temperature changes. Shown is the relationship of the change in marine animal biomass to increasing global surface air temperature since preindustrial times (1860s). Each dot represents an annual ensemble mean (n = 10) relative to 1990–1999 across historical and future emission scenarios (RCPs) in the absence of fishing. Vertical lines frame expected changes between 1.5 °C and 2 °C of warming. Graphic: Lotze, et al., 2019 / PNAS

“We know that food production on land is increasingly put at risk by climate change impacts, such as extreme heat and drought. This study adds another disconcerting chapter to the global warming story, by confirming that human-made climate change endangers food resources in the oceans too,” says co-author Jacob Schewe of the Potsdam Institute for Climate Impact Research in Potsdam, Germany.

He adds that efforts to slow the marine losses are in keeping with the UN Sustainable Development Goal to achieve zero hunger by 2030.

“Our research shows that this will require not only a much more careful management of natural resources, but also rapid reductions in global greenhouse gas emissions,” Dr. Schewe says.

Global implications

Conversely, many polar regions around the Arctic and Antarctica could see biomass increases which may provide new opportunities for marine resource use but also challenges to management and conservation.

That could have broad implications for commercial fisheries if stocks migrate to other geographic areas as waters warm and polar ice melts.

“We can already see that fish species and other marine organisms are moving away from areas, and as they come under more stress it will be quite difficult for them to maintain their fisheries,” says Dr. Tittensor. “So, we have to recognize that there are going to be winners and losers when it comes to the impacts of climate change.”

For that reason, he says the insights gained from the report should inform decisions about fisheries and ecosystem management.

“Yes, things are changing but we have an opportunity to respond to them and deal with them in an effective way.”

New study flags substantial declines in large fish and marine species if climate change goes unmitigated


Global ensemble projections reveal trophic amplification of ocean biomass declines with climate change

Spatial patterns of projected biomass changes. Shown are global ensemble projections at a 1 × 1 degree resolution for (A, C, and E) RCP2.6 and (B, D, and F) RCP8.5. (A and B) Multimodel mean change (percent, n = 10) in total marine animal biomass in 2090–2099 relative to 1990–1999 without fishing. (C and D) Variability among different ecosystem model and ESM combinations expressed as 1 SD. (E and F) Model agreement (percent) on the direction of change. Graphic: Lotze, et al., 2019 / PNAS
Spatial patterns of projected biomass changes. Shown are global ensemble projections at a 1 × 1 degree resolution for (A, C, and E) RCP2.6 and (B, D, and F) RCP8.5. (A and B) Multimodel mean change (percent, n = 10) in total marine animal biomass in 2090–2099 relative to 1990–1999 without fishing. (C and D) Variability among different ecosystem model and ESM combinations expressed as 1 SD. (E and F) Model agreement (percent) on the direction of change. Graphic: Lotze, et al., 2019 / PNAS

ABSTRACT: While the physical dimensions of climate change are now routinely assessed through multimodel intercomparisons, projected impacts on the global ocean ecosystem generally rely on individual models with a specific set of assumptions. To address these single-model limitations, we present standardized ensemble projections from six global marine ecosystem models forced with two Earth system models and four emission scenarios with and without fishing. We derive average biomass trends and associated uncertainties across the marine food web. Without fishing, mean global animal biomass decreased by 5% (±4% SD) under low emissions and 17% (±11% SD) under high emissions by 2100, with an average 5% decline for every 1 °C of warming. Projected biomass declines were primarily driven by increasing temperature and decreasing primary production, and were more pronounced at higher trophic levels, a process known as trophic amplification. Fishing did not substantially alter the effects of climate change. Considerable regional variation featured strong biomass increases at high latitudes and decreases at middle to low latitudes, with good model agreement on the direction of change but variable magnitude. Uncertainties due to variations in marine ecosystem and Earth system models were similar. Ensemble projections performed well compared with empirical data, emphasizing the benefits of multimodel inference to project future outcomes. Our results indicate that global ocean animal biomass consistently declines with climate change, and that these impacts are amplified at higher trophic levels. Next steps for model development include dynamic scenarios of fishing, cumulative human impacts, and the effects of management measures on future ocean biomass trends.

SIGNIFICANCE: Climate change can affect the distribution and abundance of marine life, with consequences for goods and services provided to people. Because different models can lead to divergent conclusions about marine futures, we present an integrated global ocean assessment of climate change impacts using an ensemble of multiple climate and ecosystem models. It reveals that global marine animal biomass will decline under all emission scenarios, driven by increasing temperature and decreasing primary production. Notably, climate change impacts are amplified at higher food web levels compared with phytoplankton. Our ensemble projections provide the most comprehensive outlook on potential climate-driven ecological changes in the global ocean to date and can inform adaptive management and conservation of marine resources under climate change.

Global ensemble projections reveal trophic amplification of ocean biomass declines with climate change