Press releases

Climate refugee Cod

High Probability for loss of breeding grounds if temperature increases by more than 1.5 degrees
Polar cod in ice
Polar cod in ice (Photo: Alfred Wegener Institute / Jasmine Nahrgang, UIT The Arctic University of Norway)

The latest research conducted by AWI experts that the chances of survival for the offspring of important fish species will dramatically worsen, if the 1.5 ° C target of the Paris Climate Agreement is not achieved. Under conditions of further warming and acidification of the ocean, Atlantic cod and its arctic relative polar cod would be forced to look for new habitats in the far north. Their populations could dwindle. If so, this could be disastrous, as the polar cod is the most important food source for Arctic seals and seabirds. In addition, fishers could lose the world’s most productive area for catching Atlantic cod, located to the north of Norway. However, the results of the study in the magazine science advances also show that a stringent climate policy could prevent the worst consequences for animals and humans.

There are some types of fish that prefer extremely cool water – and can only spawn in cold water. The Atlantic cod, a well-known and favourite food fish, is one of them. Even better adapted to the cold is the polar cod, which overwinters in the Arctic in large swarms below the sea ice. The polar cod spawns at water temperatures between 0 and 1.5 degrees Celsius, because the fertilised eggs / the embryos can best develop at this temperature. In contrast, the Atlantic cod spawns at 3 to 7 degrees, which, from a human standpoint, is still extremely cold. The AWI researchers Flemming Dahlke and Dr Daniela Storch are convinced that this dependency on cold water could prove fateful for both species; as a result of climate change, especially the waters of the North Atlantic and Arctic will warm considerably unless human beings find a way to massively reduce emissions of the greenhouse gas carbon dioxide. In addition, there is the problem of acidification: the more carbon dioxide finds its way into the atmosphere, the more carbon dioxide dissolves in the ocean. Carbon dioxide bonds with water to form carbonic acid, which acidifies the ocean as it decays. “That means Atlantic cod and polar cod will be doubly stressed in the future: their habitat will simultaneously grow warmer and more acidic,” explains marine ecologist Flemming Dahlke.

He and project director Dr Daniela Storch, as the first researchers worldwide, have now used painstaking experiments to investigate how a simultaneous acidification and warming would affect the eggs of both species. In this context, the two AWI experts have especially concentrated on the embryos’ development up to the point where they hatch as larvae, only a few millimetres long. During this stage, they are especially sensitive to changing environmental conditions, which climate change could realistically produce. The researchers’ findings are sobering: in both species, even a small rise in temperature can cause the eggs to die or produce deformations in the larvae. “As we can see, the embryos are very sensitive, especially in the early phase of their development,” says Flemming Dahlke. As the experiments clearly show, the situation becomes even worse when the water is acidic: the number of embryos that don’t survive increases by 20 to 30 percent at a pH level of 7.7, even at optimal temperatures.

In addition, the two AWI researchers’ work is unique in that they combined laboratory findings with established climate models. The models predict the extent to which temperatures in various waters will be affected by climate change, and how much they will acidify. In turn, thanks to their experiments the two researchers can now precisely determine in which areas the Atlantic cod and polar cod will no longer be able to spawn in the future. It also becomes clear that we could see shifts in fish populations, because the adults will have to search for new spawning areas where their eggs or embryos can still find viable conditions for normal development. In this regard, Dahlke and Storch have chiefly considered three climate scenarios: the business-as-usual scenario, in which there is no meaningful reduction in carbon dioxide emissions by the end of the 21st century; a climate scenario with moderate warming, and a scenario in which the IPCC’s 1.5-degree goal – according to which the Earth’s temperature can’t be allowed to increase by more than 1.5 degrees in order to avoid the worst effects of climate change – is achieved. Working together with climate modeller Martin Butzin from the AWI, they arrived at some interesting conclusions. According to Flemming Dahlke, “They show that, for the business-as-usual scenario, conditions for the young Atlantic cod will especially deteriorate in the North Atlantic near the end of this century. In the regions around Iceland and Norway, up to 60 percent fewer cod larvae will hatch from their eggs.” Generally speaking, the Atlantic cod populations in the Northeast Atlantic will likely shift into the Arctic, where the spawning grounds still offer adequate conditions. This could especially pose problems for the fishing industry, since the coasts of Iceland and Norway are currently home to the world’s largest populations of Atlantic cod: Every year, around 800,000 tonnes of cod worth 2 billion euros are harvested here. If these populations dwindle, as the AWI experts’ findings indicate, the losses could be enormous.

What’s more, the business-as-usual scenario also looks bleak for the polar cod. If the waters grow warmer, it will retreat north, not only for the business-as-usual scenario but also under the scenario with moderate warming. Since the polar cod depends on sea ice for its overwintering phase, it remains to be seen how the populations will be affected if the sea-ice extent continues to shrink. Nor is it clear to what extent the Atlantic cod will encroach on the polar cod’s territory. Given the fact that the Atlantic cod is considerably larger and more aggressive than its polar cousin, the latter may have to fight for its food. Whether or not that happens, a drop in the polar cod population would be catastrophic, as it is a staple food for many organisms in the Arctic – including seals, seabirds and even whales.

The limits of fish species’ distribution also depend on where the prevalent temperatures are optimal for spawning. Dahlke and Storch’s experiments have for the first time confirmed that acidification makes fish embryos more sensitive not only to higher temperatures, but also to lower ones. “We’ve observed that the young Atlantic cod not only react adversely to warmer temperatures, but also to especially cold ones,” says Daniela Storch. “The acidification amplifies this effect.” In other words: the added burden of acidification reduces the suitable temperature range for Atlantic cod and polar cod to spawn. As Flemming Dahlke relates: “The fish become more sensitive to extreme temperatures, and consequently to the anticipated warming.” This would ultimately mean that the two species’ potential spawning grounds shrink, and that they might have less available habitat.

Flemming Dahlke stresses that, though the experiments yielded very clear findings, predicting the development of fish populations is extremely difficult. “For instance, whether or not the embryos and larvae survive also depends on the ocean currents and available food.” The Atlantic cod now spawn near Lofoten, an archipelago to the northwest of Norway. The current takes the eggs floating in the water, and later the larvae, farther north, where ideal living conditions await them. “If the Atlantic cod populations and their spawning grounds shift to the northeast in the future, the fish will most likely spawn in completely different systems of currents,” Dahlke explains. “If that happens, we can’t yet begin to gauge the effects.”

There is also good news, says Daniela Storch: “Achieving the climate goals of 1.5 ° C can prevent the worst, maintaining important spawning areas and minimizing the risks of both species.”

Original publication

Flemming T. Dahlke, Martin Butzin, Jasmine Nahrgang, Velmurugu Puvanendran; Atle Mortensen, Hans-Otto Pörtner and Daniela Storch: Northern cod species face spawning habitat losses if global warming exceeds 1.5 °C. Science Advances (28. November 2018) DOI: 10.1126/sciadv.aas8821

The work was conducted in the frame of BIOACID.

Contact

Science

Daniela Storch
+49(471)4831-1934

Press Office

Folke Mehrtens
+49(0)471 4831-2007

Downloads

Polar cod in ice
Polar cod in ice (Photo: Alfred Wegener Institute / Jasmine Nahrgang, UIT The Arctic University of Norway)
Atlantic Cod in a tank
Kabeljau in einem Becken (Photo: Alfred-Wegener-Institut / Felix Mark)
Egg of Polar Cod ca. 24 h after fertilization. 
Ei des Polar Dorsches ca 24 Std. nach der Fertilisierung. Es findet gerade die erste Zellteilung statt...der Beginn des Lebens! Foto: Flemming Dahlke
Egg of Polar Cod ca. 24 h after fertilization. (Photo: Alfred-Wegener-Institut)
Polar Cod: Newly hatched larva
Freshly hatched larva, ca 50 days after fertilisation. (Photo: Alfred-Wegener-Institut / Flemming Dahlke)
Atlantic cod embryos, The eggs have a diametre of ca 1.5 mm.
Atlantic cod embryos, the eggs have a diametre of ca 1.5 mm. (Photo: Alfred-Wegener-Institut)
Distribution patterns of (A) Atlantic cod and (B) Polar cod. These waters are inhabited by different Atlantic cod and Polar cod populations, all of which reproduce during winter and spring (Atlantic cod: March-May, Polar cod: December-March) at species-specific locations (i.e. spawning habitats, blue-shaded areas) with characteristic temperature and sea-ice conditions (Atlantic cod: 3 to 7 °C, open water; Polar cod: -1 to 2 °C, closed sea-ice cover). Green arrows indicate egg and larval dispersal driven by prevailing surface currents. During summer, the feeding grounds (green-shaded areas) of both species partly overlap, for example around Svalbard, which marks the northernmost distribution limit of Atlantic cod. Red symbols denote the origin of animals (spawning adults) used in this study. Distribution maps were redrawn after (4, 13, 33). NEW, Northeast Water Polynya; FJL, Franz-Joseph-Land, NZ, Novaya Zemlya.
Distribution patterns of (A) Atlantic cod and (B) Polar cod. These waters are inhabited by different Atlantic cod and Polar cod populations, all of which reproduce during winter and spring (Atlantic cod: March-May, Polar cod: December-March) at species-specific location... (Photo: Alfred-Wegener-Institut)
Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the study area under Representative Concentration Pathways (RCPs). A–C, RCP8.5: Unabated ocean warming and acidification. D–F, RCP4.5: Intermediate warming (no acidification considered). G–I, RCP2.6: Less than 2 °C global warming (no acidification considered). Maps show the shift in potential egg survival (PES) between the baseline period (1985–2004, Spawning seasons of Atlantic cod: March–May and Polar cod: December–March, see Fig. 3) and the median of CMIP5 multimodel-based projections (seasonal sea surface temperature, 0-50m, see Methods) for this century’s end (2081–2100). Black shading indicates areas (cells, 1° × 1°) with high uncertainty (that is, the shift in PES within that cell is smaller than the CMIP5 ensemble spread, see Methods). Dotted magenta lines represent the sea-ice edge positions of the respective species-specific spawning season (defined as areas with ice concentrations > 70%). C, F, I, For each map, values (change in PES) of individual cells are summarized by kernel density estimations with the width corresponding to the relative occurrence of values. Box plots show the 25th, 50th and 75th percentile; the ends of the whiskers mark the 95% intervals. NEW, Northeast Water Polynya; FJL, Franz-Joseph-Land, NZ, Novaya Zemlya.
Change in thermally suitable spawning habitat of Atlantic cod (left) and Polar cod (right) in the study area under Representative Concentration Pathways (RCPs). A–C, RCP8.5: Unabated ocean warming and acidification. D–F, RCP4.5: Intermediate warming (no acidification co... (Photo: Alfred-Wegener-Institut)
AWI biologist Flemming Dahlke
AWI biologist Flemming Dahlke (Photo: Alfred-Wegener-Institut)
AWI marine biologist Dr. Daniela Storch. 
AWI-Biologin Daniela Storch
AWI marine biologist Dr. Daniela Storch. (Photo: Alfred-Wegener-Institut)
Close-up of a respiration chamber, which is used to measure oxygen consumption (here with the eggs of crabs).


Nahaufnahme einer Respirationskammer, in welcher der Sauerstoffverbrauch gemessen wird. (hier mit Krabbeneiern)
Close-up of a respiration chamber, which is used to measure oxygen consumption (here with the eggs of crabs). (Photo: Alfred-Wegener-Institut)
Archived image: Juvenile Atlantic cod in the fish tanks of the aquarium container. Juvenile Kabeljaus in den Aquarien des Aquarienconatiners.
Juvenile Atlantic cod in the fish tanks of the aquarium container. Juvenile Kabeljaus in den Aquarien des Aquarienconatiners. (Photo: Alfred-Wegener-Institut)
Polar Cod Boreogadus saida in the Arctic

Der Polardorsch Boreogadus saida in der Arktis.
Polar Cod Boreogadus saida in the Arctic (Photo: Alfred-Wegener-Institut)
A group of Polar Cod in a laboratory tank in Tromsø. 

Ein Schwarm Polardorsche im Laborbecken, Tromsø, Norwegen.

Foto von den Forschungsarbeiten des AWI-Wissenschaftlers Flemming Dahlke im Rahmen des BIOACID-Programmes zu den Folgen der Ozeanerwärmung und -versauerung.
A group of Polar Cod in a laboratory tank in Tromsø. (Photo: Alfred-Wegener-Institut)
Archived image: Scientists and the crew empty the fish lift into the fish tank on deck.
Wissenschaftler und Mannschaft entleeren den Fischlift ins Zwischenhälterungsbecken an Deck.
Scientists and the crew empty the fish lift into the fish tank on deck. (Photo: Alfred-Wegener-Institut / Kristina Bär)
Archived image: The fish lift. Der Fischlift.
The fish lift. (Photo: Alfred-Wegener-Institut)
Archived image: The crew lauches the pelagic net with the fish lift into the sea. Die Mannschaft lässt das pelagische Fischnetz mit den Fischlift zu Wasser.
The crew lauches the pelagic net with the fish lift into the sea. (Photo: Alfred-Wegener-Institut)
Archived image: RV Heincke leaves the port of Longyearbyen. In the front is the fish lift.
FS Heincke verlässt den Hafen Longyearbyens. Im Vordergrund steht der Fischlift.
RV Heincke leaves the port of Longyearbyen. In the front is the fish lift. (Photo: Alfred-Wegener-Institut)
Archived image: The pelagic net with the fish lift is pulled on board.
Das pelagische Netz mit Fischlift wird eingeholt. Krossfjord, Spitzbergen.
The pelagic net with the fish lift is pulled on board. (Photo: Alfred-Wegener-Institut)