Shifts from feast to famine contributed to Adélie penguin population boom or bust over 6,000 years
20 September 2021
A colony of Adélie penguins in Antarctica. Researchers used the chemistry of penguin poo preserved in these sediments to reconstruct 6,000 years of Antarctic Ocean circulation.
Credit: Yuesong Gao
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Contact information for the researchers:
Liguang Sun, University of Science and Technology of China, [email protected] (UTC+8 hours)
Zhouqing Xie, University of Science and Technology of China, [email protected] (UTC+8 hours)
WASHINGTON—Preserved penguin poo may be the key to connecting past Antarctic Ocean conditions and penguin populations, shedding light on how the birds and the region’s ecosystem might fare as the climate changes.
A new study analyzed the chemistry of layers of penguin guano that built up from 6,000 years of Adélie penguins nesting in the same Antarctic site. The researchers aimed to tie changes in the poo’s chemistry to shifts in ocean circulation that could have controlled the local food web. The work was published in Geophysical Research Letters, which publishes high-impact, short-format reports with immediate implications spanning all Earth and space sciences.
Antarctica can be a tough place to survive, even for hardy little Adélie penguins. It’s frigid and dark for half the year, and prey—mainly krill and fish—can be hard to come by in the icy Ross Sea. Their food supply changes seasonally with the sunlight, but it also waxes and wanes over thousands of years as ocean currents slowly shift, sea ice forms and breaks up, and water warms and cools.
The new research found several peaks of cadmium, a deep-sea nutrient, in the penguin poo that corresponded to greater densities of penguin remains buried in the nesting area. This relationship suggests that deep, nutrient-laden ocean water was redirected to the surface several times in the past 6,000 years, allowing ecosystems at the surface to thrive. The method is a novel approach to reconstructing past ocean circulation.
The researchers posited that penguin population size was linked to changes in Circumpolar Deep Water, a warm current that flows in the deep ocean roughly clockwise around Antarctica and upwells through the Ross Sea. In the past, circulation changes allowed more of the deep current to reach the surface, delivering nutrients like cadmium that are essential to sustain the base of the food web. That cadmium made its way through krill and fish into, and out of, the penguins.
In addition to providing an explanation for penguin populations, the poo record gives the researchers valuable insight into how oceans behaved in the past—and therefore, how they may work in the near future.
“Circumpolar Deep Water is of great concern to both climatologists and oceanographers because it drives the rapid melting of the West Antarctic ice shelf and outgassing of carbon dioxide to the atmosphere and determines the spatial distribution of biomass in the Southern Ocean,” said Zhouqing Xie, an environmental geochemist at the University of Science and Technology of China who co-authored the study. “But the historical reconstructed record of Circumpolar Deep Water is quite sparse. We only find clues from ocean sediment cores and can indirectly infer what the current was doing through sea-surface temperatures and sea ice.”
“It does appear to be an indicator of how water masses are changing in the Ross Sea,” said Robert McKay, an Antarctic researcher at Victoria University in Wellington who was not involved in the study. “This provides another toolset for our arsenal of understanding the impacts of changing cryosphere on biological systems.”
A warming Antarctica
Understanding how Antarctica’s circulation patterns have changed in the past is important for contextualizing changes in the biosphere and as well as predicting how modern oceans may respond to climate change. Records of past circulation are often based on marine sediments which, while useful for studying the water, do little to reflect what’s happening with life on land. The penguin guano is doubly useful, in providing an additional constraint on ocean circulation and a more direct link between the oceans and land animals.
“One of the big issues we have when we try to make this work relevant to biological systems is scaling up on the food web, which is where this paper is interesting. Because the biosphere is a much more complex system [than the oceans], it’s more chaotic in many ways and harder to model. Getting that link between plankton and megafauna is quite tricky, so this is a nice example of how you can do that,” said McKay.
The study found a peak in cadmium and penguin remains around 1,000 years ago, as the warm Circumpolar Deep Water welled up and melted sea ice. More food could have been available as melting ice cleared foraging and breeding grounds, letting penguin populations climb.
Although some warming has likely boosted penguin populations in the past, rapid warming in Antarctica today may be too much for the birds to handle.
“Current warming in West Antarctica is so fast and intense that may cause problems in other aspects. In particular, enhanced Circumpolar Deep Water upwelling in West Antarctica has caused rapid glacial melting, extreme warming of the ocean surface and possibly a southward contraction in krill distribution. This could lead to the relocating of penguin habitat and, for emperor penguins that breed on ice, the possibility of complete disappearance in some areas,” said Liguang Sun, a co-author on the study at the University of Science and Technology of China.
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Notes for Journalists:
This research study will be freely available for 30 days. Download a PDF copy of the paper here. Neither the paper nor this press release is under embargo.
Paper title:
“6,000-Year Reconstruction of Modified Circumpolar Deep Water Intrusion and Its Effects on Sea Ice and Penguin in the Ross Sea”
Authors:
- Qibin Xu, Department of Environmental Science and Engineering, Institute of Polar Environment & Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, China
- Lianjiao Yang, Department of Environmental Science and Engineering, Institute of Polar Environment & Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, China
- Yuesong Gao, Department of Environmental Science and Engineering, Institute of Polar Environment & Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, China
- Liguang Sun (corresponding author), Department of Environmental Science and Engineering, Institute of Polar Environment & Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, China
- Zhouqing Xie (corresponding author), Department of Environmental Science and Engineering, Institute of Polar Environment & Anhui Key Laboratory of Polar Environment and Global Change, University of Science and Technology of China, Hefei, China