Coastal anthropogenic carbon
By Adam Thomas
Excess carbon dioxide emitted by human activities—such as fossil fuel burning, land-use changes, and deforestation—is known as anthropogenic carbon dioxide. Approximately thirty percent of this anthropogenic carbon dioxide in the atmosphere is absorbed by the world’s oceans.
While this absorption helps mitigate global warming, it also has
adverse effects on marine life, including fish and plants.
While the impact of anthropogenic carbon dioxide on the open
oceans has been extensively studied, there has been limited observational data
on its presence and sources in coastal oceans, the broad range of saltwater
ecosystems, from estuaries to coral reefs, that link the land and sea.
A recent study from Wei-Jun Cai’s lab at the University of
Delaware, titled “The
Source and Accumulation of Anthropogenic Carbon in the U.S. East Coast,”
published in Science Advances, addresses this gap.
The lead author, Xinyu Li, earned her doctorate from UD’s
School of Marine Science and Policy in 2023 and is now a postdoctoral
researcher at the Pacific Marine Environmental Laboratory. Wei-Jun Cai,
associate dean for research and the Mary A.S. Lighthipe Chair Professor of
Earth, Ocean, and Environment, was Li’s advisor and supervised the study.
Co-authors include Zelun Wu, a dual-degree doctoral student at UD and Xiamen
University, and Zhangxian Ouyang, a postdoctoral researcher at UD.
The researchers analyzed a high-quality carbonate dataset from five research cruises conducted between 1996 and 2018. This dataset covers the East Coast of the United States’ Mid-Atlantic Bight, a coastal region stretching from Massachusetts to North Carolina.
The 1996 dataset, provided by Doug Wallace, a professor of
oceanography at Dalhousie University, allowed the researchers to track changes
in carbon dioxide levels over time. Except for the 1996 cruise, the data were
collected by members of Cai’s group under the Ocean Acidification Program of
the National Oceanic and Atmospheric Administration (NOAA).
The researchers used this data to investigate where and how
much anthropogenic carbon dioxide is entering coastal waters, which are crucial
to the global carbon budget.
Newer Water, Higher Anthropogenic Carbon Dioxide
Surface water—the top 200 meters of the ocean—showed the
highest increase in anthropogenic carbon dioxide due to its direct contact with
the atmosphere, which leads to greater absorption of atmospheric CO2.
Cai noted that an intriguing aspect of the study was
analyzing the proportions of natural versus anthropogenic CO2 in the water and
how water age affects anthropogenic carbon accumulation.
Surface water, being newer and arriving via the Gulf Stream
from the Gulf of Mexico, exhibited high levels of anthropogenic carbon dioxide
but relatively low levels of naturally occurring carbon dioxide.
In contrast, the middle layer of water (below 200 meters)
had high concentrations of natural carbon dioxide and lower levels of
anthropogenic carbon dioxide.
“The surface water has very high anthropogenic carbon
dioxide but the middle layer water, that water that comes from the Southern
Ocean and is called the Antarctic Intermediate Water, that water travels a long
time, maybe 100 years from the Southern Ocean to the East Coast,” said Cai.
“That water has a lot of natural carbon dioxide because of microbial
decomposition but that water has very low amounts of anthropogenic
carbon.”
Below these layers lies the North Atlantic Deep Water, which
sinks in winter and travels from the Labrador Sea to the East Coast over two
decades. “This water has an intermediate level of anthropogenic carbon
dioxide,” Cai said. “Each water mass has a recorded level of carbon dioxide
from its time of formation, and this gave us a history of these changes.
It’s interesting to see that the more recent waters had the highest levels of
anthropogenic carbon.”
Li described this distribution as a “sandwich structure,”
with high anthropogenic carbon on the surface, low anthropogenic carbon in the
middle layers, and intermediate levels deeper down. “This distribution is
closely related to water age, when it comes in contact with the atmosphere on
the surface and absorbs carbon dioxide from the atmosphere,” Li said.
Anthropogenic Carbon Transport
The study also found that anthropogenic carbon decreases
from offshore to nearshore waters, correlating with lower salinity. This
suggests that there is no net increase in the export of anthropogenic carbon
dioxide from nearshore areas like estuaries and wetlands to the open ocean.
“When we extrapolate our results to low salinity waters,
like the water coming out of the Delaware Bay and the Chesapeake Bay, we found
that there is actually very little anthropogenic carbon dioxide increase in
very low salinity waters,” Cai explained. “That water has a lot of natural
carbon dioxide but there’s very little anthropogenic carbon dioxide
there.”
This finding supports previous research indicating that net
anthropogenic carbon dioxide transport from estuaries and wetlands to the
continental shelf is essentially zero, or even negative. Possible reasons
include low buffer capacity and short residence times in estuarine waters,
which limit their ability to absorb anthropogenic CO2. Additionally, the loss
rate of North American wetlands is three times its growth rate, reducing the
opportunity for carbon uptake and transport to coastal waters.
Cai highlighted the broader implications of these findings for the global carbon cycle. “This paper clarifies conflicting views from terrestrial studies,” he said. “There is a big debate about whether there is an increase of transport of anthropogenic carbon dioxide from terrestrial systems to the coastal ocean.
Our conclusion is that there is no natural transport of
anthropogenic carbon and that anthropogenic carbon in the coastal waters is
really all mixed in from the offshore water masses and comes locally from the
atmosphere above it. A majority of the latter is then exported to the ocean.”