Scientists discover new facts about colored organic matter in deep ocean

by    DiveSSI    26th May 2017
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About half of atmospheric carbon dioxide is fixed by ocean's phytoplankton (c) Dominik Vögtli
2015_11_05_Osterinsel_Korallen_c_Dominik_Voegtli
About half of atmospheric carbon dioxide is fixed by ocean's phytoplankton (c) Dominik Vögtli

Picocyanobacteria found to be major cause of it

About half of atmospheric carbon dioxide is fixed by ocean's
phytoplankton, mainly picocyanobacteria, through photosynthesis.

Picocyanobacteria are unicellular microorganisms that are widely
distributed in freshwater and marine environments.

A large portion of biologically fixed carbon is formed by these
phytoplankton at the sea surface and then transported to the deep
ocean. But it is still unclear how colored dissolved organic matter
(which originates from plant detritus on land or at sea) ends up in the
deep ocean.

“We are still at the beginning of understanding the marine carbon cycle,”
said Michael Gonsior, a chemist at the University of Maryland Center
for Environmental Science (UMCES). He added that the sources of
specific chemicals in the ocean was not yet well defined as it was a
vast and complex system.

In the deep ocean, dissolved organic matter displays a fluorescence
signal similar to the humic-like fluorescence found in a river or
stream. Many scientists have hypothesized that this material is derived
from rivers and streams that carry it off the land and into the ocean.
However, there is growing evidence that there are marine sources of
this material, which may explain the majority of this colored material
found in the deep ocean.

UMCES researchers Gonsior and Feng Chen took the first step in
characterizing the organic matter released from marine
picocyanobacteria.

“Our original plan was to understand the fate of organic carbon released from viral lysis of picocyanobacteria,” said Chen, a molecular biologist.

For the first time, they have shown that cultured picocyanobacteria –
Synechococcus and Prochlorococcus – release fluorescent components that
closely match these typical fluorescent signals found in oceanic
environments.

Both Synechococus and Prochlorocccos are the most abundant carbon
fixers in the ocean. It is predicted that picocyanobacteria, which
prefer warmer temperatures, may increase 10 to 20 percent by the end of
the century if ocean warming continues.

“When you sail on the blue ocean, a
lot of picocyanbacteria are working there. They turn carbon dioxide
into organic carbon and are likely responsible for some of the deep
ocean color coming from organic matter,” said Gonsior.

Gonsior and Chen studied the strain of Synechococus and stumbled upon
the discovery. They planned to measure the fate of dissolved organic
matter by examining the molecular composition using state-of-the-art
mass spectrometry undertaken in collaboration with Professor Philippe
Schmitt-Kopplin at the Helmholtz Center for Environmental Health in
Munich, Germany.

Many biological compounds glow when excited with
light. Gonsior conducted optical analyses that measured the absorbance
and fluorescence.

“When I saw the first fluorescence
measurements of these samples, it was very clear what was going on. We
found those picocyanobacteria were releasing fluorescent organic
matter, which mimics that what we see in both the deep ocean, but also
in rivers and streams,” said Gonsior.

“To me, this is exciting because you
have such abundant photosynthetic cyanobacteria in the ocean. We’ve
known that for a long time but nobody made a connection between
picocyanobacteria and fluorescent dissolved organic matter,” said Chen.

Source of information

TAGS
ocean, research,
Written by
DiveSSI
Date
26th May 2017
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