Heterotrophic picoplankton is the fraction of

plankton Plankton are the diverse collection of organisms found in water (or air) that are unable to propel themselves against a current (or wind). The individual organisms constituting plankton are called plankters. In the ocean, they provide a crucia ...

composed by cells between 0.2 and 2 μm that do not perform

photosynthesis Photosynthesis is a process used by plants and other organisms to convert light energy into chemical energy that, through cellular respiration, can later be released to fuel the organism's activities. Some of this chemical energy is stored i ...

. They form an important component of many biogeochemical cycles. Cells can be either: * prokaryotes Archaea form a major part of the picoplankton in the Antarctic and are abundant in other regions of the ocean. Archaea have also been found in freshwater

picoplankton Picoplankton is the fraction of plankton composed by cells between 0.2 and 2 μm that can be either prokaryotic and eukaryotic phototrophs and heterotrophs: * photosynthetic * heterotrophic They are prevalent amongst microbial plankton communit ...

, but do not appear to be so abundant in these environments. * eukaryotes

Cell structure

Nucleic acid content in cells

Heterotrophic A heterotroph (; ) is an organism that cannot produce its own food, instead taking nutrition from other sources of organic carbon, mainly plant or animal matter. In the food chain, heterotrophs are primary, secondary and tertiary consumers, but ...

picoplankton can be divided into two broad categories: high nucleic acid (HNA) content cells and low nucleic acid (LNA) content cells. Nucleic acids are large biomolecules that store and express genomic information. HNA picoplankton dominate in waters that are

eutrophic Eutrophication is the process by which an entire body of water, or parts of it, becomes progressively enriched with minerals and nutrients, particularly nitrogen and phosphorus. It has also been defined as "nutrient-induced increase in phytoplan ...

to mesotrophic while low LNA picoplankton dominate in stratified oligotrophic environments. The proportion of HNA picoplankton to LNA picoplankton is a defining characteristic of bacterioplankton communities. Addition of glyphosate, a common herbicide that causes increased levels of phosphorus when introduced to aquatic systems, causes an increase in the ratio of HNA to LNA bacteria. Nucleic acids are a costly compound for cells to synthesize and the increased bioavailable phosphorus in the system likely allows HNA bacteria to rapidly synthesize more nucleic acids and divide. HNA bacterioplankton are larger and more active than LNA picoplankton. HNA cells also have higher specific metabolic and growth rates, likely allowing these type of bacterioplankton to better utilize and exploit sudden increases in nutrients within the water column. The relative abundance of HNA to LNA cells is related to overall system productivity, specifically chlorophyll concentration, though other factors likely also contribute to bacterioplankton distribution.

Biogeochemical cycling

Dissolved organic matter

Heterotrophic picoplankton play a critical role in nutrient and carbon recycling in ecological food webs by transforming and mineralizing organic matter. Aquatic dissolved organic matter is one of the largest organic pools on Earth and a major part of the

carbon cycle The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main component of biological compounds as well as a major componen ...

. The majority of dissolved organic matter is either resistant to transformation or semi-labile, limiting the availability of these compounds to biodegradation. Water bodies accumulate dissolved organic matter via both allochthonous sources, mainly decaying terrestrial plants and soil organic matter, and autochthonous sources, mainly from phytoplankton and macrophytes. As major decomposers of organic matter, heterotrophic bacterioplankton act as an important link between detritus, dissolved organic matter, and higher trophic levels in aquatic systems. Bacterioplankton degrade particulate organic matter into smaller compounds and either assimilate and absorb them or expel them as inorganic carbon. Both of these processes promote transformation of matter within the aquatic system and promote energy flow and are important components of the overall quality of a water body. Heterotrophic bacteria community structure and functionality is used to assess the trophic status and quality of freshwater systems.

References

{{plankton Biological oceanography Planktology Aquatic ecology