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Productivity (ecology)

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(Redirected fromBiological productivity)
Rate of generation of biomass in an ecosystem
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Inecology, the termproductivity refers to the rate of generation ofbiomass in anecosystem, usually expressed in units ofmass per volume (unit surface) per unit of time, such asgrams per square metre perday (g m−2 d−1). The unit of mass can relate todry matter or to the mass of generatedcarbon. The productivity ofautotrophs, such asplants, is calledprimary productivity, while the productivity ofheterotrophs, such asanimals, is calledsecondary productivity.[1]

The productivity of an ecosystem is influenced by a wide range of factors, including nutrient availability, temperature, and water availability. Understanding ecological productivity is vital because it provides insights into how ecosystems function and the extent to which they can support life.[2]

Primary production

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Main article:Primary production

Primary production is the synthesis oforganic material frominorganic molecules. Primary production in most ecosystems is dominated by the process ofphotosynthesis, In which organisms synthesize organic molecules fromsunlight,H2O, andCO2.[3] Aquatic primary productivity refers to the production of organic matter, such as phytoplankton, aquatic plants, and algae, in aquatic ecosystems, which include oceans, lakes, and rivers. Terrestrial primary productivity refers to the organic matter production that takes place in terrestrial ecosystems such as forests, grasslands, and wetlands.

Primary production is divided into Net Primary Production (NPP) and Gross Primary Production (GPP). Gross primary production measures all carbon assimilated into organic molecules by primary producers.[4] Net primary production measures the organic molecules by primary producers. Net primary production also measures the amount of carbon assimilated into organic molecules by primary producers, but does not include organic molecules that are then broken down again by these organism for biological processes such ascellular respiration.[5] The formula used to calculate NPP is net primary production = gross primary production - respiration.

Primary producers

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Photoautotrophs

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Photoautotrophy

Organisms that rely on light energy tofix carbon, and thus participate in primary production, are referred to asphotoautotrophs.[6]

Photoautotrophs exists across the tree of life. Many bacterial taxa are known to be photoautotrophic such ascyanobacteria[7] and somePseudomonadota (formerly proteobacteria).[8]Eukaryotic organisms gained the ability to participate in photosynthesis through the development ofplastids derived fromendosymbiotic relationships.[9]Archaeplastida, which includesred algae,green algae, and plants, have evolvedchloroplasts originating from an ancient endosymbiotic relationship with anAlphaproteobacteria.[10] The productivity of plants, while being photoautotrophs, is also dependent on factors such as salinity andabiotic stressors from the surrounding environment.[11] The rest of the eukaryotic photoautotrophic organisms are within theSAR clade (ComprisingStramenopila,Alveolata, andRhizaria). Organisms in the SAR clade that developed plastids did so through a secondary or a tertiary endosymbiotic relationships with green algae and/or red algae.[12] The SAR clade includes many aquatic and marine primary producers such asKelp,Diatoms, andDinoflagellates.[12]

Lithoautotrophs

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Chemosynthetic Microbial Mat

The other process of primary production islithoautotrophy. Lithoautotrophs use reduced chemical compounds such ashydrogen gas,hydrogen sulfide,methane, orferrous ion to fix carbon and participate in primary production. Lithoautotrophic organisms areprokaryotic and are represented by members of both thebacterial andarchaeal domains.[13] Lithoautotrophy is the only form of primary production possible in ecosystems without light such asground-water ecosystems,[14]hydrothermal vent ecosystems,[15]soil ecosystems,[16] and cave ecosystems.[17]

Secondary production

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Secondary production is the generation ofbiomass ofheterotrophic (consumer) organisms in a system. This is driven by the transfer of organic material betweentrophic levels, and represents the quantity of newtissue created through the use ofassimilated food. Secondary production is sometimes defined to only include consumption of primary producers byherbivorous consumers[18] (with tertiary production referring tocarnivorous consumers),[19] but is more commonly defined to include all biomass generation by heterotrophs.[1]

Organisms responsible for secondary production include animals,protists,fungi and many bacteria.[citation needed]

Secondary production can be estimated through a number of different methods including increment summation, removal summation, the instantaneous growth method and the Allen curve method.[20] The choice between these methods will depend on the assumptions of each and the ecosystem under study. For instance, whethercohorts should be distinguished, whether linear mortality can be assumed and whetherpopulation growth is exponential.[citation needed]

Net ecosystem production is defined as the difference between gross primary production (GPP) and ecosystem respiration.[21] The formula to calculate net ecosystem production is NEP = GPP - respiration (by autotrophs) - respiration (by heterotrophs).[22] The key difference between NPP and NEP is that NPP focuses primarily on autotrophic production, whereas NEP incorporates the contributions of other aspects of the ecosystem to the total carbon budget.[23]

Productivity

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Following is the list of ecosystems in order of decreasing productivity.[citation needed]

ProducerBiomass productivity (gC/m²/yr)
Swamps and Marshes2,500
Coral reefs2,000
Algal beds2,000
River estuaries1,800
Temperate forests1,250
Cultivated lands650
Tundras140
Open ocean125

Species diversity and productivity relationship

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The connection between plant productivity and biodiversity is a significant topic in ecology, although it has been controversial for decades. Both productivity and species diversity are constricted by other variables such as climate, ecosystem type, and land use intensity.[24] According to some research on the correlation between plant diversity and ecosystem functioning is that productivity increases as species diversity increases.[25] One reasoning for this is that the likelihood of discovering a highly productive species increases as the number of species initially present in an ecosystem increases.[25][26]

Other researchers believe that the relationship between species diversity and productivity is unimodal within an ecosystem.[27] A 1999 study on grassland ecosystems in Europe, for example, found that increasing species diversity initially increased productivity but gradually leveled off at intermediate levels of diversity.[28] More recently, a meta-analysis of 44 studies from various ecosystem types observed that the interaction between diversity and production was unimodal in all but one study.[29]

Human interactions

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Anthropogenic activities (human activities) have impacted the productivity and biomass of several ecosystems. Examples of these activities include habitat modification, freshwater consumption, an increase in nutrients due to fertilizers, and many others.[30] Increased nutrients can stimulate an algal bloom in waterbodies, increasing primary production but making the ecosystem less stable.[31] This would raise secondary production and have a trophic cascade effect across the food chain, ultimately increasing overall ecosystem productivity.[32] In lakes, these human impacts can "mask" the effects ofclimate change.[33] Algalbiomass is causally related to climate in some lakes, with temporary or long-term shifts in productivity (regime shifts).[33]

See also

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References

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  1. ^abAllaby, Michael, ed. (2006) [1994].A Dictionary of Ecology (Third ed.). Oxford, UK:Oxford University Press.ISBN 978-0-19-860905-6. Retrieved2009-12-03.
  2. ^US EPA, ORD (2017-11-01)."Ecological Condition".United States Environmental Protection Agency. Retrieved2023-04-27.
  3. ^Johnson, Matthew P. (2016-10-26)."Photosynthesis".Essays in Biochemistry.60 (3):255–273.doi:10.1042/EBC20160016.ISSN 0071-1365.PMC 5264509.PMID 27784776.
  4. ^Woodwell, George (1 August 2015)."Primary Production in Terrestrial Ecosystems".American Zoologist.8:19–30.doi:10.1093/icb/8.1.19.
  5. ^Yu, Bo; Chen, Fang (2016-08-02)."The global impact factors of net primary production in different land cover types from 2005 to 2011".SpringerPlus.5 (1): 1235.doi:10.1186/s40064-016-2910-1.ISSN 2193-1801.PMC 4971002.PMID 27536518.
  6. ^Scognamiglio, Viviana; Giardi, Maria Teresa; Zappi, Daniele; Touloupakis, Eleftherios; Antonacci, Amina (January 2021)."Photoautotrophs–Bacteria Co-Cultures: Advances, Challenges and Applications".Materials.14 (11): 3027.Bibcode:2021Mate...14.3027S.doi:10.3390/ma14113027.ISSN 1996-1944.PMC 8199690.PMID 34199583.
  7. ^Singh, Jay Shankar; Kumar, Arun; Rai, Amar N.; Singh, Devendra P. (2016)."Cyanobacteria: A Precious Bio-resource in Agriculture, Ecosystem, and Environmental Sustainability".Frontiers in Microbiology.7: 529.doi:10.3389/fmicb.2016.00529.ISSN 1664-302X.PMC 4838734.PMID 27148218.
  8. ^Tang, Kuo-Hsiang; Tang, Yinjie J.; Blankenship, Robert Eugene (2011)."Carbon Metabolic Pathways in Phototrophic Bacteria and Their Broader Evolutionary Implications".Frontiers in Microbiology.2: 165.doi:10.3389/fmicb.2011.00165.PMC 3149686.PMID 21866228.
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  12. ^abGrattepanche, Jean-David; Walker, Laura M.; Ott, Brittany M.; Paim Pinto, Daniela L.; Delwiche, Charles F.; Lane, Christopher E.; Katz, Laura A. (2018)."Microbial Diversity in the Eukaryotic SAR Clade: Illuminating the Darkness Between Morphology and Molecular Data".BioEssays.40 (4) e1700198.doi:10.1002/bies.201700198.PMID 29512175.S2CID 3731086.
  13. ^Lazar, Cassandre Sara; Stoll, Wenke; Lehmann, Robert; Herrmann, Martina; Schwab, Valérie F.; Akob, Denise M.; Nawaz, Ali; Wubet, Tesfaye; Buscot, François (2017-06-13)."Archaeal Diversity and CO2 Fixers in Carbonate-/Siliciclastic-Rock Groundwater Ecosystems".Archaea.2017:1–13.Bibcode:2017Archa2017....1L.doi:10.1155/2017/2136287.PMC 5485487.PMID 28694737.
  14. ^Griebler, C.; Lueders, T. (2009)."Microbial biodiversity in groundwater ecosystems".Freshwater Biology.54 (4):649–677.Bibcode:2009FrBio..54..649G.doi:10.1111/j.1365-2427.2008.02013.x.
  15. ^Sievert, Stefan; Vetriani, Costantino (2012-03-01)."Chemoautotrophy at Deep-Sea Vents: Past, Present, and Future".Oceanography.25 (1):218–233.doi:10.5670/oceanog.2012.21.hdl:1912/5172.
  16. ^Drake, Henrik; Ivarsson, Magnus (2018-01-01)."The role of anaerobic fungi in fundamental biogeochemical cycles in the deep biosphere".Fungal Biology Reviews.32 (1):20–25.Bibcode:2018FunBR..32...20D.doi:10.1016/j.fbr.2017.10.001.S2CID 89881167.
  17. ^Galassi, Diana M. P.; Fiasca, Barbara; Di Lorenzo, Tiziana; Montanari, Alessandro; Porfirio, Silvano; Fattorini, Simone (2017-03-01). "Groundwater biodiversity in a chemoautotrophic cave ecosystem: how geochemistry regulates microcrustacean community structure".Aquatic Ecology.51 (1):75–90.Bibcode:2017AqEco..51...75G.doi:10.1007/s10452-016-9599-7.S2CID 41641625.
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  19. ^"Definition of term: "Tertiary production"".The Glossary Table.FishBase. Retrieved2009-12-03.
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  21. ^Lovett, Gary M.; Cole, Jonathan J.; Pace, Michael L. (2006-01-30)."Is Net Ecosystem Production Equal to Ecosystem Carbon Accumulation?".Ecosystems.9 (1):152–155.Bibcode:2006Ecosy...9..152L.doi:10.1007/s10021-005-0036-3.ISSN 1432-9840.S2CID 5890190.
  22. ^"The Flow of Energy: Primary Production".www.globalchange.umich.edu. Retrieved2023-04-28.
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  24. ^Brun, Philipp; Zimmermann, Niklaus E.; Graham, Catherine H.; Lavergne, Sébastien; Pellissier, Loïc; Münkemüller, Tamara; Thuiller, Wilfried (2019-12-12)."The productivity-biodiversity relationship varies across diversity dimensions".Nature Communications.10 (1): 5691.Bibcode:2019NatCo..10.5691B.doi:10.1038/s41467-019-13678-1.ISSN 2041-1723.PMC 6908676.PMID 31831803.
  25. ^abvan Ruijven, Jasper; Berendse, Frank (2005-01-18)."Diversity–productivity relationships: Initial effects, long-term patterns, and underlying mechanisms".Proceedings of the National Academy of Sciences.102 (3):695–700.Bibcode:2005PNAS..102..695V.doi:10.1073/pnas.0407524102.ISSN 0027-8424.PMC 545547.PMID 15640357.
  26. ^Waide, R. B.; Willig, M. R.; Steiner, C. F.; Mittelbach, G.; Gough, L.; Dodson, S. I.; Juday, G. P.; Parmenter, R. (November 1999)."The Relationship Between Productivity and Species Richness".Annual Review of Ecology and Systematics.30 (1):257–300.Bibcode:1999AnRES..30..257W.doi:10.1146/annurev.ecolsys.30.1.257.ISSN 0066-4162.
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  29. ^Cardinale, Bradley J.; Wright, Justin P.; Cadotte, Marc W.; Carroll, Ian T.; Hector, Andy;Srivastava, Diane S.; Loreau, Michel; Weis, Jerome J. (2007-11-13)."Impacts of plant diversity on biomass production increase through time because of species complementarity".Proceedings of the National Academy of Sciences.104 (46):18123–18128.Bibcode:2007PNAS..10418123C.doi:10.1073/pnas.0709069104.ISSN 0027-8424.PMC 2084307.PMID 17991772.
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  31. ^Carroll, Oliver; Batzer, Evan; Bharath, Siddharth; Borer, Elizabeth T.; Campana, Sofía; Esch, Ellen; Hautier, Yann; Ohlert, Timothy; Seabloom, Eric W.; Adler, Peter B.; Bakker, Jonathan D.; Biederman, Lori; Bugalho, Miguel N.; Caldeira, Maria; Chen, Qingqing (2021-12-27). Penuelas, Josep (ed.)."Nutrient identity modifies the destabilising effects of eutrophication in grasslands".Ecology Letters.25 (4):754–765.doi:10.1111/ele.13946.hdl:1874/419064.ISSN 1461-023X.PMID 34957674.S2CID 245517664.
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  33. ^abSoranno, Patricia A.; Hanly, Patrick J.; Webster, Katherine E.; Wagner, Tyler; McDonald, Andrew; Shuvo, Arnab; Schliep, Erin M.; Reinl, Kaitlin L.; McCullough, Ian M.; Tan, Pang-Ning; Lottig, Noah R.; Spence Cheruvelil, Kendra (2025-03-04)."Abrupt changes in algal biomass of thousands of US lakes are related to climate and are more likely in low-disturbance watersheds".Proceedings of the National Academy of Sciences.122 (9) e2416172122.doi:10.1073/pnas.2416172122.PMC 11892623.
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