Does chemosynthesis produce oxygen

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Gas-exchange experiments in showed that the gain in weight of a plant grown in a carefully weighed pot resulted from the uptake of carbon, which came entirely from absorbed carbon dioxide, and water taken up by plant roots; the balance is oxygen, released back to the atmosphere. Almost half a century passed before the concept of chemical energy had developed sufficiently to permit the discovery in that light energy from the sun is stored as chemical energy in products formed during photosynthesis.

In chemical terms, photosynthesis is a light-energized oxidation—reduction process. Oxidation refers to the removal of electrons from a molecule; reduction refers to the gain of electrons by a molecule. Most of the removed electrons and hydrogen ions ultimately are transferred to carbon dioxide CO 2 , which is reduced to organic products. Other electrons and hydrogen ions are used to reduce nitrate and sulfate to amino and sulfhydryl groups in amino acids , which are the building blocks of proteins. In most green cells , carbohydrates —especially starch and the sugar sucrose —are the major direct organic products of photosynthesis.

The overall reaction in which carbohydrates—represented by the general formula CH 2 O —are formed during plant photosynthesis can be indicated by the following equation:. This equation is merely a summary statement, for the process of photosynthesis actually involves numerous reactions catalyzed by enzymes organic catalysts.

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During the first stage, the energy of light is absorbed and used to drive a series of electron transfers, resulting in the synthesis of ATP and the electron-donor-reduced nicotine adenine dinucleotide phosphate NADPH. This assimilation of inorganic carbon into organic compounds is called carbon fixation. During the 20th century, comparisons between photosynthetic processes in green plants and in certain photosynthetic sulfur bacteria provided important information about the photosynthetic mechanism.

Sulfur bacteria use hydrogen sulfide H 2 S as a source of hydrogen atoms and produce sulfur instead of oxygen during photosynthesis. The overall reaction is.

How Organisms Get Food

In the s Dutch biologist Cornelis van Niel recognized that the utilization of carbon dioxide to form organic compounds was similar in the two types of photosynthetic organisms. Suggesting that differences existed in the light-dependent stage and in the nature of the compounds used as a source of hydrogen atoms, he proposed that hydrogen was transferred from hydrogen sulfide in bacteria or water in green plants to an unknown acceptor called A , which was reduced to H 2 A. During the dark reactions, which are similar in both bacteria and green plants, the reduced acceptor H 2 A reacted with carbon dioxide CO 2 to form carbohydrate CH 2 O and to oxidize the unknown acceptor to A.

This putative reaction can be represented as:. By chemists were using heavy isotopes to follow the reactions of photosynthesis. Water marked with an isotope of oxygen 18 O was used in early experiments. Plants that photosynthesized in the presence of water containing H 2 18 O produced oxygen gas containing 18 O; those that photosynthesized in the presence of normal water produced normal oxygen gas. You are using an outdated browser.

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Chemosynthesis Definition and Examples

Plants and other autotrophs use it as fuel, maintaining one of nature's more grand and definitive biochemical cycles. Plants are the most familiar type of autotroph, but various others dot the global biosphere, often far from human eyes. Algae, phytoplankton and certain bacteria are autotrophs.

In particular, the bacteria that can survive deep in the sea are of special interest because of their chemosynthetic metabolism. Chemosynthesis is a process by which energy is derived via the microbial mediation of certain chemical reactions.

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The source of energy for chemosynthesis is energy liberated from a chemical reaction the oxidation of an inorganic substance rather than energy harvested from sunlight or other light. The carbon source remains CO 2 , and oxygen as O 2 must be present to operate on the inorganic molecule, but that inorganic molecule may be hydrogen gas H 2 , hydrogen sulfide H 2 S or ammonia NH 3 , depending on the environment in question. Whatever carbohydrate is formed for the cell's use will have the form CH 2 O N , as this is true of all carbohydrates by definition.

One chemosynthesis equation depicts the conversion of carbon dioxide to carbohydrate as hydrogen sulfide is oxidized to water and sulfur:.

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This is not precisely warm and welcoming, but inconsistent and sometimes violent heat is better than no heat at all if you have the right enzymatic equipment. Some "bacteria" in these so-called hydrothermal vent communities are actually Archaea , prokaryotic organisms closely related to bacteria and formerly called archaebacteria. One example is Methanopyrus kandleri , which tolerates very salty and very warm environments with unusual ease.

Chemosynthesis exploits chemical energy to convert inorganic carbon compounds into organic matter, in contrast with photosynthesis, which exploits the energy of light to produce organic matter. Energy is produced in chemosynthetic reactions from oxidizing reduced compounds.

Chemosynthesis Definition

There are a variety of chemosynthetic bacteria that carry out these reactions including nitrifying bacteria oxidizing NH 4 or NO 2 , sulfur bacteria oxidizing H 2 S, S, and other sulfur compounds , hydrogen bacteria oxidizing H 2 , methane bacteria oxidizing CH 4 , iron and manganese bacteria oxidizing reduced iron and manganese compounds , and carbon monoxide bacteria oxidizing CO.

This is not an exhaustive list and new modes of chemosynthesis as well as new chemosynthetic bacteria are still being discovered. Read full chapter. Microbial production by chemosynthesis occurs to a marked extent in layers having contact with the anaerobic zones of an aquatic system, especially in boundary layers between anaerobic and aerobic zones. As indicated in earlier discussions of the cycling of several elements, the anaerobic processes of decomposition of organic matter provide reduced inorganic compounds that serve as energy substrates for the chemoautotrophic bacteria.

Chemosynthetic secondary production becomes significant primarily in steep gradients of redox potential Sorokin, a , , Outside of these layers, chemosynthesis is very low in relation to total heterotrophic bacterial production Romanenko, ; Jordan and Likens, Chemosynthesis by bacteria is normally very low in the pelagic of streams, infertile waters, and lakes of intermediate productivity and becomes a significant contribution to the whole only in productive or meromictic lakes exhibiting steep redox gradients.

The ratio of dark CO 2 fixation almost all by heterotrophic metabolism of bacteria; see Gerletti, ; Romanenko, to photosynthetic fixation of CO 2 and bacterial chemosynthesis generally is small in oligotrophic waters. For example, the yr average of dark CO 2 fixation was This percentage is much less for the lake, about one-tenth, if the littoral photosynthesis of this lake is considered in addition to the carbon fixation of the phytoplankton. The ratio of photosynthetic to dark CO 2 fixation decreases in the transition to planktonic eutrophy and hypereutrophy.

In lakes that are deeper than Mirror Lake z m , 10 m , planktonic bacterial production probably accounts for a greater proportion of the total decomposition simply because particulate detritus would have a longer residence time in the water column. With further transition of the system or in lakes with a predominance of productivity by emergent macroflora and associated attached and littoral microflora, the relative contribution of dark CO 2 fixation to the DOC pool apparently decreases cf. Wetzel, TABLE While a voluminous nomenclature is available to differentiate among variations in these processes, for simplicity, chemosynthesis and photosynthesis are used here.

In photosynthesis, sunlight captured by proteins provides energy for the conversion of inorganic carbon carbon dioxide, CO 2 and water H 2 O into organic carbon carbohydrates, [CH 2 O] and oxygen O 2 eqn [1].

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Photosynthesis by plants is the basis for consumer and degradative food webs both on land and, as a rain of organic detritus derived from surface phytoplankton productivity, on the seabed. In the deep sea, detrital inputs of organic carbon are exceedingly small, accounting for the paucity of consumer biomass in abyssal muds. At hydrothermal vents, the supply of surface-derived organic material is overwhelmed by the supply of new organic carbon generated through chemical oxidation of hydrogen sulfide H 2 S eqn [2]. Metabolic fixation pathways for carbon can be identical in photosynthetic plants and chemosynthetic microorganisms, namely the Calvin—Benson cycle, but the energy-yielding processes that fuel the Calvin—Benson cycle photon capture versus chemical oxidation are distinctive.

High biomass at hydrothermal vents is in part a consequence of the aerobic nature of the process described in eqn [2]. Oxygen is used to oxidize the hydrogen sulfide, generating a large energy yield that in turn can fuel the production of large amounts of organic carbon Figure 1. Nonaerobic chemical reactions, such as oxidation of vent-supplied hydrogen H 2 by carbon dioxide CO 2 , can also support chemosynthesis at vents, but energy yields under such anaerobic conditions are much lower than from aerobic oxidation.

Microorganisms using these anaerobic reactions cannot by themselves support complex food webs and large invertebrates. Figure 1. Photosynthetic and chemosynthetic processes in the ocean. Sunlight fuels the generation of organic material CH 2 O from inorganic carbon dioxide CO 2 and water H 2 O by phytoplankton in surface, illuminated waters. In place of sunlight, the chemical oxidation of sulfide H 2 S by oxygen O 2 fuels the conversion of carbon dioxide to organic carbon by chemosynthetic bacteria. The physiological mechanisms for capturing chemical energy during chemosynthesis are diverse, and there are several descriptive qualifiers that define an organism based on its carbon and energy sources.

Typically, chemolithoautotrophs use compounds present in rocks or groundwater. Chemical electron donors include, but are not limited to, molecular hydrogen, reduced sulfur compounds, metals, and so on. Organisms that gain cellular energy from chemical transformations but use organic carbon compounds for their carbon source are chemoorganotrophs , and heterotrophs use organic carbon for cellular energy and carbon sources. Several studies have shown that chemolithoautotrophs can grow if organic carbon is present as mixotrophs , in which both chemolithoautotrophy and heterotrophy are expressed simultaneously.

Microorganisms also have oxygen requirements, and can respire aerobically, anaerobically, or ferment, all of which relates to electron acceptor utilization. Oxygen is the terminal electron acceptor for aerobic metabolic processes Table 1. In reducing environments, microbes that do not require oxygen anaerobes use a variety of alternative electron acceptors for respiration in a sequence of energetic, reduction reactions that occur along thermodynamic and redox gradients, from nitrate to carbon dioxide Table 1. There are several other energetically favorable, chemolithoautotrophic pathways that occur in the absence of oxygen, including sulfide oxidation via nitrate reduction and anaerobic ammonium oxidation anammox Table 1.

Differences and Similarities Between Chemosynthesis and Photosynthesis

Table 1. Louise M. Prockter, Robert T. Based on our terrestrial view, the primary ingredients for life are water, organic compounds, and chemical energy. Europa may have all three: water of the ocean, organic compounds that have been delivered to the satellite, and chemical energy from radiolysis and possibly chemosynthesis.