Moving carbon between spheres, the potential oxalate-carbonate pathway of Brosimum alicastrum Sw.; Moraceae

Aims: The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO₂ into the geologic reservoir as CaCO₃; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Br...

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Published inPlant and soil Vol. 412; no. 1/2; pp. 465 - 479
Main Authors Rowley, Mike C., Estrada-Medina, Héctor, Tzec-Gamboa, Magnolia, Rozin, Aviram, Cailleau, Guillaume, Verrecchia, Eric P., Green, Iain
Format Journal Article
LanguageEnglish
Published Cham Springer 01.03.2017
Springer International Publishing
Springer Nature B.V
Subjects
Agroforestry
alkalinization
Biomedical and Life Sciences
Brosimum alicastrum
Calcareous soils
Calcium
calcium carbonate
calcium oxalate
carbon
Carbon cycle
Carbon dioxide
Carbonates
Chemical properties
Ecological research
Ecology
Environmental aspects
Haiti
Life Sciences
Mexico
Moraceae
Neotropics
Oxalates
Physiological aspects
Plant Physiology
Plant Sciences
Regular Article
Soil Science & Conservation
Soils
Studies
Trees
Haiti
Mexico
ASW, Caribbean Sea, Greater Antilles, Haiti
Oxalate-Carbonate Pathway (OCP)
Calcium oxalate
Carbon-calcium cycle
Oxalotrophic bacteria
Online AccessGet full text

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Abstract Aims: The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO₂ into the geologic reservoir as CaCO₃; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum, a Neotropical species with agroforestry potential (ca. 70-200 kg-nuts yr⁻¹), in the calcareous soils of Haiti and Mexico. Methods / results: Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg⁻¹) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO₃ concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Conclusions: Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum, and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
AbstractList Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO 2 into the geologic reservoir as CaCO 3 ; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum , a Neotropical species with agroforestry potential ( ca. 70–200 kg-nuts yr −1 ), in the calcareous soils of Haiti and Mexico. Methods / results Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg −1 ) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO 3 concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Conclusions Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum , and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
Aims: The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO₂ into the geologic reservoir as CaCO₃; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum, a Neotropical species with agroforestry potential (ca. 70-200 kg-nuts yr⁻¹), in the calcareous soils of Haiti and Mexico. Methods / results: Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg⁻¹) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO₃ concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Conclusions: Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum, and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO sub(2) into the geologic reservoir as CaCO sub(3); however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum, a Neotropical species with agroforestry potential (ca. 70-200 kg-nuts yr super(-1)), in the calcareous soils of Haiti and Mexico. Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg super(-1)) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO sub(3) concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum, and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO.sub.2 into the geologic reservoir as CaCO.sub.3; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum, a Neotropical species with agroforestry potential (ca. 70-200 kg-nuts yr.sup.-1), in the calcareous soils of Haiti and Mexico. Methods / results Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg.sup.-1) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO.sub.3 concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Conclusions Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum, and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO2 into the geologic reservoir as CaCO3; however, until now all investigations on this process have focused on species with limited food benefits. This study evaluates a potential OCP associated with Brosimum alicastrum, a Neotropical species with agroforestry potential (ca. 70-200 kg-nuts yr-1), in the calcareous soils of Haiti and Mexico. Methods / results Enzymatic analysis demonstrated significant concentrations of calcium oxalate (5.97 % D.W.) were associated with B. alicastrum tissue in all sample sites. The presence of oxalotrophism was also confirmed with microbiological analyses in both countries. High concentrations of total calcium (>7 g kg-1) and lithogenic carbonate obscured the localised alkalinisation and identification of secondary carbonate associated with the OCP at most sample sites, except Ma Rouge, Haiti. Soils adjacent to subjects in Ma Rouge demonstrated an increase in pH (0.63) and CaCO3 concentration (5.9 %) that, when coupled with root-like secondary carbonate deposits in Mexico, implies that the OCP does also occur in calcareous soils. Conclusions Therefore this study confirms that the OCP also occurs in calcareous soils, adjacent to B. alicastrum, and could play a fundamental and un-accounted role in the global calcium-carbon coupled cycle.
Audience Academic
Author Cailleau, Guillaume
Green, Iain
Tzec-Gamboa, Magnolia
Rozin, Aviram
Estrada-Medina, Héctor
Rowley, Mike C.
Verrecchia, Eric P.
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  surname: Verrecchia
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ContentType Journal Article
Copyright Springer Science+Business Media 2017
The Author(s) 2016
COPYRIGHT 2017 Springer
Plant and Soil is a copyright of Springer, 2017.
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Issue 1/2
Keywords Oxalate-Carbonate Pathway (OCP)
Calcium oxalate
Carbon-calcium cycle
Oxalotrophic bacteria
Language English
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PublicationSubtitle An International Journal on Plant-Soil Relationships
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Snippet Aims: The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO₂ into the geologic reservoir as CaCO₃; however, until now...
Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO 2 into the geologic reservoir as CaCO 3 ; however, until now...
Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO.sub.2 into the geologic reservoir as CaCO.sub.3; however,...
Aims The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO2 into the geologic reservoir as CaCO3; however, until now...
The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO sub(2) into the geologic reservoir as CaCO sub(3); however, until...
AIMS: The Oxalate-Carbonate Pathway (OCP) is a biogeochemical process that transfers atmospheric CO₂ into the geologic reservoir as CaCO₃; however, until now...
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SubjectTerms Agroforestry
alkalinization
Biomedical and Life Sciences
Brosimum alicastrum
Calcareous soils
Calcium
calcium carbonate
calcium oxalate
carbon
Carbon cycle
Carbon dioxide
Carbonates
Chemical properties
Ecological research
Ecology
Environmental aspects
Haiti
Life Sciences
Mexico
Moraceae
Neotropics
Oxalates
Physiological aspects
Plant Physiology
Plant Sciences
Regular Article
Soil Science & Conservation
Soils
Studies
Trees
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  providerName: Springer Nature
Title Moving carbon between spheres, the potential oxalate-carbonate pathway of Brosimum alicastrum Sw.; Moraceae
URI https://www.jstor.org/stable/44245281
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