Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests
We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine ( Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and...
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| creator | Peichl, Matthias Arain, M. Altaf |
| description | We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (
Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass ( |
| doi_str_mv | 10.1016/j.agrformet.2006.08.004 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_20092856</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0168192306002188</els_id><sourcerecordid>20092856</sourcerecordid><originalsourceid>FETCH-LOGICAL-c436t-4adb7dea98e666d97a928587f9c3c755ab2d6236cddf76e57fc3dd1c1d0612843</originalsourceid><addsrcrecordid>eNqFkM1u3CAURlGVSp2kfYaw6s4uPzbYy1GUNpUiZZHOGmG4HjGyjcNlEuXtiztVt90AQudcPj5CbjmrOePq26m2xzTGNEOuBWOqZl3NWPOB7HinZSVEw67IrpBdxXshP5FrxBNjXGjd78jLfoivUFG7eDrAFN-OKZ7LGVzEd8ww0yHE2SL-IZxNQ1zoGuOENCzljtojVAgvZ1gc0DjSoqyQbAa6hqUsk12yzaFYJSNgxs_k42gnhC9_9xty-H7_6-6henz68fNu_1i5RqpcNdYP2oPtO1BK-V7bXnRtp8feSafb1g7CKyGV837UClo9Ouk9d9wzxUXXyBvy9TJ3TbHEw2zmgA6mEgjiGU3papuoCqgvoEsRMcFo1hRmm94NZ2ar2JzMv4o3TRnWmVJxMW8v5mjjhgQ0h2fBuGSci0bJthD7CwHlp68BkkEXtqp8SOCy8TH895Xf72OVIw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>20092856</pqid></control><display><type>article</type><title>Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests</title><source>Access via ScienceDirect (Elsevier)</source><creator>Peichl, Matthias ; Arain, M. Altaf</creator><creatorcontrib>Peichl, Matthias ; Arain, M. Altaf</creatorcontrib><description>We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (
Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass (<5
mm) and mineral soil C stocks were estimated from soil cores. Aboveground tree biomass became the major ecosystem C pool with increasing age, reaching 0.5, 66, 92, and 176
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Tree root biomass increased from 0.1 to 10, 18, 38
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, contributing considerably to the total ecosystem C in the three older stands. Forest floor C was 0.8, 7.5, 5.4, and 12.1
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, indicating an increase during the first two decades, but no further age-effect during the later growth phase. Mineral soil C was age-independent with 37.2, 33.9, 39.1, and 36.7
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Aboveground ecosystem C increased with age from 3 to 40, 52, and 100
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, due to an increase in aboveground tree biomass. Belowground ecosystem C remained similiar in the early decades after establishment with 37, 39, and 39
t
C
ha
−1 in the 2-, 15-, and 30-year-old stands, but increased to 56
t
C
ha
−1 in the 65-year-old stand due to an increase in root biomass. The difference in total ecosystem C between the 2- and 65-year-old stand was 116
t
C
ha
−1. Our results highlight the importance of considering the successional development of forest ecosystem C pools, when estimating C sink potentials over their complete life cycle.</description><identifier>ISSN: 0168-1923</identifier><identifier>EISSN: 1873-2240</identifier><identifier>DOI: 10.1016/j.agrformet.2006.08.004</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Afforestation ; Biomass ; carbon ; Carbon sequestration ; Carbon stock ; Chronosequence ; chronosequences ; dead wood ; dry matter accumulation ; forest ecology ; forest ecosystems ; forest litter ; forest plantations ; forest soils ; forest trees ; Great lakes region ; Pinus strobus ; Plantation ; soil organic carbon ; Temperate conifer forest ; tree age ; White pine</subject><ispartof>Agricultural and forest meteorology, 2006-11, Vol.140 (1), p.51-63</ispartof><rights>2006 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c436t-4adb7dea98e666d97a928587f9c3c755ab2d6236cddf76e57fc3dd1c1d0612843</citedby><cites>FETCH-LOGICAL-c436t-4adb7dea98e666d97a928587f9c3c755ab2d6236cddf76e57fc3dd1c1d0612843</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.agrformet.2006.08.004$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids></links><search><creatorcontrib>Peichl, Matthias</creatorcontrib><creatorcontrib>Arain, M. Altaf</creatorcontrib><title>Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests</title><title>Agricultural and forest meteorology</title><description>We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (
Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass (<5
mm) and mineral soil C stocks were estimated from soil cores. Aboveground tree biomass became the major ecosystem C pool with increasing age, reaching 0.5, 66, 92, and 176
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Tree root biomass increased from 0.1 to 10, 18, 38
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, contributing considerably to the total ecosystem C in the three older stands. Forest floor C was 0.8, 7.5, 5.4, and 12.1
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, indicating an increase during the first two decades, but no further age-effect during the later growth phase. Mineral soil C was age-independent with 37.2, 33.9, 39.1, and 36.7
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Aboveground ecosystem C increased with age from 3 to 40, 52, and 100
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, due to an increase in aboveground tree biomass. Belowground ecosystem C remained similiar in the early decades after establishment with 37, 39, and 39
t
C
ha
−1 in the 2-, 15-, and 30-year-old stands, but increased to 56
t
C
ha
−1 in the 65-year-old stand due to an increase in root biomass. The difference in total ecosystem C between the 2- and 65-year-old stand was 116
t
C
ha
−1. Our results highlight the importance of considering the successional development of forest ecosystem C pools, when estimating C sink potentials over their complete life cycle.</description><subject>Afforestation</subject><subject>Biomass</subject><subject>carbon</subject><subject>Carbon sequestration</subject><subject>Carbon stock</subject><subject>Chronosequence</subject><subject>chronosequences</subject><subject>dead wood</subject><subject>dry matter accumulation</subject><subject>forest ecology</subject><subject>forest ecosystems</subject><subject>forest litter</subject><subject>forest plantations</subject><subject>forest soils</subject><subject>forest trees</subject><subject>Great lakes region</subject><subject>Pinus strobus</subject><subject>Plantation</subject><subject>soil organic carbon</subject><subject>Temperate conifer forest</subject><subject>tree age</subject><subject>White pine</subject><issn>0168-1923</issn><issn>1873-2240</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2006</creationdate><recordtype>article</recordtype><recordid>eNqFkM1u3CAURlGVSp2kfYaw6s4uPzbYy1GUNpUiZZHOGmG4HjGyjcNlEuXtiztVt90AQudcPj5CbjmrOePq26m2xzTGNEOuBWOqZl3NWPOB7HinZSVEw67IrpBdxXshP5FrxBNjXGjd78jLfoivUFG7eDrAFN-OKZ7LGVzEd8ww0yHE2SL-IZxNQ1zoGuOENCzljtojVAgvZ1gc0DjSoqyQbAa6hqUsk12yzaFYJSNgxs_k42gnhC9_9xty-H7_6-6henz68fNu_1i5RqpcNdYP2oPtO1BK-V7bXnRtp8feSafb1g7CKyGV837UClo9Ouk9d9wzxUXXyBvy9TJ3TbHEw2zmgA6mEgjiGU3papuoCqgvoEsRMcFo1hRmm94NZ2ar2JzMv4o3TRnWmVJxMW8v5mjjhgQ0h2fBuGSci0bJthD7CwHlp68BkkEXtqp8SOCy8TH895Xf72OVIw</recordid><startdate>20061101</startdate><enddate>20061101</enddate><creator>Peichl, Matthias</creator><creator>Arain, M. Altaf</creator><general>Elsevier B.V</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7U6</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20061101</creationdate><title>Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests</title><author>Peichl, Matthias ; Arain, M. Altaf</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c436t-4adb7dea98e666d97a928587f9c3c755ab2d6236cddf76e57fc3dd1c1d0612843</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2006</creationdate><topic>Afforestation</topic><topic>Biomass</topic><topic>carbon</topic><topic>Carbon sequestration</topic><topic>Carbon stock</topic><topic>Chronosequence</topic><topic>chronosequences</topic><topic>dead wood</topic><topic>dry matter accumulation</topic><topic>forest ecology</topic><topic>forest ecosystems</topic><topic>forest litter</topic><topic>forest plantations</topic><topic>forest soils</topic><topic>forest trees</topic><topic>Great lakes region</topic><topic>Pinus strobus</topic><topic>Plantation</topic><topic>soil organic carbon</topic><topic>Temperate conifer forest</topic><topic>tree age</topic><topic>White pine</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Peichl, Matthias</creatorcontrib><creatorcontrib>Arain, M. Altaf</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Agricultural and forest meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Peichl, Matthias</au><au>Arain, M. Altaf</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests</atitle><jtitle>Agricultural and forest meteorology</jtitle><date>2006-11-01</date><risdate>2006</risdate><volume>140</volume><issue>1</issue><spage>51</spage><epage>63</epage><pages>51-63</pages><issn>0168-1923</issn><eissn>1873-2240</eissn><abstract>We assessed the successional development of above- and belowground ecosystem biomass and carbon (C) pools in an age-sequence of four White pine (
Pinus strobus L.) plantation stands (2-, 15-, 30-, and 65-years-old) in Southern Ontario, Canada. Biomass and C stocks of above- and belowground live and dead tree biomass, understorey and forest ground vegetation, forest floor C (LFH-layer), and woody debris were determined from plot-level inventories and destructive tree sampling. Small root biomass (<5
mm) and mineral soil C stocks were estimated from soil cores. Aboveground tree biomass became the major ecosystem C pool with increasing age, reaching 0.5, 66, 92, and 176
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Tree root biomass increased from 0.1 to 10, 18, 38
t
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, contributing considerably to the total ecosystem C in the three older stands. Forest floor C was 0.8, 7.5, 5.4, and 12.1
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, indicating an increase during the first two decades, but no further age-effect during the later growth phase. Mineral soil C was age-independent with 37.2, 33.9, 39.1, and 36.7
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively. Aboveground ecosystem C increased with age from 3 to 40, 52, and 100
t
C
ha
−1 in the 2-, 15-, 30-, and 65-year-old stands, respectively, due to an increase in aboveground tree biomass. Belowground ecosystem C remained similiar in the early decades after establishment with 37, 39, and 39
t
C
ha
−1 in the 2-, 15-, and 30-year-old stands, but increased to 56
t
C
ha
−1 in the 65-year-old stand due to an increase in root biomass. The difference in total ecosystem C between the 2- and 65-year-old stand was 116
t
C
ha
−1. Our results highlight the importance of considering the successional development of forest ecosystem C pools, when estimating C sink potentials over their complete life cycle.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.agrformet.2006.08.004</doi><tpages>13</tpages></addata></record> |
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| ispartof | Agricultural and forest meteorology, 2006-11, Vol.140 (1), p.51-63 |
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| language | eng |
| recordid | cdi_proquest_miscellaneous_20092856 |
| source | Access via ScienceDirect (Elsevier) |
| subjects | Afforestation Biomass carbon Carbon sequestration Carbon stock Chronosequence chronosequences dead wood dry matter accumulation forest ecology forest ecosystems forest litter forest plantations forest soils forest trees Great lakes region Pinus strobus Plantation soil organic carbon Temperate conifer forest tree age White pine |
| title | Above- and belowground ecosystem biomass and carbon pools in an age-sequence of temperate pine plantation forests |
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