Coarse woody debris in Douglas-fir forests of western Oregon and Washington

Amounts and structural characteristics of coarse woody debris (CWD) were examined in relation to stand age and site moisture condition in 196 Pseudotsuga menziesii stands in western Oregon and Washington. Stands ranged from 40 to 900 yr old, and most if not all, originated after fire. In a chronoseq...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Ecology (Durham) 1988-12, Vol.69 (6), p.1689-1702
Hauptverfasser: Spies, Thomas A., Franklin, Jerry F., Thomas, Ted B.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 1702
container_issue 6
container_start_page 1689
container_title Ecology (Durham)
container_volume 69
creator Spies, Thomas A.
Franklin, Jerry F.
Thomas, Ted B.
description Amounts and structural characteristics of coarse woody debris (CWD) were examined in relation to stand age and site moisture condition in 196 Pseudotsuga menziesii stands in western Oregon and Washington. Stands ranged from 40 to 900 yr old, and most if not all, originated after fire. In a chronosequence from the Cascade range, the amount of CWD followed a U-shaped pattern for stands
doi_str_mv 10.2307/1941147
format Article
fullrecord <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_15154287</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>1941147</jstor_id><sourcerecordid>1941147</sourcerecordid><originalsourceid>FETCH-LOGICAL-c4699-95357e633fd024a152bc46e0069733737fb2a34706288a83e408ada1c1c2518e3</originalsourceid><addsrcrecordid>eNp90U1rVDEUBuBQFDpWcd9VoMWurubkO0sZaxULXWgRV-HMvcn0DrdJm8wwzL83ZQaFgmaTwHl4eTkh5C2w91ww8wGcBJDmiMzACdc5MOwFmTEGvHNa2WPyqtYVaweknZFv84ylBrrNedjRISzKWOmY6Ke8WU5YuzgWGnMJdV1pjnTbHqEkelPCMieKaaA_sd6NabnO6TV5GXGq4c3hPiG3ny9_zL901zdXX-cfr7teatcaKaFM0ELEgXGJoPiiDQJj2hkhjDBxwVFIwzS3Fq0IklkcEHrouQIbxAl5t899KPlx0xr5-7H2YZowhbypHhQoya1p8OwZXOVNSa2bB-605NpY1dTFXvUl11pC9A9lvMey88D800r9YaVNnh_ysPY4xYKpH-sfbriyoJ6Y2LPtOIXdv9L85fwXOGu106Ct-xu-qutc_tPhdM8iZo_L9l3-9rt1TAvLxG9fqpRi</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1296426785</pqid></control><display><type>article</type><title>Coarse woody debris in Douglas-fir forests of western Oregon and Washington</title><source>Periodicals Index Online</source><source>JSTOR Archive Collection A-Z Listing</source><creator>Spies, Thomas A. ; Franklin, Jerry F. ; Thomas, Ted B.</creator><creatorcontrib>Spies, Thomas A. ; Franklin, Jerry F. ; Thomas, Ted B.</creatorcontrib><description>Amounts and structural characteristics of coarse woody debris (CWD) were examined in relation to stand age and site moisture condition in 196 Pseudotsuga menziesii stands in western Oregon and Washington. Stands ranged from 40 to 900 yr old, and most if not all, originated after fire. In a chronosequence from the Cascade range, the amount of CWD followed a U-shaped pattern for stands &lt;500 yr old, with moderate levels (92 Mg/ha) in stands &lt;80 yr old, lowest levels (&lt;50 Mg/ha) in stands 80-120 yr old, and highest levels (173 Mg/ha) in stands 400-500 yr old. After 500 yr the amounts of CWD declined to intermediate levels. In the southern Coast Range, lowest levels (32 Mg/ha) of CWD were in the youngest stands (60-80 yr), primarily because they inherited little CWD from the preceding (prefire) stands. In the Cascade Range, levels of CWD inherited from preceding stands were highest in young stands and declined to near zero by 250 yr. The overall decay rate constant (k) for snags and logs in the Cascade Range, calculated indirectly from the chronosequence, was 0.029 yr^-^1. Volume and biomass of CWD differed significantly in old-growth stands (&gt;200 yr old) among site moisture classes. Dry sites averaged 72 Mg/ha moderate sites 137 Mg/ha, and moist sites 174 Mg/ha. The dynamics of CWD were modeled for three fire histories, each beginning with an initial fire in an old-growth stand but differing in number and severity of subsequent fires. All three models exhibited low values of CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD during succession occurred when additional fires burned early in succession, which probably happened preceding many stands in the southern Coast Range. The results of the study indicate that a steady-state condition in CWD may not be reached for &gt;1000 yr, and that the nature and timing of disturbance play a key role in the dynamics of CWD in the dynamics of CWD in the region.</description><identifier>ISSN: 0012-9658</identifier><identifier>EISSN: 1939-9170</identifier><identifier>DOI: 10.2307/1941147</identifier><identifier>CODEN: ECGYAQ</identifier><language>eng</language><publisher>Washington, DC: The Ecological Society of America</publisher><subject>AGE ; Age structure ; Animal and plant ecology ; Animal, plant and microbial ecology ; Biological and medical sciences ; Biomass ; BOSQUES ; Coarse woody debris ; Coastal ranges ; Coniferous forests ; CONTENIDO DE AGUA EN EL SUELO ; DECHET DE BOIS ; DESECHOS DE LA MADERA ; ECOLOGICAL SUCCESSION ; EDAD ; ETAPAS DE DESARROLLO DE LA PLANTA ; Forest ecology ; Forest ecosystems ; FOREST FIRES ; Forest succession ; FORESTS ; FORET ; Fundamental and applied biological sciences. Psychology ; INCENDIE DE FORET ; INCENDIOS FORESTALES ; Old growth forests ; OREGON ; PLANT DEVELOPMENTAL STAGES ; PSEUDOTSUGA MENZIESII ; SOIL WATER CONTENT ; STADE DE DEVELOPPEMENT VEGETAL ; Stand age ; SUCCESSION ECOLOGIQUE ; SUCESION ECOLOGICA ; Synecology ; TENEUR EN EAU DU SOL ; Terrestrial ecosystems ; WASHINGTON ; WOOD RESIDUES</subject><ispartof>Ecology (Durham), 1988-12, Vol.69 (6), p.1689-1702</ispartof><rights>Copyright 1988 The Ecological Society of America</rights><rights>1988 by the Ecological Society of America</rights><rights>1989 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4699-95357e633fd024a152bc46e0069733737fb2a34706288a83e408ada1c1c2518e3</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1941147$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1941147$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27869,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=7258157$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Spies, Thomas A.</creatorcontrib><creatorcontrib>Franklin, Jerry F.</creatorcontrib><creatorcontrib>Thomas, Ted B.</creatorcontrib><title>Coarse woody debris in Douglas-fir forests of western Oregon and Washington</title><title>Ecology (Durham)</title><description>Amounts and structural characteristics of coarse woody debris (CWD) were examined in relation to stand age and site moisture condition in 196 Pseudotsuga menziesii stands in western Oregon and Washington. Stands ranged from 40 to 900 yr old, and most if not all, originated after fire. In a chronosequence from the Cascade range, the amount of CWD followed a U-shaped pattern for stands &lt;500 yr old, with moderate levels (92 Mg/ha) in stands &lt;80 yr old, lowest levels (&lt;50 Mg/ha) in stands 80-120 yr old, and highest levels (173 Mg/ha) in stands 400-500 yr old. After 500 yr the amounts of CWD declined to intermediate levels. In the southern Coast Range, lowest levels (32 Mg/ha) of CWD were in the youngest stands (60-80 yr), primarily because they inherited little CWD from the preceding (prefire) stands. In the Cascade Range, levels of CWD inherited from preceding stands were highest in young stands and declined to near zero by 250 yr. The overall decay rate constant (k) for snags and logs in the Cascade Range, calculated indirectly from the chronosequence, was 0.029 yr^-^1. Volume and biomass of CWD differed significantly in old-growth stands (&gt;200 yr old) among site moisture classes. Dry sites averaged 72 Mg/ha moderate sites 137 Mg/ha, and moist sites 174 Mg/ha. The dynamics of CWD were modeled for three fire histories, each beginning with an initial fire in an old-growth stand but differing in number and severity of subsequent fires. All three models exhibited low values of CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD during succession occurred when additional fires burned early in succession, which probably happened preceding many stands in the southern Coast Range. The results of the study indicate that a steady-state condition in CWD may not be reached for &gt;1000 yr, and that the nature and timing of disturbance play a key role in the dynamics of CWD in the dynamics of CWD in the region.</description><subject>AGE</subject><subject>Age structure</subject><subject>Animal and plant ecology</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Biomass</subject><subject>BOSQUES</subject><subject>Coarse woody debris</subject><subject>Coastal ranges</subject><subject>Coniferous forests</subject><subject>CONTENIDO DE AGUA EN EL SUELO</subject><subject>DECHET DE BOIS</subject><subject>DESECHOS DE LA MADERA</subject><subject>ECOLOGICAL SUCCESSION</subject><subject>EDAD</subject><subject>ETAPAS DE DESARROLLO DE LA PLANTA</subject><subject>Forest ecology</subject><subject>Forest ecosystems</subject><subject>FOREST FIRES</subject><subject>Forest succession</subject><subject>FORESTS</subject><subject>FORET</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>INCENDIE DE FORET</subject><subject>INCENDIOS FORESTALES</subject><subject>Old growth forests</subject><subject>OREGON</subject><subject>PLANT DEVELOPMENTAL STAGES</subject><subject>PSEUDOTSUGA MENZIESII</subject><subject>SOIL WATER CONTENT</subject><subject>STADE DE DEVELOPPEMENT VEGETAL</subject><subject>Stand age</subject><subject>SUCCESSION ECOLOGIQUE</subject><subject>SUCESION ECOLOGICA</subject><subject>Synecology</subject><subject>TENEUR EN EAU DU SOL</subject><subject>Terrestrial ecosystems</subject><subject>WASHINGTON</subject><subject>WOOD RESIDUES</subject><issn>0012-9658</issn><issn>1939-9170</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><sourceid>K30</sourceid><recordid>eNp90U1rVDEUBuBQFDpWcd9VoMWurubkO0sZaxULXWgRV-HMvcn0DrdJm8wwzL83ZQaFgmaTwHl4eTkh5C2w91ww8wGcBJDmiMzACdc5MOwFmTEGvHNa2WPyqtYVaweknZFv84ylBrrNedjRISzKWOmY6Ke8WU5YuzgWGnMJdV1pjnTbHqEkelPCMieKaaA_sd6NabnO6TV5GXGq4c3hPiG3ny9_zL901zdXX-cfr7teatcaKaFM0ELEgXGJoPiiDQJj2hkhjDBxwVFIwzS3Fq0IklkcEHrouQIbxAl5t899KPlx0xr5-7H2YZowhbypHhQoya1p8OwZXOVNSa2bB-605NpY1dTFXvUl11pC9A9lvMey88D800r9YaVNnh_ysPY4xYKpH-sfbriyoJ6Y2LPtOIXdv9L85fwXOGu106Ct-xu-qutc_tPhdM8iZo_L9l3-9rt1TAvLxG9fqpRi</recordid><startdate>198812</startdate><enddate>198812</enddate><creator>Spies, Thomas A.</creator><creator>Franklin, Jerry F.</creator><creator>Thomas, Ted B.</creator><general>The Ecological Society of America</general><general>Ecological Society of America</general><general>Brooklyn Botanic Garden, etc</general><scope>FBQ</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>FIXVA</scope><scope>FKUCP</scope><scope>IOIBA</scope><scope>K30</scope><scope>PAAUG</scope><scope>PAWHS</scope><scope>PAWZZ</scope><scope>PAXOH</scope><scope>PBHAV</scope><scope>PBQSW</scope><scope>PBYQZ</scope><scope>PCIWU</scope><scope>PCMID</scope><scope>PCZJX</scope><scope>PDGRG</scope><scope>PDWWI</scope><scope>PETMR</scope><scope>PFVGT</scope><scope>PGXDX</scope><scope>PIHIL</scope><scope>PISVA</scope><scope>PJCTQ</scope><scope>PJTMS</scope><scope>PLCHJ</scope><scope>PMHAD</scope><scope>PNQDJ</scope><scope>POUND</scope><scope>PPLAD</scope><scope>PQAPC</scope><scope>PQCAN</scope><scope>PQCMW</scope><scope>PQEME</scope><scope>PQHKH</scope><scope>PQMID</scope><scope>PQNCT</scope><scope>PQNET</scope><scope>PQSCT</scope><scope>PQSET</scope><scope>PSVJG</scope><scope>PVMQY</scope><scope>PZGFC</scope><scope>7SN</scope><scope>C1K</scope></search><sort><creationdate>198812</creationdate><title>Coarse woody debris in Douglas-fir forests of western Oregon and Washington</title><author>Spies, Thomas A. ; Franklin, Jerry F. ; Thomas, Ted B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c4699-95357e633fd024a152bc46e0069733737fb2a34706288a83e408ada1c1c2518e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>AGE</topic><topic>Age structure</topic><topic>Animal and plant ecology</topic><topic>Animal, plant and microbial ecology</topic><topic>Biological and medical sciences</topic><topic>Biomass</topic><topic>BOSQUES</topic><topic>Coarse woody debris</topic><topic>Coastal ranges</topic><topic>Coniferous forests</topic><topic>CONTENIDO DE AGUA EN EL SUELO</topic><topic>DECHET DE BOIS</topic><topic>DESECHOS DE LA MADERA</topic><topic>ECOLOGICAL SUCCESSION</topic><topic>EDAD</topic><topic>ETAPAS DE DESARROLLO DE LA PLANTA</topic><topic>Forest ecology</topic><topic>Forest ecosystems</topic><topic>FOREST FIRES</topic><topic>Forest succession</topic><topic>FORESTS</topic><topic>FORET</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>INCENDIE DE FORET</topic><topic>INCENDIOS FORESTALES</topic><topic>Old growth forests</topic><topic>OREGON</topic><topic>PLANT DEVELOPMENTAL STAGES</topic><topic>PSEUDOTSUGA MENZIESII</topic><topic>SOIL WATER CONTENT</topic><topic>STADE DE DEVELOPPEMENT VEGETAL</topic><topic>Stand age</topic><topic>SUCCESSION ECOLOGIQUE</topic><topic>SUCESION ECOLOGICA</topic><topic>Synecology</topic><topic>TENEUR EN EAU DU SOL</topic><topic>Terrestrial ecosystems</topic><topic>WASHINGTON</topic><topic>WOOD RESIDUES</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Spies, Thomas A.</creatorcontrib><creatorcontrib>Franklin, Jerry F.</creatorcontrib><creatorcontrib>Thomas, Ted B.</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Periodicals Index Online Segment 03</collection><collection>Periodicals Index Online Segment 04</collection><collection>Periodicals Index Online Segment 29</collection><collection>Periodicals Index Online</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - West</collection><collection>Primary Sources Access (Plan D) - International</collection><collection>Primary Sources Access &amp; Build (Plan A) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Midwest</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Northeast</collection><collection>Primary Sources Access (Plan D) - Southeast</collection><collection>Primary Sources Access (Plan D) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Southeast</collection><collection>Primary Sources Access (Plan D) - South Central</collection><collection>Primary Sources Access &amp; Build (Plan A) - UK / I</collection><collection>Primary Sources Access (Plan D) - Canada</collection><collection>Primary Sources Access (Plan D) - EMEALA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - South Central</collection><collection>Primary Sources Access &amp; Build (Plan A) - International</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - International</collection><collection>Primary Sources Access (Plan D) - West</collection><collection>Periodicals Index Online Segments 1-50</collection><collection>Primary Sources Access (Plan D) - APAC</collection><collection>Primary Sources Access (Plan D) - Midwest</collection><collection>Primary Sources Access (Plan D) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Canada</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - EMEALA</collection><collection>Primary Sources Access &amp; Build (Plan A) - APAC</collection><collection>Primary Sources Access &amp; Build (Plan A) - Canada</collection><collection>Primary Sources Access &amp; Build (Plan A) - West</collection><collection>Primary Sources Access &amp; Build (Plan A) - EMEALA</collection><collection>Primary Sources Access (Plan D) - Northeast</collection><collection>Primary Sources Access &amp; Build (Plan A) - Midwest</collection><collection>Primary Sources Access &amp; Build (Plan A) - North Central</collection><collection>Primary Sources Access &amp; Build (Plan A) - Northeast</collection><collection>Primary Sources Access &amp; Build (Plan A) - South Central</collection><collection>Primary Sources Access &amp; Build (Plan A) - Southeast</collection><collection>Primary Sources Access (Plan D) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - APAC</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - MEA</collection><collection>Ecology Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Ecology (Durham)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Spies, Thomas A.</au><au>Franklin, Jerry F.</au><au>Thomas, Ted B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coarse woody debris in Douglas-fir forests of western Oregon and Washington</atitle><jtitle>Ecology (Durham)</jtitle><date>1988-12</date><risdate>1988</risdate><volume>69</volume><issue>6</issue><spage>1689</spage><epage>1702</epage><pages>1689-1702</pages><issn>0012-9658</issn><eissn>1939-9170</eissn><coden>ECGYAQ</coden><abstract>Amounts and structural characteristics of coarse woody debris (CWD) were examined in relation to stand age and site moisture condition in 196 Pseudotsuga menziesii stands in western Oregon and Washington. Stands ranged from 40 to 900 yr old, and most if not all, originated after fire. In a chronosequence from the Cascade range, the amount of CWD followed a U-shaped pattern for stands &lt;500 yr old, with moderate levels (92 Mg/ha) in stands &lt;80 yr old, lowest levels (&lt;50 Mg/ha) in stands 80-120 yr old, and highest levels (173 Mg/ha) in stands 400-500 yr old. After 500 yr the amounts of CWD declined to intermediate levels. In the southern Coast Range, lowest levels (32 Mg/ha) of CWD were in the youngest stands (60-80 yr), primarily because they inherited little CWD from the preceding (prefire) stands. In the Cascade Range, levels of CWD inherited from preceding stands were highest in young stands and declined to near zero by 250 yr. The overall decay rate constant (k) for snags and logs in the Cascade Range, calculated indirectly from the chronosequence, was 0.029 yr^-^1. Volume and biomass of CWD differed significantly in old-growth stands (&gt;200 yr old) among site moisture classes. Dry sites averaged 72 Mg/ha moderate sites 137 Mg/ha, and moist sites 174 Mg/ha. The dynamics of CWD were modeled for three fire histories, each beginning with an initial fire in an old-growth stand but differing in number and severity of subsequent fires. All three models exhibited low values of CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD between 80 and 200 yr. The lowest and most prolonged minimum in CWD during succession occurred when additional fires burned early in succession, which probably happened preceding many stands in the southern Coast Range. The results of the study indicate that a steady-state condition in CWD may not be reached for &gt;1000 yr, and that the nature and timing of disturbance play a key role in the dynamics of CWD in the dynamics of CWD in the region.</abstract><cop>Washington, DC</cop><pub>The Ecological Society of America</pub><doi>10.2307/1941147</doi><tpages>14</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0012-9658
ispartof Ecology (Durham), 1988-12, Vol.69 (6), p.1689-1702
issn 0012-9658
1939-9170
language eng
recordid cdi_proquest_miscellaneous_15154287
source Periodicals Index Online; JSTOR Archive Collection A-Z Listing
subjects AGE
Age structure
Animal and plant ecology
Animal, plant and microbial ecology
Biological and medical sciences
Biomass
BOSQUES
Coarse woody debris
Coastal ranges
Coniferous forests
CONTENIDO DE AGUA EN EL SUELO
DECHET DE BOIS
DESECHOS DE LA MADERA
ECOLOGICAL SUCCESSION
EDAD
ETAPAS DE DESARROLLO DE LA PLANTA
Forest ecology
Forest ecosystems
FOREST FIRES
Forest succession
FORESTS
FORET
Fundamental and applied biological sciences. Psychology
INCENDIE DE FORET
INCENDIOS FORESTALES
Old growth forests
OREGON
PLANT DEVELOPMENTAL STAGES
PSEUDOTSUGA MENZIESII
SOIL WATER CONTENT
STADE DE DEVELOPPEMENT VEGETAL
Stand age
SUCCESSION ECOLOGIQUE
SUCESION ECOLOGICA
Synecology
TENEUR EN EAU DU SOL
Terrestrial ecosystems
WASHINGTON
WOOD RESIDUES
title Coarse woody debris in Douglas-fir forests of western Oregon and Washington
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-07T03%3A47%3A54IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Coarse%20woody%20debris%20in%20Douglas-fir%20forests%20of%20western%20Oregon%20and%20Washington&rft.jtitle=Ecology%20(Durham)&rft.au=Spies,%20Thomas%20A.&rft.date=1988-12&rft.volume=69&rft.issue=6&rft.spage=1689&rft.epage=1702&rft.pages=1689-1702&rft.issn=0012-9658&rft.eissn=1939-9170&rft.coden=ECGYAQ&rft_id=info:doi/10.2307/1941147&rft_dat=%3Cjstor_proqu%3E1941147%3C/jstor_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1296426785&rft_id=info:pmid/&rft_jstor_id=1941147&rfr_iscdi=true