Spatial and temporal variation of roots, arbuscular mycorrhizal fungi, and plant and soil nutrients in a mature Pinot Noir (Vitis vinifera L.) vineyard in Oregon, USA

The spatial and temporal development of grapevine roots and associated mycorrhizal fungi was studied in 1999 and 2000 in a 21-year-old, Pinot Noir (Vitis vinifera L.) vineyard located on a Jory soil (Palehumult, silty clay loam) in Oregon, USA. The density of woody roots and fine (primary) roots dee...

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description The spatial and temporal development of grapevine roots and associated mycorrhizal fungi was studied in 1999 and 2000 in a 21-year-old, Pinot Noir (Vitis vinifera L.) vineyard located on a Jory soil (Palehumult, silty clay loam) in Oregon, USA. The density of woody roots and fine (primary) roots deemed to be physiologically active (based on color and cellular integrity) were determined at monthly intervals in the weed-free, vine row and in the alleyway between rows at two depths (0-50 and 50-100 cm). The majority of fine roots were growing in the vine row at 0-50 cm depth. Fine root density did not change dramatically over the 1999 or 2000 seasons until the time of fruit harvest in the fall. Apparently, new root growth kept pace with turnover (death) prior to harvest, but new root growth surpassed turnover in the fall after fruit harvest. Colonization of fine roots by arbuscular mycorrhizal fungi (AMF) was consistently high in the vine row at 0-50 cm depth, but was lower in roots growing in the alleyway, and in roots below 50 cm. The proportion of fine roots containing arbuscules (the site of nutrient exchange in arbuscular mycorrhizas) was also greatest for roots growing in the vine row at 0-50 cm depth. Arbuscular colonization of these roots increased prior to budbreak in the spring, reached a high level (50-60% root length) by early summer, and remained high until after the time of leaf senescence in late fall. Arbuscular colonization decreased rapidly by December of 1999 when November rainfall exceeded 200 mm, but did not decline by December of 2000 when November rainfall was below 80 mm. The availability of important plant nutrients in the soil, with the exception of Mg and Zn, was higher in the upper 50 cm of the soil profile where the majority of roots were found. In addition, available nitrate and phosphate were higher in the vine row than in the alleyway soil. Seasonal changes in leaf nutrient concentrations of Pinot Noir confirmed findings in other cultivars, but fluctuations of N, P, and K concentrations in fine roots over the season suggested that fine roots may play a role in nutrient storage, as well as nutrient uptake, in grapevines. Grapevines grown in Oregon direct significant resources to roots and AMF after fruit harvest and substantial post-harvest nutrient uptake may extend into the early winter.
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The density of woody roots and fine (primary) roots deemed to be physiologically active (based on color and cellular integrity) were determined at monthly intervals in the weed-free, vine row and in the alleyway between rows at two depths (0-50 and 50-100 cm). The majority of fine roots were growing in the vine row at 0-50 cm depth. Fine root density did not change dramatically over the 1999 or 2000 seasons until the time of fruit harvest in the fall. Apparently, new root growth kept pace with turnover (death) prior to harvest, but new root growth surpassed turnover in the fall after fruit harvest. Colonization of fine roots by arbuscular mycorrhizal fungi (AMF) was consistently high in the vine row at 0-50 cm depth, but was lower in roots growing in the alleyway, and in roots below 50 cm. The proportion of fine roots containing arbuscules (the site of nutrient exchange in arbuscular mycorrhizas) was also greatest for roots growing in the vine row at 0-50 cm depth. Arbuscular colonization of these roots increased prior to budbreak in the spring, reached a high level (50-60% root length) by early summer, and remained high until after the time of leaf senescence in late fall. Arbuscular colonization decreased rapidly by December of 1999 when November rainfall exceeded 200 mm, but did not decline by December of 2000 when November rainfall was below 80 mm. The availability of important plant nutrients in the soil, with the exception of Mg and Zn, was higher in the upper 50 cm of the soil profile where the majority of roots were found. In addition, available nitrate and phosphate were higher in the vine row than in the alleyway soil. Seasonal changes in leaf nutrient concentrations of Pinot Noir confirmed findings in other cultivars, but fluctuations of N, P, and K concentrations in fine roots over the season suggested that fine roots may play a role in nutrient storage, as well as nutrient uptake, in grapevines. 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Plant production ; grapes ; Leaves ; mature plants ; microbial colonization ; Microbiology ; mycorrhizal fungi ; Nitrate ; nutrient availability ; Nutrient concentrations ; Nutrient uptake ; Nutrients ; Orchard soils ; Phosphate ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Physiology ; Plant growth ; plant nutrition ; Plant roots ; Rainfall ; root growth ; rooting ; Roots ; Seasonal variations ; Senescence ; Soil ; Soil nutrients ; Soil profiles ; Soil samples ; Soil science ; Soil water ; soil-plant interactions ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Soils ; spatial variation ; Subsoil ; Symbiosis (nodules, symbiotic nitrogen fixation, mycorrhiza...) ; temporal variation ; Temporal variations ; Topsoil ; vesicular arbuscular mycorrhizae ; Vines ; Vineyards ; Vitaceae ; Vitis vinifera ; Zinc</subject><ispartof>Plant and soil, 2005-10, Vol.276 (1-2), p.219-234</ispartof><rights>2005 Springer</rights><rights>2006 INIST-CNRS</rights><rights>Springer 2005</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c412t-a5dac585377b0eb871023883474bfb70bfb75f640830961b1050d908173545593</citedby><cites>FETCH-LOGICAL-c412t-a5dac585377b0eb871023883474bfb70bfb75f640830961b1050d908173545593</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/24124993$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/24124993$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=17309925$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Schreiner, R.P</creatorcontrib><title>Spatial and temporal variation of roots, arbuscular mycorrhizal fungi, and plant and soil nutrients in a mature Pinot Noir (Vitis vinifera L.) vineyard in Oregon, USA</title><title>Plant and soil</title><description>The spatial and temporal development of grapevine roots and associated mycorrhizal fungi was studied in 1999 and 2000 in a 21-year-old, Pinot Noir (Vitis vinifera L.) vineyard located on a Jory soil (Palehumult, silty clay loam) in Oregon, USA. The density of woody roots and fine (primary) roots deemed to be physiologically active (based on color and cellular integrity) were determined at monthly intervals in the weed-free, vine row and in the alleyway between rows at two depths (0-50 and 50-100 cm). The majority of fine roots were growing in the vine row at 0-50 cm depth. Fine root density did not change dramatically over the 1999 or 2000 seasons until the time of fruit harvest in the fall. Apparently, new root growth kept pace with turnover (death) prior to harvest, but new root growth surpassed turnover in the fall after fruit harvest. Colonization of fine roots by arbuscular mycorrhizal fungi (AMF) was consistently high in the vine row at 0-50 cm depth, but was lower in roots growing in the alleyway, and in roots below 50 cm. The proportion of fine roots containing arbuscules (the site of nutrient exchange in arbuscular mycorrhizas) was also greatest for roots growing in the vine row at 0-50 cm depth. Arbuscular colonization of these roots increased prior to budbreak in the spring, reached a high level (50-60% root length) by early summer, and remained high until after the time of leaf senescence in late fall. Arbuscular colonization decreased rapidly by December of 1999 when November rainfall exceeded 200 mm, but did not decline by December of 2000 when November rainfall was below 80 mm. The availability of important plant nutrients in the soil, with the exception of Mg and Zn, was higher in the upper 50 cm of the soil profile where the majority of roots were found. In addition, available nitrate and phosphate were higher in the vine row than in the alleyway soil. Seasonal changes in leaf nutrient concentrations of Pinot Noir confirmed findings in other cultivars, but fluctuations of N, P, and K concentrations in fine roots over the season suggested that fine roots may play a role in nutrient storage, as well as nutrient uptake, in grapevines. Grapevines grown in Oregon direct significant resources to roots and AMF after fruit harvest and substantial post-harvest nutrient uptake may extend into the early winter.</description><subject>Agrology</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Alleys</subject><subject>arbuscular mycorrhizas</subject><subject>Biochemistry and biology</subject><subject>Biological and medical sciences</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>Clay loam</subject><subject>Clays</subject><subject>climate change</subject><subject>Colonization</subject><subject>Color</subject><subject>Cultivars</subject><subject>Economic plant physiology</subject><subject>Forest ecosystems</subject><subject>Fruits</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Fungi</subject><subject>General agronomy. Plant production</subject><subject>grapes</subject><subject>Leaves</subject><subject>mature plants</subject><subject>microbial colonization</subject><subject>Microbiology</subject><subject>mycorrhizal fungi</subject><subject>Nitrate</subject><subject>nutrient availability</subject><subject>Nutrient concentrations</subject><subject>Nutrient uptake</subject><subject>Nutrients</subject><subject>Orchard soils</subject><subject>Phosphate</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Physiology</subject><subject>Plant growth</subject><subject>plant nutrition</subject><subject>Plant roots</subject><subject>Rainfall</subject><subject>root growth</subject><subject>rooting</subject><subject>Roots</subject><subject>Seasonal variations</subject><subject>Senescence</subject><subject>Soil</subject><subject>Soil nutrients</subject><subject>Soil profiles</subject><subject>Soil samples</subject><subject>Soil science</subject><subject>Soil water</subject><subject>soil-plant interactions</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. 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Soil science and plant productions</topic><topic>Alleys</topic><topic>arbuscular mycorrhizas</topic><topic>Biochemistry and biology</topic><topic>Biological and medical sciences</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>Clay loam</topic><topic>Clays</topic><topic>climate change</topic><topic>Colonization</topic><topic>Color</topic><topic>Cultivars</topic><topic>Economic plant physiology</topic><topic>Forest ecosystems</topic><topic>Fruits</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Fungi</topic><topic>General agronomy. Plant production</topic><topic>grapes</topic><topic>Leaves</topic><topic>mature plants</topic><topic>microbial colonization</topic><topic>Microbiology</topic><topic>mycorrhizal fungi</topic><topic>Nitrate</topic><topic>nutrient availability</topic><topic>Nutrient concentrations</topic><topic>Nutrient uptake</topic><topic>Nutrients</topic><topic>Orchard soils</topic><topic>Phosphate</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Physiology</topic><topic>Plant growth</topic><topic>plant nutrition</topic><topic>Plant roots</topic><topic>Rainfall</topic><topic>root growth</topic><topic>rooting</topic><topic>Roots</topic><topic>Seasonal variations</topic><topic>Senescence</topic><topic>Soil</topic><topic>Soil nutrients</topic><topic>Soil profiles</topic><topic>Soil samples</topic><topic>Soil science</topic><topic>Soil water</topic><topic>soil-plant interactions</topic><topic>Soil-plant relationships. Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Soils</topic><topic>spatial variation</topic><topic>Subsoil</topic><topic>Symbiosis (nodules, symbiotic nitrogen fixation, mycorrhiza...)</topic><topic>temporal variation</topic><topic>Temporal variations</topic><topic>Topsoil</topic><topic>vesicular arbuscular mycorrhizae</topic><topic>Vines</topic><topic>Vineyards</topic><topic>Vitaceae</topic><topic>Vitis vinifera</topic><topic>Zinc</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Schreiner, R.P</creatorcontrib><collection>AGRIS</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural &amp; Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Schreiner, R.P</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and temporal variation of roots, arbuscular mycorrhizal fungi, and plant and soil nutrients in a mature Pinot Noir (Vitis vinifera L.) vineyard in Oregon, USA</atitle><jtitle>Plant and soil</jtitle><date>2005-10-01</date><risdate>2005</risdate><volume>276</volume><issue>1-2</issue><spage>219</spage><epage>234</epage><pages>219-234</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>The spatial and temporal development of grapevine roots and associated mycorrhizal fungi was studied in 1999 and 2000 in a 21-year-old, Pinot Noir (Vitis vinifera L.) vineyard located on a Jory soil (Palehumult, silty clay loam) in Oregon, USA. The density of woody roots and fine (primary) roots deemed to be physiologically active (based on color and cellular integrity) were determined at monthly intervals in the weed-free, vine row and in the alleyway between rows at two depths (0-50 and 50-100 cm). The majority of fine roots were growing in the vine row at 0-50 cm depth. Fine root density did not change dramatically over the 1999 or 2000 seasons until the time of fruit harvest in the fall. Apparently, new root growth kept pace with turnover (death) prior to harvest, but new root growth surpassed turnover in the fall after fruit harvest. Colonization of fine roots by arbuscular mycorrhizal fungi (AMF) was consistently high in the vine row at 0-50 cm depth, but was lower in roots growing in the alleyway, and in roots below 50 cm. The proportion of fine roots containing arbuscules (the site of nutrient exchange in arbuscular mycorrhizas) was also greatest for roots growing in the vine row at 0-50 cm depth. Arbuscular colonization of these roots increased prior to budbreak in the spring, reached a high level (50-60% root length) by early summer, and remained high until after the time of leaf senescence in late fall. Arbuscular colonization decreased rapidly by December of 1999 when November rainfall exceeded 200 mm, but did not decline by December of 2000 when November rainfall was below 80 mm. The availability of important plant nutrients in the soil, with the exception of Mg and Zn, was higher in the upper 50 cm of the soil profile where the majority of roots were found. In addition, available nitrate and phosphate were higher in the vine row than in the alleyway soil. Seasonal changes in leaf nutrient concentrations of Pinot Noir confirmed findings in other cultivars, but fluctuations of N, P, and K concentrations in fine roots over the season suggested that fine roots may play a role in nutrient storage, as well as nutrient uptake, in grapevines. Grapevines grown in Oregon direct significant resources to roots and AMF after fruit harvest and substantial post-harvest nutrient uptake may extend into the early winter.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1007/s11104-005-4895-0</doi><tpages>16</tpages></addata></record>
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source SpringerNature Journals; JSTOR Archive Collection A-Z Listing
subjects Agrology
Agronomy. Soil science and plant productions
Alleys
arbuscular mycorrhizas
Biochemistry and biology
Biological and medical sciences
Chemical, physicochemical, biochemical and biological properties
Clay loam
Clays
climate change
Colonization
Color
Cultivars
Economic plant physiology
Forest ecosystems
Fruits
Fundamental and applied biological sciences. Psychology
Fungi
General agronomy. Plant production
grapes
Leaves
mature plants
microbial colonization
Microbiology
mycorrhizal fungi
Nitrate
nutrient availability
Nutrient concentrations
Nutrient uptake
Nutrients
Orchard soils
Phosphate
Physics, chemistry, biochemistry and biology of agricultural and forest soils
Physiology
Plant growth
plant nutrition
Plant roots
Rainfall
root growth
rooting
Roots
Seasonal variations
Senescence
Soil
Soil nutrients
Soil profiles
Soil samples
Soil science
Soil water
soil-plant interactions
Soil-plant relationships. Soil fertility
Soil-plant relationships. Soil fertility. Fertilization. Amendments
Soils
spatial variation
Subsoil
Symbiosis (nodules, symbiotic nitrogen fixation, mycorrhiza...)
temporal variation
Temporal variations
Topsoil
vesicular arbuscular mycorrhizae
Vines
Vineyards
Vitaceae
Vitis vinifera
Zinc
title Spatial and temporal variation of roots, arbuscular mycorrhizal fungi, and plant and soil nutrients in a mature Pinot Noir (Vitis vinifera L.) vineyard in Oregon, USA
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