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Analysis of fern spore banks from the soil of three vegetation types in the central region of Mexico
The vertical structure of fern spore banks was studied in a xerophilous shrubland, montane rain forest, and pine-oak forest in Hidalgo, Mexico, using the emergence method. Soil samples were collected in April 1999 at depths of 0-10, 10-20, and 20-30 cm. Viable spores decreased significantly with dep...
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Published in: | American journal of botany 2004-05, Vol.91 (5), p.682-688 |
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description | The vertical structure of fern spore banks was studied in a xerophilous shrubland, montane rain forest, and pine-oak forest in Hidalgo, Mexico, using the emergence method. Soil samples were collected in April 1999 at depths of 0-10, 10-20, and 20-30 cm. Viable spores decreased significantly with depth in all vegetation types, and the highest number of prothallia and sporophytes was found in the uppermost layer. The montane rain forest and the xerophilous shrubland had the largest and the richest banks, respectively. Twenty-three fern taxa were registered in the aboveground vegetation, 12 in the soil banks, and 43.5% were in both. Aboveground and in the soil bank, the xerophilous shrubland, the montane rain forest, and the pine-oak forest had, 17 and 7, 1 and 6, and 7 and 3 taxa, respectively. These were distributed differentially in relation to depth. The Sorensen index indicated a similarity of 61.5% between the xerophilous shrubland and the montane rain forest, and the Czeckanovsky index indicated 19.75%. The presence of viable spores in the soil of all vegetation types confirmed the existence of natural spore banks. Long-distance dispersal was an important factor determining the specific composition of the xerophilous shrubland and the pine-oak forest. |
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Soil samples were collected in April 1999 at depths of 0-10, 10-20, and 20-30 cm. Viable spores decreased significantly with depth in all vegetation types, and the highest number of prothallia and sporophytes was found in the uppermost layer. The montane rain forest and the xerophilous shrubland had the largest and the richest banks, respectively. Twenty-three fern taxa were registered in the aboveground vegetation, 12 in the soil banks, and 43.5% were in both. Aboveground and in the soil bank, the xerophilous shrubland, the montane rain forest, and the pine-oak forest had, 17 and 7, 1 and 6, and 7 and 3 taxa, respectively. These were distributed differentially in relation to depth. The Sorensen index indicated a similarity of 61.5% between the xerophilous shrubland and the montane rain forest, and the Czeckanovsky index indicated 19.75%. The presence of viable spores in the soil of all vegetation types confirmed the existence of natural spore banks. Long-distance dispersal was an important factor determining the specific composition of the xerophilous shrubland and the pine-oak forest.</description><identifier>ISSN: 0002-9122</identifier><identifier>EISSN: 1537-2197</identifier><identifier>DOI: 10.3732/ajb.91.5.682</identifier><identifier>PMID: 21653423</identifier><identifier>CODEN: AJBOAA</identifier><language>eng</language><publisher>United States: Botanical Soc America</publisher><subject>Analysis ; botanical composition ; depth ; Ecology ; Ferns ; ferns and fern allies ; Forest soils ; forests ; geographical variation ; Mexico ; Montane forests ; pine-oak forest ; plant communities ; Plant spores ; Rain forests ; Shrublands ; soil propagule banks ; Soil samples ; soil spore banks ; Soils ; spore dispersal ; Spores ; Taxa ; Trees ; Vegetation ; vegetation types ; xerophytes</subject><ispartof>American journal of botany, 2004-05, Vol.91 (5), p.682-688</ispartof><rights>Copyright 2004 Botanical Society of America, Inc.</rights><rights>2004 Botanical Society of America</rights><rights>Copyright Botanical Society of America, Inc. 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Soil samples were collected in April 1999 at depths of 0-10, 10-20, and 20-30 cm. Viable spores decreased significantly with depth in all vegetation types, and the highest number of prothallia and sporophytes was found in the uppermost layer. The montane rain forest and the xerophilous shrubland had the largest and the richest banks, respectively. Twenty-three fern taxa were registered in the aboveground vegetation, 12 in the soil banks, and 43.5% were in both. Aboveground and in the soil bank, the xerophilous shrubland, the montane rain forest, and the pine-oak forest had, 17 and 7, 1 and 6, and 7 and 3 taxa, respectively. These were distributed differentially in relation to depth. The Sorensen index indicated a similarity of 61.5% between the xerophilous shrubland and the montane rain forest, and the Czeckanovsky index indicated 19.75%. The presence of viable spores in the soil of all vegetation types confirmed the existence of natural spore banks. Long-distance dispersal was an important factor determining the specific composition of the xerophilous shrubland and the pine-oak forest.</description><subject>Analysis</subject><subject>botanical composition</subject><subject>depth</subject><subject>Ecology</subject><subject>Ferns</subject><subject>ferns and fern allies</subject><subject>Forest soils</subject><subject>forests</subject><subject>geographical variation</subject><subject>Mexico</subject><subject>Montane forests</subject><subject>pine-oak forest</subject><subject>plant communities</subject><subject>Plant spores</subject><subject>Rain forests</subject><subject>Shrublands</subject><subject>soil propagule banks</subject><subject>Soil samples</subject><subject>soil spore banks</subject><subject>Soils</subject><subject>spore dispersal</subject><subject>Spores</subject><subject>Taxa</subject><subject>Trees</subject><subject>Vegetation</subject><subject>vegetation types</subject><subject>xerophytes</subject><issn>0002-9122</issn><issn>1537-2197</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNp9kk1v1DAQhi0EokvhxhGBhQRc2MWfcXzcVnyqiAP0bDnxZNdLEi92lnT_PU5TKsShJ8uaZx6P5jVCTylZccXZO7urVpqu5Koo2T20oJKrJaNa3UcLQghbasrYCXqU0i5ftdDsITphtJBcML5Abt3b9ph8wqHBDcQep32IgCvb_0y4iaHDwxZwCr6diGEbAfBv2MBgBx96PBz3kLDvr6ka-iHaFkfYTLXMf4UrX4fH6EFj2wRPbs5TdPnh_Y_zT8uLbx8_n68vlrUkIk9aKiUsAFNV6YQDUkjLRS2rQjjdaMmZqwtXCEqlErlQOc40kEoQJxtHCn6K3szefQy_DpAG0_lUQ9vaHsIhmVJRXpaiZJl8fSdJlaKyLGgGX_4H7sIh5p0lwzJR5iVOtrczVMeQUoTG7KPvbDwaSswUkskhGU2NNMX1489vnIeqA3cL_00lA2wGRt_C8U6ZWX85Y2S2PpubdmkI8bZJUMaVnJyv5vLWb7ajj2BSZ9s2j0DNOI7_DPdi5hobjN1En8zld0Yonz6PItn2B7miuvc</recordid><startdate>200405</startdate><enddate>200405</enddate><creator>Ramirez-Trejo, M. del R</creator><creator>Perez-Garcia, B</creator><creator>Orozco-Segovia, A</creator><general>Botanical Soc America</general><general>Botanical Society of America</general><general>Botanical Society of America, Inc</general><scope>FBQ</scope><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QL</scope><scope>7SN</scope><scope>7SS</scope><scope>7ST</scope><scope>7U9</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>H94</scope><scope>M7N</scope><scope>P64</scope><scope>RC3</scope><scope>SOI</scope><scope>7X8</scope></search><sort><creationdate>200405</creationdate><title>Analysis of fern spore banks from the soil of three vegetation types in the central region of Mexico</title><author>Ramirez-Trejo, M. del R ; Perez-Garcia, B ; Orozco-Segovia, A</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5042-98774aee27b8d4de065a34c5b64d9f9532dc6d641157434cbd329e0b40d5fd063</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2004</creationdate><topic>Analysis</topic><topic>botanical composition</topic><topic>depth</topic><topic>Ecology</topic><topic>Ferns</topic><topic>ferns and fern allies</topic><topic>Forest soils</topic><topic>forests</topic><topic>geographical variation</topic><topic>Mexico</topic><topic>Montane forests</topic><topic>pine-oak forest</topic><topic>plant communities</topic><topic>Plant spores</topic><topic>Rain forests</topic><topic>Shrublands</topic><topic>soil propagule banks</topic><topic>Soil samples</topic><topic>soil spore banks</topic><topic>Soils</topic><topic>spore dispersal</topic><topic>Spores</topic><topic>Taxa</topic><topic>Trees</topic><topic>Vegetation</topic><topic>vegetation types</topic><topic>xerophytes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ramirez-Trejo, M. del R</creatorcontrib><creatorcontrib>Perez-Garcia, B</creatorcontrib><creatorcontrib>Orozco-Segovia, A</creatorcontrib><collection>AGRIS</collection><collection>PubMed</collection><collection>CrossRef</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Ecology Abstracts</collection><collection>Entomology Abstracts (Full archive)</collection><collection>Environment Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><collection>MEDLINE - Academic</collection><jtitle>American journal of botany</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ramirez-Trejo, M. del R</au><au>Perez-Garcia, B</au><au>Orozco-Segovia, A</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Analysis of fern spore banks from the soil of three vegetation types in the central region of Mexico</atitle><jtitle>American journal of botany</jtitle><addtitle>Am J Bot</addtitle><date>2004-05</date><risdate>2004</risdate><volume>91</volume><issue>5</issue><spage>682</spage><epage>688</epage><pages>682-688</pages><issn>0002-9122</issn><eissn>1537-2197</eissn><coden>AJBOAA</coden><abstract>The vertical structure of fern spore banks was studied in a xerophilous shrubland, montane rain forest, and pine-oak forest in Hidalgo, Mexico, using the emergence method. Soil samples were collected in April 1999 at depths of 0-10, 10-20, and 20-30 cm. Viable spores decreased significantly with depth in all vegetation types, and the highest number of prothallia and sporophytes was found in the uppermost layer. The montane rain forest and the xerophilous shrubland had the largest and the richest banks, respectively. Twenty-three fern taxa were registered in the aboveground vegetation, 12 in the soil banks, and 43.5% were in both. Aboveground and in the soil bank, the xerophilous shrubland, the montane rain forest, and the pine-oak forest had, 17 and 7, 1 and 6, and 7 and 3 taxa, respectively. These were distributed differentially in relation to depth. The Sorensen index indicated a similarity of 61.5% between the xerophilous shrubland and the montane rain forest, and the Czeckanovsky index indicated 19.75%. The presence of viable spores in the soil of all vegetation types confirmed the existence of natural spore banks. Long-distance dispersal was an important factor determining the specific composition of the xerophilous shrubland and the pine-oak forest.</abstract><cop>United States</cop><pub>Botanical Soc America</pub><pmid>21653423</pmid><doi>10.3732/ajb.91.5.682</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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subjects | Analysis botanical composition depth Ecology Ferns ferns and fern allies Forest soils forests geographical variation Mexico Montane forests pine-oak forest plant communities Plant spores Rain forests Shrublands soil propagule banks Soil samples soil spore banks Soils spore dispersal Spores Taxa Trees Vegetation vegetation types xerophytes |
title | Analysis of fern spore banks from the soil of three vegetation types in the central region of Mexico |
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