<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-09-20T21:30:13Z</responseDate><request verb="GetRecord" identifier="oai:mountainscholar.org:10217/242935" metadataPrefix="dim">https://api.mountainscholar.org/server/oai/request</request><GetRecord><record><header><identifier>oai:mountainscholar.org:10217/242935</identifier><datestamp>2026-06-05T15:35:29Z</datestamp><setSpec>com_10217_100532</setSpec><setSpec>com_10217_100000</setSpec><setSpec>com_10217_100430</setSpec><setSpec>com_10217_100303</setSpec><setSpec>col_10217_100538</setSpec><setSpec>col_10217_100433</setSpec></header><metadata><dim:dim xmlns:dim="http://www.dspace.org/xmlns/dspace/dim" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.dspace.org/xmlns/dspace/dim http://www.dspace.org/schema/dim.xsd">
   <dim:field mdschema="dc" element="contributor" qualifier="author">Brown, Peter Mark, author</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Binkley, Dan, advisor</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Lauenroth, William, committee member</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Romme, William H., committee member</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Smith, Skip, committee member</dim:field>
   <dim:field mdschema="dc" element="contributor" qualifier="author">Sieg, Carolyn Hull, committee member</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="accessioned">2026-01-23T17:30:05Z</dim:field>
   <dim:field mdschema="dc" element="date" qualifier="issued">2003</dim:field>
   <dim:field mdschema="dc" element="identifier">ETDF_2003_Brown_3092655.pdf</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">https://hdl.handle.net/10217/242935</dim:field>
   <dim:field mdschema="dc" element="identifier" qualifier="uri">https://doi.org/10.25675/3.025792</dim:field>
   <dim:field mdschema="dc" element="description" qualifier="abstract">A prevailing model for historical conditions in ponderosa pine forests is that
 frequent surface fires maintained open, low-density forest stands composted primarily of
 old, large trees. However, this model may not apply uniformly to ponderosa pine forests
 in the Black Hills of southwestern South Dakota and northeastern Wyoming. Infrequent,
 extensive stand-replacing fires also may have occurred and apparently resulted in large
 landscapes of dense, even-aged forest. I examined this alternative model for the Black
 Hills using fire-sear and tree-age data. Fire chronologies from over 1000 trees collected
 at over 50 locations span the past four to six centuries. Compared to other ponderosa
 pine forests in the southwest US or southern Rocky Mountains, these communities
 burned less frequently. Surface fire frequency varied from an average of every 10 to 13
 years at lower elevation sites on the ponderosa pine - northern Great Plains prairie
 ecotone to as much as 30 to 33 years at higher elevations. Mid-elevation interior sites at
 Jewel Cave National Monument burned on average every 20 to 26 years. Fires largely
 ceased in all areas shortly after Euro-American settlement began in the 1870s. Pre-settlement
 age structure documents very pulsed patterns of tree establishment, with the
 most abundant cohort occurring from 1770 to 1805. Cohorts established during wet periods in the northern Great Plains. Extended wet conditions likely promoted abundant
 tree regeneration, fast growth, and longer periods between surface fires that would have
 permitted more trees to reach canopy status, therefore becoming more “fireproof’ during
 later surface fires. The absence of fire was likely more critical to structuring the current
 forest than any potential variation in fire behavior. The late 1700s cohort also followed
 an extended drought from1756 to 1761, and tree mortality caused by moisture stress may
 have contributed to stand opening. Patchy crown mortality from fire coupled with other
 disturbances undoubtedly contributed to stand opening before pulses of climatically
 driven seedling establishment. Mortality and regeneration were likely completely
 uncoupled processes and even-aged structure is not definitive evidence of stand-replacing
 fires in ponderosa pine forests. However, abundant fire scars indicate that surface fires
 were ubiquitous across the Black Hills landscape. Thus, the prevailing historical model
 of frequent surface fires promoting and maintaining mostly open forest stands is largely
 supported by the tree-ring evidence, although the Black Hills had a greater range of
 variability in fire behavior than ponderosa pine forests of other regions as documented by
 historic descriptions of the forest at settlement.</dim:field>
   <dim:field mdschema="dc" element="format" qualifier="medium">born digital</dim:field>
   <dim:field mdschema="dc" element="format" qualifier="medium">doctoral dissertations</dim:field>
   <dim:field mdschema="dc" element="language">English</dim:field>
   <dim:field mdschema="dc" element="language" qualifier="iso">eng</dim:field>
   <dim:field mdschema="dc" element="publisher">Colorado State University. Libraries</dim:field>
   <dim:field mdschema="dc" element="relation" qualifier="ispartof">2000-2019</dim:field>
   <dim:field mdschema="dc" element="rights">Copyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.</dim:field>
   <dim:field mdschema="dc" element="rights" qualifier="license">Per the terms of a contractual agreement, all use of this item is limited to the non-commercial use of Colorado State University and its authorized users.</dim:field>
   <dim:field mdschema="dc" element="subject">ecology</dim:field>
   <dim:field mdschema="dc" element="subject">forestry</dim:field>
   <dim:field mdschema="dc" element="title">Fire, climate, and forest structure in ponderosa pine forests of the Black Hills</dim:field>
   <dim:field mdschema="dc" element="type">Text</dim:field>
   <dim:field mdschema="thesis" element="degree" qualifier="name">Doctor of Philosophy (Ph.D.)</dim:field>
   <dim:field mdschema="thesis" element="degree" qualifier="level">Doctoral</dim:field>
   <dim:field mdschema="thesis" element="degree" qualifier="discipline">Forest, Rangeland, and Watershed Stewardship</dim:field>
   <dim:field mdschema="thesis" element="degree" qualifier="grantor">Colorado State University</dim:field>
   <dim:field mdschema="dcterms" element="rights" qualifier="dpla">This Item is protected by copyright and/or related rights (https://rightsstatements.org/vocab/InC/1.0/). You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).</dim:field>
   <dim:field mdschema="others" element="access-status">open.access</dim:field>
</dim:dim>
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