Intra-specific Dominance Determines Subseasonal Pinus ponderosa Growth Response to Warm-Season Precipitation amid Drought in southern Nevada, U.S.A.

preprint OA: closed
Full text JSON View at publisher
AI-generated summary by claude@2026-07, 2026-07-15

Dominant ponderosa pines reflected deeper soil moisture fluctuations, while codominant trees responded to shallow precipitation pulses and formed false rings during drought in southern Nevada.

One-sentence paraphrase of the abstract; not a substitute for reading it. No clinical advice. How this works

AI-generated deep summary by claude@2026-07, 2026-07-15 · read from full text

The paper investigates how within-species dominance affects warm-season growth responses of drought-stressed Pinus ponderosa in southern Nevada by measuring stable oxygen isotopes in precipitation, xylem water, and tree-ring cellulose, alongside wood anatomy metrics used to date wood formation. Using dominant and codominant trees over the 2015 and 2016 warm seasons, and leveraging false rings formed after a remnant Hurricane Dolores storm, the authors found different δ18O signals in cellulose between codominant and dominant trees that correspond to soil-moisture access at different depths, while no subseasonal differences were detected in δ13C cellulose. A limitation is that the study is a preprint and focuses on specific warm-season drought years and one storm event to interpret subseasonal water sources. This paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.

Read from the paper's body, not the abstract. Not a substitute for reading the paper. No clinical advice. How this works

Abstract

The isotopic composition of soil water used by trees is affected by multiple ecohydrological processes, and the relative abundance of stable isotopes in plant tissue is determined by subseasonal hydroclimatic conditions. We measured δ 18 O in precipitation (δ 18 O PPT ), xylem water (δ 18 O XW ), and cellulose of tree-rings (δ­ 18 O CELL and δ­ 13 C CELL ) in dominant and codominant ponderosa pines for the 2015 and 2016 warm seasons during drought conditions. Quantitative wood anatomy, including tracheid lumen diameter (LD) and cell wall thickness (CWT), provided phenological dates of wood formation. False ring formation was measured in multiple trees in response to precipitation from a large remnant storm of Hurricane Dolores that reached southern Nevada . We utilized the opportunity to test if the α-cellulose in false rings had a different isotopic signal between dominant and codominant trees. Indeed, we measured a different isotopic ratio (δ­ 18 O CELL ) in codominant trees associated with higher soil moisture at shallower soil depths. Contrariwise, the δ­ 18 O CELL in dominant trees formed during the 2016 warm season reflected fluctuations in soil moisture at deeper soil depths, accessing water stored in the macropores of bedrock after a wetter early warm-season and drier monsoon season. No subseasonal differences between codominant and dominant trees were measured in δ­ 13 C CELL . Throughout our study, we observed that codominant ponderosa pine tree-ring growth responded to pulses of warm-season precipitation more readily than dominant trees. If southern Nevada continues to trend toward a drier and warmer future, deep soil water recharge will be less reliable and drought stress will threaten dominant trees in old-growth forests.
Full text 7,442 characters · extracted from preprint-html · click to expand
Intra-specific Dominance Determines Subseasonal Pinus ponderosa Growth Response to Warm-Season Precipitation amid Drought in southern Nevada, U.S.A. | Authorea try { document.documentElement.classList.add('js'); } catch (e) { } var _gaq = _gaq || []; _gaq.push(['_setAccount', 'G-8VDV14Y67G']); _gaq.push(['_trackPageview']); (function() { var ga = document.createElement('script'); ga.type = 'text/javascript'; ga.async = true; ga.src = ('https:' == document.location.protocol ? 'https://ssl' : 'http://www') + '.google-analytics.com/ga.js'; var s = document.getElementsByTagName('script')[0]; s.parentNode.insertBefore(ga, s); })(); Skip to main content Preprints Collections Wiley Open Research IET Open Research Ecological Society of Japan All Collections About About Authorea FAQs Contact Us Quick Search anywhere Search for preprint articles, keywords, etc. Search Search ADVANCED SEARCH SCROLL Ecohydrology This is a preprint and has not been peer reviewed. Data may be preliminary. 9 January 2025 V1 Latest version Share on Intra-specific Dominance Determines Subseasonal Pinus ponderosa Growth Response to Warm-Season Precipitation amid Drought in southern Nevada, U.S.A. Authors : Charles Truettner 0000-0002-8247-6154 [email protected] , Simon R. Poulson , Emanuele Ziaco , and Adam Z. Csank 0000-0002-7001-4470 Authors Info & Affiliations https://doi.org/10.22541/au.173639045.50102795/v1 257 views 158 downloads Contents Abstract Supplementary Material Information & Authors Metrics & Citations View Options References Figures Tables Media Share Abstract The isotopic composition of soil water used by trees is affected by multiple ecohydrological processes, and the relative abundance of stable isotopes in plant tissue is determined by subseasonal hydroclimatic conditions. We measured δ 18 O in precipitation (δ 18 O PPT ), xylem water (δ 18 O XW ), and cellulose of tree-rings (δ­ 18 O CELL and δ­ 13 C CELL ) in dominant and codominant ponderosa pines for the 2015 and 2016 warm seasons during drought conditions. Quantitative wood anatomy, including tracheid lumen diameter (LD) and cell wall thickness (CWT), provided phenological dates of wood formation. False ring formation was measured in multiple trees in response to precipitation from a large remnant storm of Hurricane Dolores that reached southern Nevada . We utilized the opportunity to test if the α-cellulose in false rings had a different isotopic signal between dominant and codominant trees. Indeed, we measured a different isotopic ratio (δ­ 18 O CELL ) in codominant trees associated with higher soil moisture at shallower soil depths. Contrariwise, the δ­ 18 O CELL in dominant trees formed during the 2016 warm season reflected fluctuations in soil moisture at deeper soil depths, accessing water stored in the macropores of bedrock after a wetter early warm-season and drier monsoon season. No subseasonal differences between codominant and dominant trees were measured in δ­ 13 C CELL . Throughout our study, we observed that codominant ponderosa pine tree-ring growth responded to pulses of warm-season precipitation more readily than dominant trees. If southern Nevada continues to trend toward a drier and warmer future, deep soil water recharge will be less reliable and drought stress will threaten dominant trees in old-growth forests. Supplementary Material File (subseason_sheep_ecohydrology.docx) Download 77.12 KB Information & Authors Information Version history V1 Version 1 09 January 2025 Copyright This work is licensed under a Non Exclusive No Reuse License. Collection Ecohydrology Keywords ecohydrology high-resolution dendrochronology hurricanes monsoon stable isotopes tree physiology wood anatomy Authors Affiliations Charles Truettner 0000-0002-8247-6154 [email protected] University of Nevada Reno Department of Natural Resources and Environmental Science View all articles by this author Simon R. Poulson University of Nevada Reno View all articles by this author Emanuele Ziaco Johannes Gutenberg Universitat Mainz Geographisches Institut View all articles by this author Adam Z. Csank 0000-0002-7001-4470 University of Nevada Reno View all articles by this author Metrics & Citations Metrics Article Usage 257 views 158 downloads .FvxKWukQNSOunydq8rnd { width: 100px; } Citations Download citation Charles Truettner, Simon R. Poulson, Emanuele Ziaco, et al. Intra-specific Dominance Determines Subseasonal Pinus ponderosa Growth Response to Warm-Season Precipitation amid Drought in southern Nevada, U.S.A.. Authorea . 09 January 2025. DOI: https://doi.org/10.22541/au.173639045.50102795/v1 If you have the appropriate software installed, you can download article citation data to the citation manager of your choice. Simply select your manager software from the list below and click Download. For more information or tips please see 'Downloading to a citation manager' in the Help menu . Format Please select one from the list RIS (ProCite, Reference Manager) EndNote BibTex Medlars RefWorks Direct import Tips for downloading citations document.getElementById('citMgrHelpLink').addEventListener('click', function() { popupHelp(this.href); return false; }); $(".js__slcInclude").on("change", function(e){ if ($(this).val() == 'refworks') $('#direct').prop("checked", false); $('#direct').prop("disabled", ($(this).val() == 'refworks')); }); View Options View options PDF View PDF Figures Tables Media Share Share Share article link Copy Link Copied! Copying failed. Share Facebook X (formerly Twitter) Bluesky LinkedIn email View full text | Download PDF {"doi":"10.22541/au.173639045.50102795/v1","type":"Article"} Now Reading: Share Figures Tables Close figure viewer Back to article Figure title goes here Change zoom level Go to figure location within the article Download figure Toggle share panel Toggle share panel Share Toggle information panel Toggle information panel Go to previous graphic Go to next graphic Go to previous table Go to next table All figures All tables View all material View all material xrefBack.goTo xrefBack.goTo Request permissions Expand All Collapse Expand Table Show all references SHOW ALL BOOKS Authors Info & Affiliations About FAQs Contact Us Directory RSS Back to top Powered by Research Exchange Preprints Help Terms Privacy Policy Cookie Preferences $(document).ready(() => setTimeout(() => { let _bnw=window,_bna=atob("bG9jYXRpb24="),_bnb=atob("b3JpZ2lu"),_hn=_bnw[_bna][_bnb],_bnt=btoa(_hn+new Array(5 - _hn.length % 4).join(" ")); $.get("/resource/lodash?t="+_bnt); },4000)); (function(){function c(){var b=a.contentDocument||a.contentWindow.document;if(b){var d=b.createElement('script');d.innerHTML="window.__CF$cv$params={r:'9ff609fbcebc06eb',t:'MTc3OTM5MjI4MA=='};var a=document.createElement('script');a.src='/cdn-cgi/challenge-platform/scripts/jsd/main.js';document.getElementsByTagName('head')[0].appendChild(a);";b.getElementsByTagName('head')[0].appendChild(d)}}if(document.body){var a=document.createElement('iframe');a.height=1;a.width=1;a.style.position='absolute';a.style.top=0;a.style.left=0;a.style.border='none';a.style.visibility='hidden';document.body.appendChild(a);if('loading'!==document.readyState)c();else if(window.addEventListener)document.addEventListener('DOMContentLoaded',c);else{var e=document.onreadystatechange||function(){};document.onreadystatechange=function(b){e(b);'loading'!==document.readyState&&(document.onreadystatechange=e,c())}}}})();

Text is read by the "Ask this paper" AI Q&A widget below. Extraction quality varies by source — PMC NXML preserves structure cleanly, OA-HTML may include some navigation residue, and OA-PDF can have broken hyphenation. The publisher copy (via DOI) is the canonical version.

My notes (saved in your browser only)

Ask this paper AI returns verbatim quotes from the full text · source: preprint-html

Answers must be backed by verbatim quotes from this paper's full text. Hallucinated quotes are dropped automatically; if no verbatim passage answers the question, we say so. How this works

Citation neighborhood (no data yet)

We don't have any in-corpus citations linked to this paper yet. This is a recent paper (2025) — citers typically take a year or two to land, and the OpenAlex reference graph may still be filling in.

Source provenance

europepmc
last seen: 2026-05-20T01:45:00.602351+00:00