Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"

This data package contains data that were used for analysis in “Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range”, by Moyes et al. 2013. All data collection and field research were completed on Niwot Ridge,...

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Bibliographic Details
Main Authors: Andrew B. Moyes, Cristina Castanha, Matthew J. Germino, Lara M. Kueppers
Format: Dataset
Language:unknown
Published: ESS-DIVE: Deep Insight for Earth Science Data 2022
Subjects:
Rd
PAR
Online Access:https://search.dataone.org/view/ess-dive-0ab86e13ed12278-20220519T210010647
id dataone:ess-dive-0ab86e13ed12278-20220519T210010647
record_format openpolar
institution Open Polar
collection ESS-DIVE: Deep Insight for Earth Science Data (via DataONE)
op_collection_id dataone:urn:node:ESS_DIVE
language unknown
topic limber pine
treeline
experimental warming
moisture stress
EARTH SCIENCE > BIOSPHERE > ECOLOGICAL DYNAMICS
EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS
EARTH SCIENCE > BIOSPHERE > VEGETATION
EARTH SCIENCE > CLIMATE INDICATORS > CLIMATE FEEDBACKS
Silhouette area
Seedling photos
Seedling scans
LICOR output
Gas exchange
Net assimilation
Anet
Rd
Ci/Ca
Conductance
Transpiration flux rate
Vapor pressure deficit
Photosynthetically active radiation
PAR
Midday water potential
MATLAB code
Meteorology
Air temperature
Relative humidity
Wind speed
Volumetric water content
Soil temperature
Seedling mortality
FvFm
Fluorescence
spellingShingle limber pine
treeline
experimental warming
moisture stress
EARTH SCIENCE > BIOSPHERE > ECOLOGICAL DYNAMICS
EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS
EARTH SCIENCE > BIOSPHERE > VEGETATION
EARTH SCIENCE > CLIMATE INDICATORS > CLIMATE FEEDBACKS
Silhouette area
Seedling photos
Seedling scans
LICOR output
Gas exchange
Net assimilation
Anet
Rd
Ci/Ca
Conductance
Transpiration flux rate
Vapor pressure deficit
Photosynthetically active radiation
PAR
Midday water potential
MATLAB code
Meteorology
Air temperature
Relative humidity
Wind speed
Volumetric water content
Soil temperature
Seedling mortality
FvFm
Fluorescence
Andrew B. Moyes
Cristina Castanha
Matthew J. Germino
Lara M. Kueppers
Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
topic_facet limber pine
treeline
experimental warming
moisture stress
EARTH SCIENCE > BIOSPHERE > ECOLOGICAL DYNAMICS
EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS
EARTH SCIENCE > BIOSPHERE > VEGETATION
EARTH SCIENCE > CLIMATE INDICATORS > CLIMATE FEEDBACKS
Silhouette area
Seedling photos
Seedling scans
LICOR output
Gas exchange
Net assimilation
Anet
Rd
Ci/Ca
Conductance
Transpiration flux rate
Vapor pressure deficit
Photosynthetically active radiation
PAR
Midday water potential
MATLAB code
Meteorology
Air temperature
Relative humidity
Wind speed
Volumetric water content
Soil temperature
Seedling mortality
FvFm
Fluorescence
description This data package contains data that were used for analysis in “Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range”, by Moyes et al. 2013. All data collection and field research were completed on Niwot Ridge, Colorado, USA. This data package contains nine comma-separated-values (.csv) files, one text (.txt) file, and two zipped seedling folders that were used for leaf area analysis. One zipped folder contains 468 .jpg photographs of seedlings, and the second contains 468 corresponding Image J-processed .jpg images that include silhouette leaf area values. .csv and .txt files can be opened using any compatible simple text-editor software such as TextEdit (Mac) and Notepad (Windows); .csv’s can also be opened using R and Microsoft Excel. Image files can be opened using Preview (Mac) and Photos (Windows). In addition, there are a total of 31 Microsoft Excel files: three .xlsx files, and 28 raw Li-Cor output .xls files. This data user’s guide is available in .pdf format, and can be opened using Adobe Acrobat Reader, or any other compatible file viewing software. Geospatial data showing field site locations are also included in the archive for use and reference. There are two geospatial formats in this archive: ESRI shapefiles (.shp) and keyhole markup-language (.kml) files. Both file types contain bounding box information, with the former being polygons, and the latter containing corner coordinates for each site. ESRI shapefiles can be opened using any geospatial software compatible with the file type (such as ESRI’s ArcGIS suite and QGIS), and .kml files are compatible with Google Earth and Google Maps. -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- Continued changes in climate are projected to alter the geographic distributions of plant species, in part by affecting where individuals can establish from seed. We tested the hypothesis that warming promotes uphill redistribution of subalpine tree populations by reducing cold limitation at high elevation and enhancing drought stress at low elevation. We seeded limber pine (Pinus flexilis) into plots with combinations of infrared heating and water addition treatments, at sites positioned in lower subalpine forest, the treeline ecotone, and alpine tundra. In 2010, first-year seedlings were assessed for physiological performance and survival over the snow-free growing season. Seedlings emerged in midsummer, about 5–8 weeks after snowmelt. Low temperature was not observed to limit seedling photosynthesis or respiration between emergence and October, and thus experimental warming did not appear to reduce cold limitation at high elevation. Instead, gas exchange and water potential from all sites indicated a prevailing effect of summer moisture stress on photosynthesis and carbon balance. Infrared heaters raised soil growing degree days (base 5 °C, p < 0.001) and August–September mean soil temperature (p < 0.001). Despite marked differences in vegetation cover and meteorological conditions across sites, volumetric soil moisture content (θ) at 5–10 cm below 0.16 and 0.08 m^3 m^(−3) consistently corresponded with moderate and severe indications of drought stress in midday stem water potential, stomatal conductance, photosynthesis, and respiration. Seedling survival was greater in watered plots than in heated plots (p = 0.01), and negatively related to soil growing degree days and duration of exposure to θ < 0.08 m^3 m^(−3) in a stepwise linear regression model (p < 0.0001). We concluded that seasonal moisture stress and high soil surface temperature imposed a strong limitation to limber pine seedling establishment across a broad elevation gradient, including at treeline, and that these limitations are likely to be enhanced by further climate warming.
format Dataset
author Andrew B. Moyes
Cristina Castanha
Matthew J. Germino
Lara M. Kueppers
author_facet Andrew B. Moyes
Cristina Castanha
Matthew J. Germino
Lara M. Kueppers
author_sort Andrew B. Moyes
title Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
title_short Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
title_full Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
title_fullStr Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
title_full_unstemmed Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
title_sort data from: "warming and the dependence of limber pine (pinus flexilis) establishment on summer soil moisture within and above its current elevation range"
publisher ESS-DIVE: Deep Insight for Earth Science Data
publishDate 2022
url https://search.dataone.org/view/ess-dive-0ab86e13ed12278-20220519T210010647
op_coverage Research was conducted within the Alpine Treeline Warming Experiment (ATWE), on Niwot Ridge in the Front Range of the Colorado Rocky Mountains, USA. The lower subalpine site (LSA; 3060 m) is a previously logged forest that has since naturally-regenerated. The site is composed mostly of mature Engelmann spruce (Picea engelmannii) and lodgepole pine (Pinus contorta), with subalpine fir (Abies lasiocarpa) and limber pine (Pinus flexilis) also present. The site has a southeastern aspect, and is located on the lower-elevation edge of the subalpine forest.
The upper subalpine site (USA; 3430 m) is located on the upper-elevation edge of the subalpine forest, and is an open meadow surrounded by krummholz mats and flag trees. The site has a south-southwestern aspect, and has the highest snowpack due to snow being blown in and trapped from upwind.
The alpine site (ALP; 3540 m) is on Niwot Ridge and is located on a shallow southeastern slope approximately 400 m above timberline. The site is dominated by sedges, forbs, and grasses, and is characterized as an alpine meadow.
ENVELOPE(-105.54854,-105.54743,40.03723,40.03668)
BEGINDATE: 2009-01-01T00:00:00Z ENDDATE: 2010-01-01T00:00:00Z
long_lat ENVELOPE(96.417,96.417,-66.583,-66.583)
ENVELOPE(-67.338,-67.338,-68.785,-68.785)
ENVELOPE(27.987,27.987,65.920,65.920)
ENVELOPE(-105.54854,-105.54743,40.03723,40.03668)
geographic Moyes
Keyhole
Anet
geographic_facet Moyes
Keyhole
Anet
genre Tundra
genre_facet Tundra
_version_ 1782011811970678784
spelling dataone:ess-dive-0ab86e13ed12278-20220519T210010647 2023-11-08T14:15:00+01:00 Data from: "Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range" Andrew B. Moyes Cristina Castanha Matthew J. Germino Lara M. Kueppers Research was conducted within the Alpine Treeline Warming Experiment (ATWE), on Niwot Ridge in the Front Range of the Colorado Rocky Mountains, USA. The lower subalpine site (LSA; 3060 m) is a previously logged forest that has since naturally-regenerated. The site is composed mostly of mature Engelmann spruce (Picea engelmannii) and lodgepole pine (Pinus contorta), with subalpine fir (Abies lasiocarpa) and limber pine (Pinus flexilis) also present. The site has a southeastern aspect, and is located on the lower-elevation edge of the subalpine forest. The upper subalpine site (USA; 3430 m) is located on the upper-elevation edge of the subalpine forest, and is an open meadow surrounded by krummholz mats and flag trees. The site has a south-southwestern aspect, and has the highest snowpack due to snow being blown in and trapped from upwind. The alpine site (ALP; 3540 m) is on Niwot Ridge and is located on a shallow southeastern slope approximately 400 m above timberline. The site is dominated by sedges, forbs, and grasses, and is characterized as an alpine meadow. ENVELOPE(-105.54854,-105.54743,40.03723,40.03668) BEGINDATE: 2009-01-01T00:00:00Z ENDDATE: 2010-01-01T00:00:00Z 2022-01-01T00:00:00Z https://search.dataone.org/view/ess-dive-0ab86e13ed12278-20220519T210010647 unknown ESS-DIVE: Deep Insight for Earth Science Data limber pine treeline experimental warming moisture stress EARTH SCIENCE > BIOSPHERE > ECOLOGICAL DYNAMICS EARTH SCIENCE > BIOSPHERE > ECOSYSTEMS EARTH SCIENCE > BIOSPHERE > VEGETATION EARTH SCIENCE > CLIMATE INDICATORS > CLIMATE FEEDBACKS Silhouette area Seedling photos Seedling scans LICOR output Gas exchange Net assimilation Anet Rd Ci/Ca Conductance Transpiration flux rate Vapor pressure deficit Photosynthetically active radiation PAR Midday water potential MATLAB code Meteorology Air temperature Relative humidity Wind speed Volumetric water content Soil temperature Seedling mortality FvFm Fluorescence Dataset 2022 dataone:urn:node:ESS_DIVE 2023-11-08T13:47:45Z This data package contains data that were used for analysis in “Warming and the dependence of limber pine (Pinus flexilis) establishment on summer soil moisture within and above its current elevation range”, by Moyes et al. 2013. All data collection and field research were completed on Niwot Ridge, Colorado, USA. This data package contains nine comma-separated-values (.csv) files, one text (.txt) file, and two zipped seedling folders that were used for leaf area analysis. One zipped folder contains 468 .jpg photographs of seedlings, and the second contains 468 corresponding Image J-processed .jpg images that include silhouette leaf area values. .csv and .txt files can be opened using any compatible simple text-editor software such as TextEdit (Mac) and Notepad (Windows); .csv’s can also be opened using R and Microsoft Excel. Image files can be opened using Preview (Mac) and Photos (Windows). In addition, there are a total of 31 Microsoft Excel files: three .xlsx files, and 28 raw Li-Cor output .xls files. This data user’s guide is available in .pdf format, and can be opened using Adobe Acrobat Reader, or any other compatible file viewing software. Geospatial data showing field site locations are also included in the archive for use and reference. There are two geospatial formats in this archive: ESRI shapefiles (.shp) and keyhole markup-language (.kml) files. Both file types contain bounding box information, with the former being polygons, and the latter containing corner coordinates for each site. ESRI shapefiles can be opened using any geospatial software compatible with the file type (such as ESRI’s ArcGIS suite and QGIS), and .kml files are compatible with Google Earth and Google Maps. -------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- Continued changes in climate are projected to alter the geographic distributions of plant species, in part by affecting where individuals can establish from seed. We tested the hypothesis that warming promotes uphill redistribution of subalpine tree populations by reducing cold limitation at high elevation and enhancing drought stress at low elevation. We seeded limber pine (Pinus flexilis) into plots with combinations of infrared heating and water addition treatments, at sites positioned in lower subalpine forest, the treeline ecotone, and alpine tundra. In 2010, first-year seedlings were assessed for physiological performance and survival over the snow-free growing season. Seedlings emerged in midsummer, about 5–8 weeks after snowmelt. Low temperature was not observed to limit seedling photosynthesis or respiration between emergence and October, and thus experimental warming did not appear to reduce cold limitation at high elevation. Instead, gas exchange and water potential from all sites indicated a prevailing effect of summer moisture stress on photosynthesis and carbon balance. Infrared heaters raised soil growing degree days (base 5 °C, p < 0.001) and August–September mean soil temperature (p < 0.001). Despite marked differences in vegetation cover and meteorological conditions across sites, volumetric soil moisture content (θ) at 5–10 cm below 0.16 and 0.08 m^3 m^(−3) consistently corresponded with moderate and severe indications of drought stress in midday stem water potential, stomatal conductance, photosynthesis, and respiration. Seedling survival was greater in watered plots than in heated plots (p = 0.01), and negatively related to soil growing degree days and duration of exposure to θ < 0.08 m^3 m^(−3) in a stepwise linear regression model (p < 0.0001). We concluded that seasonal moisture stress and high soil surface temperature imposed a strong limitation to limber pine seedling establishment across a broad elevation gradient, including at treeline, and that these limitations are likely to be enhanced by further climate warming. Dataset Tundra ESS-DIVE: Deep Insight for Earth Science Data (via DataONE) Moyes ENVELOPE(96.417,96.417,-66.583,-66.583) Keyhole ENVELOPE(-67.338,-67.338,-68.785,-68.785) Anet ENVELOPE(27.987,27.987,65.920,65.920) ENVELOPE(-105.54854,-105.54743,40.03723,40.03668)