cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20020821.50.2
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2002-08-21. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20020821.50.3
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2002-08-21. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20020821.50.4
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2002-08-21. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20030418.40.1
title: (:unkn)
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20030418.50.1
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-04-18. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20030418.50.2
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-04-18. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20030418.50.3
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-04-18. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20030418.50.4
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-04-18. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20031122.40.1
title: (:unkn)
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20031122.40.2
title: (:unkn)
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20031122.50.1
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-11-22. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20031122.50.5
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2003-11-22. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20040315.40.2
title: (:unkn)
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20040315.50.1
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2004-03-15. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.6085/aa/shlx00_xxxitbdxlsr03_20040315.50.2
title: PISCO: Intertidal: site temperature data: Strawberry Hill, Oregon, USA (SHLX00)

description: This metadata record describes a mix of intertidal seawater and air temperature data collected at Strawberry Hill, Oregon, USA, by PISCO. Measurements were collected using StowAway TidbiT Temperature Loggers (Onset Computer Corp. TBI32-05+37) beginning 2004-03-15. Site temperature loggers are bolted down in a wire cage at three locations within each site near MLLW. Temperature is recorded at 1 hour intervals.
DOI: 10.5063/aa/bowdish.96.2
title: Bythotrephes abundance in Harp Lake

description: This table contains the average abundance of Bythotrephes (#/m3), in each barb class, in Harp Lake. The data are the average of ten randomly selected stations on each date.
DOI: 10.5063/aa/bowdish.97.2
title: Chaoborus abundances in the 8 Dorset lakes on one evening

description: Weighted areal density of chaoborus larvae in the DORSET lakes. Data are # of larvae per m^2, correcting for areas of the two sampling strata.There are three species, and a potential for 4 instars of each, called CI to CIV. The data set is called chaob.cvs.
DOI: 10.5063/aa/bowdish.97.3
title: Chaoborus abundances in the 8 Dorset lakes on one evening

description: Weighted areal density of chaoborus larvae in the DORSET lakes. Data are # of larvae per m^2, correcting for areas of the two sampling strata.There are three species, and a potential for 4 instars of each, called CI to CIV. The data set is called chaob.cvs.
DOI: 10.5063/aa/bowdish.99.1
title: Serengeti Ecosystem

description: The Serengeti ecosystem exemplifies a number of general features of terrestrial food web dynamics and can therefore be viewed as a model system for studying a complex interplay of basic ecological principles. These include: (1) the diverse roles of generalist top predators in governing coexistence in prey communities, (2) the importance of omnivory and intraguild predation in modulating the magnitude of 'top-down' impacts of predators, (3) trophic cascades; (4) the implications of movement, landscape pattern, and spatial heterogeneity for food web dynamics, and, (5) the impact of temporal variation on stability and species composition of local communities. The Serengeti, like many ecosystems, is subject to increasing human use. Understanding human behavior and the links between humans and the ecosystem provides a necessary foundation for conservation.
DOI: 10.5063/aa/bowdish.99.3
title: Serengeti Ecosystem

description: The Serengeti ecosystem exemplifies a number of general features of terrestrial food web dynamics and can therefore be viewed as a model system for studying a complex interplay of basic ecological principles. These include: (1) the diverse roles of generalist top predators in governing coexistence in prey communities, (2) the importance of omnivory and intraguild predation in modulating the magnitude of 'top-down' impacts of predators, (3) trophic cascades; (4) the implications of movement, landscape pattern, and spatial heterogeneity for food web dynamics, and, (5) the impact of temporal variation on stability and species composition of local communities. The Serengeti, like many ecosystems, is subject to increasing human use. Understanding human behavior and the links between humans and the ecosystem provides a necessary foundation for conservation.
DOI: 10.5063/aa/bowdish.99.5
title: Serengeti Ecosystem

description: The Serengeti ecosystem exemplifies a number of general features of terrestrial food web dynamics and can therefore be viewed as a model system for studying a complex interplay of basic ecological principles. These include: (1) the diverse roles of generalist top predators in governing coexistence in prey communities, (2) the importance of omnivory and intraguild predation in modulating the magnitude of 'top-down' impacts of predators, (3) trophic cascades; (4) the implications of movement, landscape pattern, and spatial heterogeneity for food web dynamics, and, (5) the impact of temporal variation on stability and species composition of local communities. The Serengeti, like many ecosystems, is subject to increasing human use. Understanding human behavior and the links between humans and the ecosystem provides a necessary foundation for conservation.
DOI: 10.5063/aa/broitman.3.1
title: rdifs_npp_sample_data_lter_ecoinformatics_workshop

description: Sevilleta National Wildlife Refuge, operated by the U.S. Fish & Wildlife Service, is located in Soccoro County in central New Mexico. The Sevilleta spans approximately 100,000 ha of land and has vegetative influences representative of the Chihuahuan Desert, the Great Plains grassland and the Colorado Plateau. creosote shrubland (C), blue grama grassland (B), black grama grassland (G), and pinon/juniper woodland (P).
DOI: 10.5063/aa/broitman.3.3
title: rdifs_npp_sample_data_lter_ecoinformatics_workshop

description: Sevilleta National Wildlife Refuge, operated by the U.S. Fish & Wildlife Service, is located in Soccoro County in central New Mexico. The Sevilleta spans approximately 100,000 ha of land and has vegetative influences representative of the Chihuahuan Desert, the Great Plains grassland and the Colorado Plateau. creosote shrubland (C), blue grama grassland (B), black grama grassland (G), and pinon/juniper woodland (P).
DOI: 10.5063/aa/brooke.63.1
title: (:unkn)
DOI: 10.5063/aa/brownc.4.1
title: My Microclimate data

description: The purpose of the data were to test the hypothesis that a flagstone substrate in the sun would warm our sensor faster after moving from a cement substrate in the shade than would a grassy substrate in the sun.
DOI: 10.5063/aa/chadden.36.1
title: (:unkn)
DOI: 10.5063/aa/chadden.39.1
title: (:unkn)
DOI: 10.5063/aa/chadden.42.1
title: (:unkn)
DOI: 10.5063/aa/chadden.43.1
title: (:unkn)
DOI: 10.5063/aa/chadden.48.1
title: Scots Pine NPP Dataset (Siberia)- data from 14 boreal forest stands in eastern Russia

description: Data from 14 stands of Scots Pine (Pinus sylvestris) at two locations in Siberia have been compiled by Dr. Olga Krankina of Oregon State University, U.S.A. These plots represent one of the main dominant tree species in Siberian forests, growing in stands of relatively high density and productivity. The data reported previously in Gabeev (1990) were gathered from stands studied under the former U.S.S.R. International Biological Programme in Tomsk Region, Western Siberia (approximately 58 N 83 E; 54-year mean precipitation = 501.2 mm). Above-ground measurements were obtained using standard allometric forestry methods, and below-ground data were originally reported in considerable detail by size class and depth. Data reported previously by Buzykin (1978) are from a study of carbon and nutrient cycling in the forests of the Angara River basin, Irkutsk Region, near Lake Baikal (approximately 53 N 103 E). Here Scots Pine (Pinus sylvestris) is the dominant tree species on about 26 percent of the forested area. The three study sites represent the three most common site conditions found in this area. Trees were measured by standard allometric methods on 0.3-0.4 hectare plots, and understory was determined from 20 x 0.25 hectare plots at each site for three successive years. Data on litterfall are mean values, 1968-1974, and were originally reported separately for needles, bark, branches, cones, and other litter. Below-ground biomass was determined by excavation of entire root systems, and root turnover was estimated for different size classes. Both authors have published extensively in the Russian literature. Components of net primary productivity (NPP) and standing biomass, above- and below-ground, are available for each stand of Pinus sylvestris. The range of above-ground biomass was 5000-32700 g/m2 (25-163 tC/ha, assuming mean carbon content of 50 percent for wood and 45 percent for foliage); below-ground coarse roots ranged between 974 and 6430 g/m2 (5-32 tC/ha at 50 percent carbon content). Above-ground NPP averaged 905 g (438 gC)/m2/year and 765 g (374 gC)/m2/year for the Tomsk and Irkutsk studies, respectively; the corresponding mean figures for total NPP were 1018 g (489 gC)/m2/year and 1695 g (792 gC)/m2/year. Abstract from http://www-eosdis.ornl.gov/NPP/other_files/ssp_des.html.
DOI: 10.5063/aa/chadden.60.1
title: NPP in tropical forests: an evaluation and synthesis of existing field data

description: Information on net primary production in tropical forests is needed for the development of realistic global carbon budgets, for projecting how these ecosystems will be affected by climatic and atmospheric changes, and for evaluating eddy covariance measurements of tropical forest carbon flux. However, a review of the database commonly used to address these issues shows that it has serious flaws. In this paper we synthesize the data in the primary literature on NPP in old-growth tropical forests to produce a consistent data set on NPP for these forests. Studies in this biome have addressed only a few NPP components, all aboveground. Given the limited scope of the direct field measurements, we sought relationships in the existing data that allow estimation of unmeasured aspects of production from those that are more easily assessed. We found a predictive relationship between annual litterfall and aboveground biomass increment. For 39 diverse tropical forest sites, we then developed consistent, documented estimates of the upper and lower bounds around total NPP to serve as benchmarks for calibrating and validating biogeochemical models with respect to this biome. We developed these estimates based on existing field measurements, current understanding of aboveground consumption and biogenic volatile organic carbon emissions, and our judgment that belowground production is bounded by the range 0.21.2 3 ANPP (aboveground NPP). Across this broad spectrum of tropical forests (dry to wet, lowland to montane, nutrient-rich to nutrient-poor soils), our estimates of lower and upper bounds on total NPP range from 1.7 to 11.8 Mg C/ha-yr (lower bounds) and from 3.1 to 21.7 Mg C/ha-yr (upper bounds). We also showed that two relationships that have been used for estimating NPP (the Bray-Gorham relationship based on leaf litterfall and the Miami model based on temperature or precipitation) are not valid for the tropical forest biome.
DOI: 10.5063/aa/chadden.60.3
title: NPP in tropical forests: an evaluation and synthesis of existing field data

description: Information on net primary production in tropical forests is needed for the development of realistic global carbon budgets, for projecting how these ecosystems will be affected by climatic and atmospheric changes, and for evaluating eddy covariance measurements of tropical forest carbon flux. However, a review of the database commonly used to address these issues shows that it has serious flaws. In this paper we synthesize the data in the primary literature on NPP in old-growth tropical forests to produce a consistent data set on NPP for these forests. Studies in this biome have addressed only a few NPP components, all aboveground. Given the limited scope of the direct field measurements, we sought relationships in the existing data that allow estimation of unmeasured aspects of production from those that are more easily assessed. We found a predictive relationship between annual litterfall and aboveground biomass increment. For 39 diverse tropical forest sites, we then developed consistent, documented estimates of the upper and lower bounds around total NPP to serve as benchmarks for calibrating and validating biogeochemical models with respect to this biome. We developed these estimates based on existing field measurements, current understanding of aboveground consumption and biogenic volatile organic carbon emissions, and our judgment that belowground production is bounded by the range 0.21.2 3 ANPP (aboveground NPP). Across this broad spectrum of tropical forests (dry to wet, lowland to montane, nutrient-rich to nutrient-poor soils), our estimates of lower and upper bounds on total NPP range from 1.7 to 11.8 Mg C/ha-yr (lower bounds) and from 3.1 to 21.7 Mg C/ha-yr (upper bounds). We also showed that two relationships that have been used for estimating NPP (the Bray-Gorham relationship based on leaf litterfall and the Miami model based on temperature or precipitation) are not valid for the tropical forest biome.
DOI: 10.5063/aa/chadden.60.4
title: NPP in tropical forests: an evaluation and synthesis of existing field data

description: Information on net primary production in tropical forests is needed for the development of realistic global carbon budgets, for projecting how these ecosystems will be affected by climatic and atmospheric changes, and for evaluating eddy covariance measurements of tropical forest carbon flux. However, a review of the database commonly used to address these issues shows that it has serious flaws. In this paper we synthesize the data in the primary literature on NPP in old-growth tropical forests to produce a consistent data set on NPP for these forests. Studies in this biome have addressed only a few NPP components, all aboveground. Given the limited scope of the direct field measurements, we sought relationships in the existing data that allow estimation of unmeasured aspects of production from those that are more easily assessed. We found a predictive relationship between annual litterfall and aboveground biomass increment. For 39 diverse tropical forest sites, we then developed consistent, documented estimates of the upper and lower bounds around total NPP to serve as benchmarks for calibrating and validating biogeochemical models with respect to this biome. We developed these estimates based on existing field measurements, current understanding of aboveground consumption and biogenic volatile organic carbon emissions, and our judgment that belowground production is bounded by the range 0.21.2 3 ANPP (aboveground NPP). Across this broad spectrum of tropical forests (dry to wet, lowland to montane, nutrient-rich to nutrient-poor soils), our estimates of lower and upper bounds on total NPP range from 1.7 to 11.8 Mg C/ha-yr (lower bounds) and from 3.1 to 21.7 Mg C/ha-yr (upper bounds). We also showed that two relationships that have been used for estimating NPP (the Bray-Gorham relationship based on leaf litterfall and the Miami model based on temperature or precipitation) are not valid for the tropical forest biome.
DOI: 10.5063/aa/chadden.60.6
title: NPP in tropical forests: an evaluation and synthesis of existing field data

description: Information on net primary production in tropical forests is needed for the development of realistic global carbon budgets, for projecting how these ecosystems will be affected by climatic and atmospheric changes, and for evaluating eddy covariance measurements of tropical forest carbon flux. However, a review of the database commonly used to address these issues shows that it has serious flaws. In this paper we synthesize the data in the primary literature on NPP in old-growth tropical forests to produce a consistent data set on NPP for these forests. Studies in this biome have addressed only a few NPP components, all aboveground. Given the limited scope of the direct field measurements, we sought relationships in the existing data that allow estimation of unmeasured aspects of production from those that are more easily assessed. We found a predictive relationship between annual litterfall and aboveground biomass increment. For 39 diverse tropical forest sites, we then developed consistent, documented estimates of the upper and lower bounds around total NPP to serve as benchmarks for calibrating and validating biogeochemical models with respect to this biome. We developed these estimates based on existing field measurements, current understanding of aboveground consumption and biogenic volatile organic carbon emissions, and our judgment that belowground production is bounded by the range 0.2-1.2 x ANPP (aboveground NPP). Across this broad spectrum of tropical forests (dry to wet, lowland to montane, nutrient-rich to nutrient-poor soils), our estimates of lower and upper bounds on total NPP range from 1.7 to 11.8 Mg C/ha-yr (lower bounds) and from 3.1 to 21.7 Mg C/ha-yr (upper bounds). We also showed that two relationships that have been used for estimating NPP (the Bray-Gorham relationship based on leaf litterfall and the Miami model based on temperature or precipitation) are not valid for the tropical forest biome.