cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050315.50.3
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-03-15. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050315.50.4
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-03-15. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050315.50.5
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-03-15. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.40.1
title: (:unkn)
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.40.2
title: (:unkn)
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.50.1
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-04-16. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.50.2
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-04-16. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.50.3
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-04-16. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.50.4
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-04-16. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050416.50.5
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-04-16. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.6085/aa/smgxxx_015mtbd014r00_20050524.50.1
title: PISCO: Physical Oceanography: moored temperature data: Santa Cruz Island, California, USA (SMG)

description: This metadata record describes moored seawater temperature data collected at Santa Cruz Island, California, USA, by PISCO. Measurements were collected using StowAway Tidbit Temperature Loggers (Onset Computer Corp. TBIC32+4+27) beginning 2005-05-24. The instrument depth was 014 meters, in an overall water depth of 015 meters (both relative to Mean Sea Level, MSL). The sampling interval was 2.0 minutes.
DOI: 10.5063/aa/myrashulman.6.11
title: Coral reefs of San Blas, Caribbean Panama: 1983-1990

description: Between 1983-1990 large changes in abundances of corals and macroalgae occurred on shallow (1-5 m) lagoonal reefs in the San Blas Islands of Panama. In 1983 these reefs were dominated by the vertical plate forms of the coral genera Agaricia and Millepora. By 1990 we observed the following major changes: (1) loss of approximately one-half of the initial live coral cover, primarily during 1983-1986, and almost completely due to a declinein the abundance of Agaricia. Corals only occupied 12-26% of the reef area by 1990. (2) Macroalgae (mostly Dictyota and HaIimeda) increased from ~ 2% cover in 1983 to 28% cover in 1990. (3) Microatgal cover increased two to ten-fold between 1983 and 1986, then declined to 50% greater than the initial values by 1990. There are at least three contributors to these changes in the benthic community: (1) a coral bleaching event in 1983, which disproportionately affected Agaricia; (2) the mass mortality of Diaderna antillarum in 1983, which led to decreases in grazing pressure on algae; and (3) possible increases in sediment and nutrient loads due to runoff from deforested mountainsides. Temporal patterns and observations of interactions suggest that the decrease in Diadema herbivory is a major factor in this shift in coral and algal populations. Publication: Shulman, M.J. & D. R. Robertson, 1996. Changes in the coral reefs of San Blas, Caribbean Panama: 1983-1990. Coral Reefs 15: 231-236. Dataset includes: percent cover of corals, microalgae, and bare space; macroalgae (by genera) abundance; counts of sea urchins.
DOI: 10.5063/aa/myrashulman.6.3
title: Coral reefs of San Blas, Caribbean Panama: 1983-1990

description: Between 1983-1990 large changes in abundances of corals and macroalgae occurred on shallow (1-5 m) lagoonal reefs in the San Blas Islands of Panama. In 1983 these reefs were dominated by the vertical plate forms of the coral genera Agaricia and Millepora. By 1990 we observed the following major changes: (1) loss of approximately one-half of the initial live coral cover, primarily during 1983-1986, and almost completely due to a declinein the abundance of Agaricia. Corals only occupied 12-26% of the reef area by 1990. (2) Macroalgae (mostly Dictyota and HaIimeda) increased from ~ 2% cover in 1983 to 28% cover in 1990. (3) Microatgal cover increased two to ten-fold between 1983 and 1986, then declined to 50% greater than the initial values by 1990. There are at least three contributors to these changes in the benthic community: (1) a coral bleaching event in 1983, which disproportionately affected Agaricia; (2) the mass mortality of Diaderna antillarum in 1983, which led to decreases in grazing pressure on algae; and (3) possible increases in sediment and nutrient loads due to runoff from deforested mountainsides. Temporal patterns and observations of interactions suggest that the decrease in Diadema herbivory is a major factor in this shift in coral and algal populations. Publication: Shulman, M.J. & D. R. Robertson, 1996. Changes in the coral reefs of San Blas, Caribbean Panama: 1983-1990. Coral Reefs 15: 231-236. Dataset includes: percent cover of corals, microalgae, and bare space; macroalgae (by genera) abundance; counts of sea urchins.
DOI: 10.5063/aa/myrashulman.6.6
title: Coral reefs of San Blas, Caribbean Panama: 1983-1990

description: Between 1983-1990 large changes in abundances of corals and macroalgae occurred on shallow (1-5 m) lagoonal reefs in the San Blas Islands of Panama. In 1983 these reefs were dominated by the vertical plate forms of the coral genera Agaricia and Millepora. By 1990 we observed the following major changes: (1) loss of approximately one-half of the initial live coral cover, primarily during 1983-1986, and almost completely due to a declinein the abundance of Agaricia. Corals only occupied 12-26% of the reef area by 1990. (2) Macroalgae (mostly Dictyota and HaIimeda) increased from ~ 2% cover in 1983 to 28% cover in 1990. (3) Microatgal cover increased two to ten-fold between 1983 and 1986, then declined to 50% greater than the initial values by 1990. There are at least three contributors to these changes in the benthic community: (1) a coral bleaching event in 1983, which disproportionately affected Agaricia; (2) the mass mortality of Diaderna antillarum in 1983, which led to decreases in grazing pressure on algae; and (3) possible increases in sediment and nutrient loads due to runoff from deforested mountainsides. Temporal patterns and observations of interactions suggest that the decrease in Diadema herbivory is a major factor in this shift in coral and algal populations. Publication: Shulman, M.J. & D. R. Robertson, 1996. Changes in the coral reefs of San Blas, Caribbean Panama: 1983-1990. Coral Reefs 15: 231-236. Dataset includes: percent cover of corals, microalgae, and bare space; macroalgae (by genera) abundance; counts of sea urchins.
DOI: 10.5063/aa/myrashulman.6.7
title: Coral reefs of San Blas, Caribbean Panama: 1983-1990

description: Between 1983-1990 large changes in abundances of corals and macroalgae occurred on shallow (1-5 m) lagoonal reefs in the San Blas Islands of Panama. In 1983 these reefs were dominated by the vertical plate forms of the coral genera Agaricia and Millepora. By 1990 we observed the following major changes: (1) loss of approximately one-half of the initial live coral cover, primarily during 1983-1986, and almost completely due to a declinein the abundance of Agaricia. Corals only occupied 12-26% of the reef area by 1990. (2) Macroalgae (mostly Dictyota and HaIimeda) increased from ~ 2% cover in 1983 to 28% cover in 1990. (3) Microatgal cover increased two to ten-fold between 1983 and 1986, then declined to 50% greater than the initial values by 1990. There are at least three contributors to these changes in the benthic community: (1) a coral bleaching event in 1983, which disproportionately affected Agaricia; (2) the mass mortality of Diaderna antillarum in 1983, which led to decreases in grazing pressure on algae; and (3) possible increases in sediment and nutrient loads due to runoff from deforested mountainsides. Temporal patterns and observations of interactions suggest that the decrease in Diadema herbivory is a major factor in this shift in coral and algal populations. Publication: Shulman, M.J. & D. R. Robertson, 1996. Changes in the coral reefs of San Blas, Caribbean Panama: 1983-1990. Coral Reefs 15: 231-236. Dataset includes: percent cover of corals, microalgae, and bare space; macroalgae (by genera) abundance; counts of sea urchins.
DOI: 10.5063/aa/myrashulman.6.9
title: Coral reefs of San Blas, Caribbean Panama: 1983-1990

description: Between 1983-1990 large changes in abundances of corals and macroalgae occurred on shallow (1-5 m) lagoonal reefs in the San Blas Islands of Panama. In 1983 these reefs were dominated by the vertical plate forms of the coral genera Agaricia and Millepora. By 1990 we observed the following major changes: (1) loss of approximately one-half of the initial live coral cover, primarily during 1983-1986, and almost completely due to a declinein the abundance of Agaricia. Corals only occupied 12-26% of the reef area by 1990. (2) Macroalgae (mostly Dictyota and HaIimeda) increased from ~ 2% cover in 1983 to 28% cover in 1990. (3) Microatgal cover increased two to ten-fold between 1983 and 1986, then declined to 50% greater than the initial values by 1990. There are at least three contributors to these changes in the benthic community: (1) a coral bleaching event in 1983, which disproportionately affected Agaricia; (2) the mass mortality of Diaderna antillarum in 1983, which led to decreases in grazing pressure on algae; and (3) possible increases in sediment and nutrient loads due to runoff from deforested mountainsides. Temporal patterns and observations of interactions suggest that the decrease in Diadema herbivory is a major factor in this shift in coral and algal populations. Publication: Shulman, M.J. & D. R. Robertson, 1996. Changes in the coral reefs of San Blas, Caribbean Panama: 1983-1990. Coral Reefs 15: 231-236. Dataset includes: percent cover of corals, microalgae, and bare space; macroalgae (by genera) abundance; counts of sea urchins.
DOI: 10.5063/aa/myrashulman.8.1
title: (:unkn)
DOI: 10.5063/aa/nceas.100.1
title: Biomass and growth of 20-year-old stands of Scots pine

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow.
DOI: 10.5063/aa/nceas.100.2
title: Biomass and growth of 20-year-old stands of Scots pine

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow.
DOI: 10.5063/aa/nceas.100.3
title: Biomass and growth of 20-year-old stands of Scots pine

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow.
DOI: 10.5063/aa/nceas.100.4
title: Biomass and growth of 20-year-old stands of Scots pine

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow. The study site was planted with 4-yr old seedlings in 1963 after clear-felling. The fertilisation experiment, consisting of four treatments with four replicates each (100 m x 50 m plots), commenced in 1987. Treatments comprised irrigation with sprinklers, solid fertilisation, irrigation with liquid fertiliser, and a control. The annual dose of nitrogen was initially 100 kg N per ha, the other nutrients (P, K, Ca, S, Mg) being supplied in fixed proportion to N, adjusted annually against needle samples, in an attempt to attain the optimal nutrient dose. The N dose was reduced 25 percent in 1990. Complete inventories were carried out in 1986, 1991 and 1996, determining height and diameter at breast height for every tree. In the intervening years, about 100 trees per treatment were sub-sampled. After three years' treatment, height and diameter growth in both fertilised stands was double that of the control stand. After 10 years, volume growth of fertilised stands was almost four times that of the control. There was no effect of irrigation on growth. Data from this site were used to parameterise and test the BIOMASS process-based model: parameter values are available from the references below. Total net primary production of a 36-year old untreated stand in 1995 was estimated at 291 g/m2/year (above-ground = 198; below-ground = 93 g/m2/year), and increased more than three times in the irrigated and fertilised treatment to 902 g/m2/year, with more carbon allocated to shoot than root growth (above-ground = 678; below-ground = 224 g/m2/year).
DOI: 10.5063/aa/nceas.100.5
title: Biomass and growth of 20-year-old stands of Scots pine

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow. The study site was planted with 4-yr old seedlings in 1963 after clear-felling. The fertilisation experiment, consisting of four treatments with four replicates each (100 m x 50 m plots), commenced in 1987. Treatments comprised irrigation with sprinklers, solid fertilisation, irrigation with liquid fertiliser, and a control. The annual dose of nitrogen was initially 100 kg N per ha, the other nutrients (P, K, Ca, S, Mg) being supplied in fixed proportion to N, adjusted annually against needle samples, in an attempt to attain the optimal nutrient dose. The N dose was reduced 25 percent in 1990. Complete inventories were carried out in 1986, 1991 and 1996, determining height and diameter at breast height for every tree. In the intervening years, about 100 trees per treatment were sub-sampled. After three years' treatment, height and diameter growth in both fertilised stands was double that of the control stand. After 10 years, volume growth of fertilised stands was almost four times that of the control. There was no effect of irrigation on growth. Data from this site were used to parameterise and test the BIOMASS process-based model: parameter values are available from the references below. Total net primary production of a 36-year old untreated stand in 1995 was estimated at 291 g/m2/year (above-ground = 198; below-ground = 93 g/m2/year), and increased more than three times in the irrigated and fertilised treatment to 902 g/m2/year, with more carbon allocated to shoot than root growth (above-ground = 678; below-ground = 224 g/m2/year).
DOI: 10.5063/aa/nceas.100.6
title: Biomass and growth of 20-year-old stands of Scots pine datasets

description: Productivity of a boreal coniferous forest was determined at the Flakaliden experimental site for a yield optimisation study, beginning in 1986. The principal aim was to determine the potential yield of a young stand of Norway spruce Picea abies, under given climatic conditions, non-limiting soil water and optimal nutritional status without leaching to groundwater. The 8.25 ha Flakaliden study site (64.12 N 19.45 E) is situated in northern Sweden, about 60 km west of the city of Umeaa. The site has a harsh boreal climate with short cool summers of long days, and long, cold winters of short days. Monthly mean air temperature ranges from -8.7 C in February to 14.4 C in July. More than one-third of precipitation falls as snow. The study site was planted with 4-yr old seedlings in 1963 after clear-felling. The fertilisation experiment, consisting of four treatments with four replicates each (100 m x 50 m plots), commenced in 1987. Treatments comprised irrigation with sprinklers, solid fertilisation, irrigation with liquid fertiliser, and a control. The annual dose of nitrogen was initially 100 kg N per ha, the other nutrients (P, K, Ca, S, Mg) being supplied in fixed proportion to N, adjusted annually against needle samples, in an attempt to attain the optimal nutrient dose. The N dose was reduced 25 percent in 1990. Complete inventories were carried out in 1986, 1991 and 1996, determining height and diameter at breast height for every tree. In the intervening years, about 100 trees per treatment were sub-sampled. After three years' treatment, height and diameter growth in both fertilised stands was double that of the control stand. After 10 years, volume growth of fertilised stands was almost four times that of the control. There was no effect of irrigation on growth. Data from this site were used to parameterise and test the BIOMASS process-based model: parameter values are available from the references below. Total net primary production of a 36-year old untreated stand in 1995 was estimated at 291 g/m2/year (above-ground = 198; below-ground = 93 g/m2/year), and increased more than three times in the irrigated and fertilised treatment to 902 g/m2/year, with more carbon allocated to shoot than root growth (above-ground = 678; below-ground = 224 g/m2/year).