cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.3535/g8k-b4d-evz
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/ja8-7z2-yk8
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.5281/zenodo.18741714
title: Datset fot "Dissociative ionization cross sections and rate coefficients of H2S, OCS, LiH, and SiC"

description: The dataset contains the partial and total ionization cross sections, rate coefficients, and their fitting parameters. The cross sections are in 1E-16 cm^2, and the incident energy in electron Volts. The rates are in cm^3/s
DOI: 10.3535/cdq-7hz-7aa
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/ghc-1dw-020
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/4tg-7qx-g8h
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/cm7-eb5-rvq
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/g3q-23y-lcf
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/lc9-2ga-z3v
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/gey-btr-tbp
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/gze-378-744
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/z7w-s90-phc
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/0r1-4tz-wz8
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/65f-9b3-cdd
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.3535/kfq-jdk-dgm
title: Receptaculites sp.

description: Digital Specimen for the physical specimen hosted at Tallinn University of Technology.
DOI: 10.5281/zenodo.18752494
title: CORRECTIONALACTIVITIESFORPRESCHOOLCHILDRENWITHSPEECHDISORDERS

description: Thisarticlediscussesthecontent,directionsandpedagogicalsignificanceofcorrectiveworkwithpreschoolchildrenwithspeechdisorders.Theroleofspeechtherapyandcorrectional-pedagogicalapproachesineliminatingspeechdisordersisanalyzedbasedonscientificliterature.
DOI: 10.5281/zenodo.18752493
title: CORRECTIONALACTIVITIESFORPRESCHOOLCHILDRENWITHSPEECHDISORDERS

description: Thisarticlediscussesthecontent,directionsandpedagogicalsignificanceofcorrectiveworkwithpreschoolchildrenwithspeechdisorders.Theroleofspeechtherapyandcorrectional-pedagogicalapproachesineliminatingspeechdisordersisanalyzedbasedonscientificliterature.
DOI: 10.15468/dl.ezxqbt
title: Occurrence Download

description: A dataset containing 1202 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Galbula galbula",
 "Year is greater than or equal to 2000",
 "Year is less than or equal to 2026",
 "Country is Colombia",
 "HasCoordinate is true"
 ]
}

 The dataset includes 1202 records from 16 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0005548-260221153910048/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.7tjyqq
title: Occurrence Download

description: A dataset containing 4 species occurrences available in GBIF matching the query:
{
 "and" : [
 "GadmGid is CHN.29_1",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Babax lanceolatus"
 ]
}

 The dataset includes 4 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0005550-260221153910048/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25921/smgk-ka88
title: NOAA/WDS Paleoclimatology - Cherubini - Mugello Valley UB - FASY - ITRDB ITAL037

description: Tree ring data from the International Tree Ring Data Bank and World Data Center for Paleoclimatology archives.  Most data sets include raw treering measurements (most are annual ring width, with some collections of earlywood or latewood width or wood density), plus chronologies (standardized growth indices for a site compiled from multiple treering samples). Reconstructions of climate variables are included with some of these data sets.  Each data type is stored in a separate data file; the data type is coded into the file name. For details please see: http://www.ncdc.noaa.gov/paleo/treeinfo.htmll
description: Collection purpose: 
# Assessment of forest GPP using NDVI (satellite data)
# 
# Cores are stored at: 
# 
# Notes: 
# forests were originally managed as a coppice, thinning between 1993 - 1998
# Formerly mugoB
# 
# References:
# Rodolfi et al (2007): 
# Assessment of forest GPP variations in central Italy. 
# Can. J. For. Res. 37, 1944-1953 NOAA Template Raw Measurements file added 2019-02-05.
DOI: 10.25921/s1qq-ax94
title: NOAA/WDS Paleoclimatology - Neuwirth - Nordrhein-Westfalen/Köln-Bonner Bucht drk03 - QURO - ITRDB GERM199

description: An improved understanding of the spatiotemporal climate/growth relationship of our forests is of particular importance for assessing the consequences of climate warming. A total of 67 stands of beech (Fagus sylvatica L.), pedunculate oak (Quercus robur L.), sessile oak (Quercus petraea (Matt.) Liebl.), Scots pine (Pinus sylvestris L.), and spruce (Picea abies Karst.) from sites located in the transition zone from the lowlands to the low mountain ranges of West Germany have been analysed. A combination of pointer year and cluster analysis was used to find groups with similar growth anomaly patterns over the 1941-2000 period. Shifted reaction patterns especially characterise differences in the growth behaviour of the clusters. These are controlled by different reactions to the climate conditions in winter and spring and are determined by a complex system of forcing factors. Results of this study reflect the enormous importance of the length of the growing season. Increasing the duration of the vegetation period climate warming can change the climate/growth relationship of trees, thereby confounding climate reconstructions which use tree rings. Since forcing factors have been detected that are more important than the tree species, we recommend the application of growth-specific approaches for the analysis of tree species' vulnerability to climate.
description: Purpose of Collection:
# climate/growth relationship NOAA Template Raw Measurements file added 2019-02-05.
DOI: 10.25921/stkp-3737
title: NOAA/WDS Paleoclimatology - Bräker - Lärchenwald - LADE - ITRDB SWIT360

description: Tree ring data from the International Tree Ring Data Bank and World Data Center for Paleoclimatology archives.  Most data sets include raw treering measurements (most are annual ring width, with some collections of earlywood or latewood width or wood density), plus chronologies (standardized growth indices for a site compiled from multiple treering samples). Reconstructions of climate variables are included with some of these data sets.  Each data type is stored in a separate data file; the data type is coded into the file name. For details please see: http://www.ncdc.noaa.gov/paleo/treeinfo.htmll
description: Collection purpose: 
# Growth and Yield
# 
# Notes: 
# Slope W 70%
# Formerly Wiesen_Laerche_n2(0)_1996.fh NOAA Template Raw Measurements file added 2019-02-05.
DOI: 10.25921/smg6-8v95
title: NOAA/WDS Paleoclimatology - Fischer - Rheinland-Pfalz/Westeifel dpe07 - PCAB - ITRDB GERM162

description: An improved understanding of the spatiotemporal climate/growth relationship of our forests is of particular importance for assessing the consequences of climate warming. A total of 67 stands of beech (Fagus sylvatica L.), pedunculate oak (Quercus robur L.), sessile oak (Quercus petraea (Matt.) Liebl.), Scots pine (Pinus sylvestris L.), and spruce (Picea abies Karst.) from sites located in the transition zone from the lowlands to the low mountain ranges of West Germany have been analysed. A combination of pointer year and cluster analysis was used to find groups with similar growth anomaly patterns over the 1941-2000 period. Shifted reaction patterns especially characterise differences in the growth behaviour of the clusters. These are controlled by different reactions to the climate conditions in winter and spring and are determined by a complex system of forcing factors. Results of this study reflect the enormous importance of the length of the growing season. Increasing the duration of the vegetation period climate warming can change the climate/growth relationship of trees, thereby confounding climate reconstructions which use tree rings. Since forcing factors have been detected that are more important than the tree species, we recommend the application of growth-specific approaches for the analysis of tree species' vulnerability to climate.
description: Purpose of Collection:
# climate/growth relationship NOAA Template Raw Measurements file added 2019-02-05.
DOI: 10.25921/sxkv-ht03
title: NOAA/WDS Paleoclimatology - Colenutt - Racehorse Pass - LALY - ITRDB CANA416

description: Tree ring data from the International Tree Ring Data Bank and World Data Center for Paleoclimatology archives.  Most data sets include raw treering measurements (most are annual ring width, with some collections of earlywood or latewood width or wood density), plus chronologies (standardized growth indices for a site compiled from multiple treering samples). Reconstructions of climate variables are included with some of these data sets.  Each data type is stored in a separate data file; the data type is coded into the file name. For details please see: http://www.ncdc.noaa.gov/paleo/treeinfo.htmll
description: Cores are stored at:
# # University of Western Ontario
# # 
# # 
# # References:
# # Colenutt M.  2000.  
# # Climate reconstruction in the southern Canadian Rockies using tree-ring data from alpine larch.  
# # PhD dissertation, University of Western Ontario, London, Ontario. NOAA Template Raw Measurements file added 2019-01-27. NOAA Template Raw Measurements file added 2019-02-04.
DOI: 10.25921/s93v-9a24
title: NOAA/WDS Paleoclimatology - Fischer - Nordrhein-Westfalen/Ostmünsterland drt03 - PISY - ITRDB GERM216

description: An improved understanding of the spatiotemporal climate/growth relationship of our forests is of particular importance for assessing the consequences of climate warming. A total of 67 stands of beech (Fagus sylvatica L.), pedunculate oak (Quercus robur L.), sessile oak (Quercus petraea (Matt.) Liebl.), Scots pine (Pinus sylvestris L.), and spruce (Picea abies Karst.) from sites located in the transition zone from the lowlands to the low mountain ranges of West Germany have been analysed. A combination of pointer year and cluster analysis was used to find groups with similar growth anomaly patterns over the 1941-2000 period. Shifted reaction patterns especially characterise differences in the growth behaviour of the clusters. These are controlled by different reactions to the climate conditions in winter and spring and are determined by a complex system of forcing factors. Results of this study reflect the enormous importance of the length of the growing season. Increasing the duration of the vegetation period climate warming can change the climate/growth relationship of trees, thereby confounding climate reconstructions which use tree rings. Since forcing factors have been detected that are more important than the tree species, we recommend the application of growth-specific approaches for the analysis of tree species' vulnerability to climate.
description: Purpose of Collection:
# climate/growth relationship NOAA Template Raw Measurements file added 2019-02-05.
DOI: 10.25921/sgfc-wd76
title: NOAA/WDS Paleoclimatology - Central Andes composite 4 Tree ring width, PAGES LOTRED-SA Version

description: This study presents a comprehensive assessment of high-resolution Southern Hemisphere (SH) paleoarchives covering the last 2000 years. We identified 174 monthly to annually resolved climate proxy (tree ring, coral, ice core, documentary, speleothem and sedimentary) records from the Hemisphere. We assess the interannual and decadal sensitivity of each proxy record to large-scale circulation indices from the Pacific, Indian and Southern Ocean regions over the twentieth century. We then analyse the potential of this newly expanded palaeoclimate network to collectively represent predictands (sea surface temperature, sea level pressure, surface air temperature and precipitation) commonly used in climate reconstructions. The key dynamical centres-of-action of the equatorial Indo-Pacific are well captured by the palaeoclimate network, indicating that there is considerable reconstruction potential in this region, particularly in the post AD 1600 period when a number of long coral records are available. Current spatiotemporal gaps in data coverage and regions where significant potential for future proxy collection exists are discussed. We then highlight the need for new and extended records from key dynamical regions of the Southern Hemisphere. Although large-scale climate field reconstructions for the SH are in their infancy, we report that excellent progress in the development of regional proxies now makes plausible estimates of continental- to hemispheric-scale climate variations possible.
description: Uploaded by R. Neukom, data obtained from original authors.
	These are not raw data but processed and truncated chronologies, representing a composite of two or more individual sites. Details see (Neukom and Gergis 2011, The Holocene, DOI: 10.1177/0959683611427335). For the raws contact the authors or/and check ITRDB.
DOI: 10.25921/shfn-v869
title: NOAA/WDS Paleoclimatology - Southern African Precipitation Reconstructions From Ships' Logbooks 1796-1854

description: Atmospheric circulation in the oceans surrounding southern Africa plays an important role in determining its precipitation. This study uses wind information recorded in ships' logbooks in order to statistically reconstruct summer and winter season precipitation at four southern African weather stations from 1796 to 1854. The reconstruction was obtained by first relating gridded 8 x 8 degree NCEP-DOE reanalysis seasonal mean wind vectors in the adjacent oceans to station precipitation. Over a 30-year calibration period (1979-2008), significant correlations between wind and precipitation at Cape Town, Mthatha and Royal National Park showed particular correspondence with those areas with the greatest concentration of logbook observations. Principal component regression was used to assess the potential of the dominant patterns of variability in the wind vectors as predictors to reconstruct precipitation. Cross-validation in the calibration period gave confidence that precipitation could be reconstructed at several stations across South Africa, meaning the regression relationships derived in the calibration period could be applied to the gridded seasonal mean logbook data to produce reconstructions of precipitation from 1796 to 1854. The reconstructions show a degree of correspondence with other regional data sets. For instance, the decade beginning in 1810 was the wettest of the period at Mthatha and Royal National Park, while the 1820s were the driest. At Cape Town, the 1820s were the wettest decade, with drier conditions observed in the 1830s. An index of west-east circulation in the summer season revealed correspondence with two documentary reconstructions of El Niño events and increased westerliness, although this did not always result in drier conditions. Attention is also drawn to the remaining 3000 yet to be digitised English East India Company logbooks which would provide a high-resolution picture of atmospheric circulation back to 1700 in the region under consideration.
description: Wind data from ships' logbooks are used to reconstruct precipitation at southern African rainfall stations, including Mthatha, Royal National Park and Cape Town, between 1796-1854. The reconstructions are based on relationships derived between NCEP-DOE 2 reanalysis u-wind data and station precipitation data over a calibration period of 1979-2008.
DOI: 10.25921/saqd-zh57
title: NOAA/WDS Paleoclimatology - Bear River, Utah 1,200 Year Streamflow Reconstruction

description: The Bear River contributes more water to the eastern Great Basin than any other river system. It is also the most significant source of water for the burgeoning Wasatch Front metropolitan area in northern Utah. Despite its importance for water resources for the region's agricultural, urban, and wildlife needs, our understanding of the variability of Bear River's stream flow derives entirely from the short instrumental record (1943-2010). Here we present a 1200-year calibrated and verified tree-ring reconstruction of stream flow for the Bear River that explains 67% of the variance of the instrumental record over the period from 1943 to 2010. Furthermore, we developed this reconstruction from a species that is not typically used for dendroclimatology, Utah juniper (Juniperus osteosperma). We identify highly significant periodicity in our reconstruction at quasi-decadal (7-8 year), multi-decadal (30 year), and centennial (>50 years) scales. The latter half of the 20th century was found to be the 2nd wettest (~40-year) period of the past 1200 years, while the first half of the 20th century marked the 4th driest period. The most severe period of reduced stream flow occurred during the Medieval Warm Period (ca. mid-1200s CE) and persisted for ~70 years. Upper-level circulation anomalies suggest that atmospheric teleconnections originating in the western tropical Pacific are responsible for the delivery of precipitation to the Bear River watershed during the October-December (OND) season of the previous year. The Bear River flow was compared to recent reconstructions of the other tributaries to the Great Salt Lake (GSL) and the GSL level. Implications for water management could be drawn from the observation that the latter half of the 20th century was the 2nd wettest in 1200 years, and that management for future water supply should take into account the stream flow variability over the past millennium.
description: Tree-ring-based reconstruction of Bear River, Utah streamflow over the past 1200 years.   Utah Juniper tree-ring data are archived in the International Tree-Ring Data Bank, Site Code UT541: 
https://www.ncdc.noaa.gov/paleo/study/19359
DOI: 10.25921/s64c-6g19
title: NOAA/WDS Paleoclimatology - Lake Titicaca 370KYr LT01-2B Sediment Data

description: A 136-m-long drill core of sediments was recovered from tropical high-altitude Lake Titicaca, Bolivia-Peru, enabling a reconstruction of past climate that spans four cycles of regional glacial advance and retreat and that is estimated to extend continuously over the last 370,000 yr. 
Within the errors of the age model, the periods of regional glacial advance and retreat are concordant respectively with global glacial and interglacial stages. Periods of ice advance in the southern tropical Andes generally were periods of positive water balance, as evidenced by deeper and fresher conditions in Lake Titicaca. Conversely, reduced glaciation occurred during periods of negative water balance and shallow closed-basin conditions in the lake. The apparent coincidence of positive water balance of Lake Titicaca and glacial growth in the adjacent Andes with Northern Hemisphere ice sheet expansion implies that regional water balance and glacial mass balance are strongly influenced by global-scale temperature changes, 
as well as by precessional forcing of the South American summer monsoon.
description: Carbon and diatom data from 136m long sediment core LT01-2B, Lake Titicaca, Bolivia/Peru, covering approximately 370,000 years.
DOI: 10.25921/sw4t-5603
title: NOAA/WDS Paleoclimatology - Mono Lake 150 Year Stable Isotope Data

description: The relationship between d18O and d13C in a closed-basin lake is a function of hydrological change, vapor exchange, lake productivity, and total CO2 (or carbonate alkalinity) concentration. Covariance of d18O and d13C usually occurs in lake sediments under the condition of hydrological closure for time periods of the order of 5000 yr or longer. On shorter time scales, however, certain subtleties in the use of the d13C-d18O covariance as a hydrology history indicator must be recognized. The covariant trend may not be found in hyper-alkaline lakes because of the insensitivity of d13C to lake volume changes. For less alkaline closed-basin lakes, covariance of d13C-d18O will result from relatively rapid increase or decrease of lake volume, with the rapid-decrease condition giving rise to heavy and narrow-ranged isotopic values for both d13C and d18O due to the coupled evaporation-productivity effect. When the lake volume remains stable (as is the case for an over-flowing open lake), poor d13C-d18O covariance will ensue, due to the effect of vapor exchange with the atmosphere.  We have used the measured d13C-d18O covariance in carbonate sediments of Mono Lake, California, to deduce paleo-hydrological and lake-water alkalinity (and salinity) variations and found the results in consonance with Holocene lake-level history derived from the d18O and other information.
description: Isotopic records of Mono Lake sediments, Core F3, California, USA.  d13C-d18O covariance in carbonate sediments of Mono Lake, California,  used to deduce Holocene paleohydrology and lake water alkalinity and salinity variations.