cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.5281/zenodo.18765993
title: MODERN CONCEPTS OF COMPREHENSIVE TREATMENT OF CHILDREN WITH CONGENITAL CLEFT PALATE AFTER URANOPLASTY (REVIEW)

description: In the domestic and international literature, there are a number of studies on the treatment outcomes of patients with cleft lip and palate, operated on at different ages using various uranoplasty techniques. However, there are no studies characterizing the relationship between biometric parameters of the maxilla and the uranoplasty technique. Comparative analysis of treatment outcomes in the vast majority of cases is conducted with an emphasis on a single diagnostic criterion. However, studying surgical outcomes in patients with cleft lip and palate is only possible using a comprehensive diagnostic algorithm that includes biometric analysis, graphic recording of maxillary parameters, and radiographic examination. Inadequate attention has been paid to graphic reconstructive analysis of the shape and size of the upper oral cavity in patients with congenital malformations of the maxillofacial region. The lack of information regarding the specific changes in the biometric parameters of the upper jaw using various methods of uranoplasty, as well as additional diagnostic methods for disorders of the dentoalveolar system in patients with congenital malformations, justifies further research in this area.
DOI: 10.15468/dl.qp2m5v
title: Occurrence Download

description: A dataset containing 67090 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is one of (Plantae, Aves, Insecta)",
 "Geometry MULTIPOLYGON (((17.07075 -22.52096, 17.0682 -22.48761, 17.01581 -22.48761, 17.01644 -22.49595, 17.00596 -22.49595, 17.00724 -22.51262, 16.99676 -22.51262, 16.99739 -22.52096, 17.00787 -22.52096, 17.00851 -22.5293, 17.01899 -22.5293, 17.02026 -22.54597, 17.00978 -22.54597, 17.01042 -22.55431, 16.99994 -22.55431, 17.00057 -22.56264, 17.03202 -22.56264, 17.03265 -22.57098, 17.04314 -22.57098, 17.04377 -22.57932, 17.05426 -22.57932, 17.05554 -22.59599, 17.06602 -22.59599, 17.0673 -22.61267, 17.09875 -22.61267, 17.09939 -22.62101, 17.10988 -22.62101, 17.10667 -22.57932, 17.11715 -22.57932, 17.11587 -22.56264, 17.10538 -22.56264, 17.10474 -22.55431, 17.09426 -22.55431, 17.09298 -22.53763, 17.0825 -22.53763, 17.08123 -22.52096, 17.07075 -22.52096)))"
 ]
}

 The dataset includes 67090 records from 81 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0008867-260221153910048/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25921/2b9y-6976
title: NOAA/WDS Paleoclimatology - Asian Monsoon Region Speleothem Triple Oxygen Isotope Data over the Past 300 Years

description: Characterization of moisture origins is crucial to understanding hydroclimatic processes. Nevertheless, documenting past atmospheric moisture contents and their sources remains challenging partially due to insufficient moisture-tracing proxies. Here, we present triple oxygen isotope compositions in 21 cave speleothems from monsoonal Asia to examine spatial moisture origin differences in eastern Asia over the past 300 years. Our data suggest an isotopic equilibrium fractionation during speleothem formation, and thus parent water 17O anomalies (Δ′17O) values reconstructed from speleothems preserve information on moisture origins and recycling across space. Notably, speleothem Δ′17O records exhibit a distinct geographical distribution, with low values in central-eastern and southern China, high values in northwestern and northern China, and relatively high values in the Yangtze River region. This spatial pattern underscores the diverse influence of different moisture sources regulated by regional hydrological circulation, and demonstrates the potential use of speleothem Δ′17O in reconstructing the moisture cycle at spatial scales.
DOI: 10.25921/26qz-fg69
title: NOAA/WDS Paleoclimatology - Hartl - Höllengebirge, Salzberg B - FASY - ITRDB AUT119

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
DOI: 10.25921/2a9w-1x62
title: NOAA/WDS Paleoclimatology - Hartl - Höllengebirge, Salzberg C - PCAB - ITRDB AUT120

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
DOI: 10.25921/2rgp-my12
title: NOAA/WDS Paleoclimatology - Iniguez fire data from Catalina Rose Canyon CRC02 - IMPD USCRC_02

description: Fire histories contribute important information to contemporary fire planning, however, our knowledge is not comprehensive geographically. We evaluated the influence of topography on fire history patterns in two contrasting landscapes within the Santa Catalina Mountains of southeastern Arizona. Multiple fire-scarred trees from randomly selected 2-ha plots were used to develop plot composite mean fire intervals (PCMFIs) within the Butterfly Peak (BP) and Rose Canyon (RC) landscapes. BP is dominated by steep, northerly aspects and presence of potential fire spread barriers (exposed rock bluffs and scree slopes). RC is dominated by more gentle and southerly aspects with relatively few fire barriers. Within each landscape, PCMFIs did not differ significantly between aspect classes from A.D. 1748 to 1910 (BP: p = 0.73 and RC: p = 0.57). Pooled PCMFIs in the gentler RC landscape were, however, significantly shorter (p < 0.001) than in the steeper BP landscape. The frequency of relatively widespread fires (i.e., number of fire years when ≥2 plots scarred) was similar between landscapes, but fires in the gentler RC landscape were significantly larger (p = 0.033). The higher frequency of large fires (i.e., fires that burned >75% of the landscape) in RC resulted in more area burned over time and shorter fire intervals at individual plots. Conversely, smaller fires in the dissected BP landscape resulted in less area burned and longer periods between fires at individual plots. The different topographies in the two landscapes likely result in different wind intensities, fuel moistures, and fuel/vegetation types—and consequently, different historical fire spread patterns. Our conclusion is that fire history patterns are not influenced primarily by stand-scale topography, but rather by the topographic characteristics of the broader, surrounding landscape.
description: 
This dataset was contributed as part of the North American Tree-ring Fire Scar Synthesis (NAFSS) project (https://www.ncei.noaa.gov/access/paleo-search/study/34853). Data were contributed to the project from the original data generators.

Sample Storage Location: Laboratory of Tree-Ring, University of Arizona
Dating Method: Dated
Related ITRDB_Chronology: Not Applicable

Fire scar data from this site are available in FHX2 format at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscrc_02.fhx
along with associated metadata at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscrc_02-noaa.txt
DOI: 10.25921/2q5q-e813
title: NOAA/WDS Paleoclimatology - Iniguez fire data from Catalina Rose Canyon CRC06 - IMPD USCRC_06

description: Fire histories contribute important information to contemporary fire planning, however, our knowledge is not comprehensive geographically. We evaluated the influence of topography on fire history patterns in two contrasting landscapes within the Santa Catalina Mountains of southeastern Arizona. Multiple fire-scarred trees from randomly selected 2-ha plots were used to develop plot composite mean fire intervals (PCMFIs) within the Butterfly Peak (BP) and Rose Canyon (RC) landscapes. BP is dominated by steep, northerly aspects and presence of potential fire spread barriers (exposed rock bluffs and scree slopes). RC is dominated by more gentle and southerly aspects with relatively few fire barriers. Within each landscape, PCMFIs did not differ significantly between aspect classes from A.D. 1748 to 1910 (BP: p = 0.73 and RC: p = 0.57). Pooled PCMFIs in the gentler RC landscape were, however, significantly shorter (p < 0.001) than in the steeper BP landscape. The frequency of relatively widespread fires (i.e., number of fire years when ≥2 plots scarred) was similar between landscapes, but fires in the gentler RC landscape were significantly larger (p = 0.033). The higher frequency of large fires (i.e., fires that burned >75% of the landscape) in RC resulted in more area burned over time and shorter fire intervals at individual plots. Conversely, smaller fires in the dissected BP landscape resulted in less area burned and longer periods between fires at individual plots. The different topographies in the two landscapes likely result in different wind intensities, fuel moistures, and fuel/vegetation types—and consequently, different historical fire spread patterns. Our conclusion is that fire history patterns are not influenced primarily by stand-scale topography, but rather by the topographic characteristics of the broader, surrounding landscape.
description: 
This dataset was contributed as part of the North American Tree-ring Fire Scar Synthesis (NAFSS) project (https://www.ncei.noaa.gov/access/paleo-search/study/34853). Data were contributed to the project from the original data generators.

Sample Storage Location: Laboratory of Tree-Ring, University of Arizona
Dating Method: Dated
Related ITRDB_Chronology: Not Applicable

Fire scar data from this site are available in FHX2 format at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscrc_06.fhx
along with associated metadata at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscrc_06-noaa.txt
DOI: 10.25921/2x0n-8n11
title: NOAA/WDS Paleoclimatology - Hartl - Oberammergau, Laichwald B - ABAL - ITRDB DEU372

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
DOI: 10.25921/2c7x-2p69
title: NOAA/WDS Paleoclimatology - Hartl - Schliersee, Hausberg-Alm oben - PCAB - ITRDB DEU407

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
DOI: 10.25921/2h15-vm82
title: NOAA/WDS Paleoclimatology - Hartl - Schliersee, Hausberg-Alm oben - LADE - ITRDB DEU411

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
DOI: 10.25921/25jn-w916
title: NOAA/WDS Paleoclimatology - Lake Superior Region Lake Sediment Geochemistry Data over the last 10,000 Years

description: Determining the timing and transport mechanisms (i.e. fluvial and/or atmospheric) of pollution associated with ancient copper mining on Isle Royale in Lake Superior (United States) is important for understanding the current and future trajectory of ecosystems affected by human activity. This study reports metal concentrations in sediment from two small, closed-basin lakes located on Isle Royale (Lily Lake and Pond 2) as a measure of the extent of heavy metal emissions from Indigenous, precontact mining and annealing activities associated with one of the world’s oldest metal working industries. Lily Lake and Pond 2 are both located near known mines, but neither lake contains mines in its catchment and thus could not have received pollution via fluvial transport. Elevated concentrations of lead in sediments dating to ~6000 years ago at both lakes provide evidence of at- mospheric transport of pollution associated with mining emissions. The age of ~6000 years before present is consistent with the timing of elevated lead concentrations in sediment from McCargoe Cove on the northern shore of Isle Royale. Collectively, the data indicate that the peak in Archaic Period mining occurred on south- western Isle Royale ~6000 years ago and was preceded by periods that varied in intensity and location across the area. The discovery of pollution signals in lake sediments from the Lake Superior region provides clues as to the timing, spatial patterns, and magnitude of one of the world’s earliest large-scale metal mining efforts. These findings provide a basis for determining the transport mechanisms of ancient mining pollution and are a step toward assessing the full environmental impact of mining and metal working efforts by early human civilizations.
description: Provided Keywords: ancient pollution, copper mining, Lake Superior, lake sediment, lead pollution, metallurgy
DOI: 10.25921/24rp-df66
title: NOAA/WDS Paleoclimatology - Coulthard - Joffre Lakes Update - TSME - ITRDB CAN674

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: Update to Joffre Lakes collections, ITRDB site codes CANA640, CANA641. Cores with IDs JOFxxxxx are 2023 update.
DOI: 10.25921/2gt7-tm58
title: NOAA/WDS Paleoclimatology - Iniguez fire data from Catalina Butterfly Peak Plot 01 - IMPD USCBP_01

description: Fire histories contribute important information to contemporary fire planning, however, our knowledge is not comprehensive geographically. We evaluated the influence of topography on fire history patterns in two contrasting landscapes within the Santa Catalina Mountains of southeastern Arizona. Multiple fire-scarred trees from randomly selected 2-ha plots were used to develop plot composite mean fire intervals (PCMFIs) within the Butterfly Peak (BP) and Rose Canyon (RC) landscapes. BP is dominated by steep, northerly aspects and presence of potential fire spread barriers (exposed rock bluffs and scree slopes). RC is dominated by more gentle and southerly aspects with relatively few fire barriers. Within each landscape, PCMFIs did not differ significantly between aspect classes from A.D. 1748 to 1910 (BP: p = 0.73 and RC: p = 0.57). Pooled PCMFIs in the gentler RC landscape were, however, significantly shorter (p < 0.001) than in the steeper BP landscape. The frequency of relatively widespread fires (i.e., number of fire years when ≥2 plots scarred) was similar between landscapes, but fires in the gentler RC landscape were significantly larger (p = 0.033). The higher frequency of large fires (i.e., fires that burned >75% of the landscape) in RC resulted in more area burned over time and shorter fire intervals at individual plots. Conversely, smaller fires in the dissected BP landscape resulted in less area burned and longer periods between fires at individual plots. The different topographies in the two landscapes likely result in different wind intensities, fuel moistures, and fuel/vegetation types—and consequently, different historical fire spread patterns. Our conclusion is that fire history patterns are not influenced primarily by stand-scale topography, but rather by the topographic characteristics of the broader, surrounding landscape.
description: 
This dataset was contributed as part of the North American Tree-ring Fire Scar Synthesis (NAFSS) project (https://www.ncei.noaa.gov/access/paleo-search/study/34853). Data were contributed to the project from the original data generators.

Sample Storage Location: Laboratory of Tree-Ring, University of Arizona
Dating Method: Dated
Related ITRDB_Chronology: Not Applicable

Fire scar data from this site are available in FHX2 format at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscbp_01.fhx
along with associated metadata at:
  https://www.ncei.noaa.gov/pub/data/paleo/firehistory/firescar/northamerica/uscbp_01-noaa.txt
DOI: 10.25921/25zs-1t89
title: NOAA/WDS Paleoclimatology - Ammersee 15,000 Year Ostracod Oxygen Isotope Data

description: Oxygen-isotope ratios of precipitation (delta 18OP) inferred from deep-lake ostracods from the Ammersee (southern Germany) provide a climate record with decadal resolution. The record in detail shows many of the rapid climate shifts seen in central Greenland ice cores between 15,000 and 5000 years before the present (B.P.). Negative excursions in the estimated delta 18OP from both of these records likely reflect short weakenings of the thermohaline circulation caused by episodic discharges of continental freshwater into the North Atlantic. Deviating millennial-scale trends, however, indicate that climate gradients between Europe and Greenland changed systematically, reflecting a gradual rearrangement of North Atlantic circulation during deglaciation.
description: The file contains a compilation of oxygen isotope values measured on juvenile valves of three different species of Candona from four cores taken in the profundal plain of Ammersee, Southern Germany. Temporal coverage of a sample varies and is less than 3 years for the youngest samples (AS Tmax), increasing to more 20 years for oldest (base of AS96- 1). The periods between 15500 calendar years BP to 5300 calendar years BP and the last 300 years are represented by continuous samples of 1-cm slices (cores AS Tmax, AS93-1, and AS92-5) or 0.5-cm slices (core AS96-1). The period between 5300 and 300 calendar years BP is represented by discontinuous 1-cm samples at 10-cm intervals.

Please refer to the original publications for details concerning the chronology. The chronology of ASTmax is based on varve-counting, confirmed by Cs137 and PB210 and by the identification of several historical flood events. Cores AS92-5, AS93-1, and AS96-1 are dated by using a combination of radiocarbon dates, a well dated tephra layer, and by correlating to an absolutely dated varved lake sequence, which confirms a second, independently produced correlation to the GRIP Summit delta-18O ice record.

The upper, highest resolution portion of the Ammersee stable isotope record successfully reproduces measured mean annual air temperatures over the last 200 years (von Grafenstein et al. 1996).
DOI: 10.25921/2t5x-vv10
title: NOAA/WDS Paleoclimatology - Greenland Lake Sediment Magnetic Susceptibility and Titanium Concentration Data over the Past 12 ka

description: Greenland Ice Sheet (GrIS) outlet glaciers are currently losing mass, leading to sea level rise. Reconstructions of past outlet glacier behavior through the Holocene help us better understand how they respond to climate change. Kiattuut Sermiat, a southern Greenland outlet glacier near Narsarsuaq, is known to have experienced an unusually large Late Holocene advance that culminated at ~1600 cal yr BP and exceeded the glacier's Little Ice Age extent. We report sedimentary records from two lakes at slightly different elevations in an upland valley adjacent to Kiattuut Sermiat. These reveal when the outlet glacier's surface elevation was higher than during the Little Ice Age and constrain the associated outlet glacier surface elevation. We use bulk sediment geochemistry, magnetic susceptibility, color, texture, and the presence of aquatic plant macrofossils to distinguish between till, glaciolacustrine sediments, and organic lake sediments. Our 14C results above basal till recording regional deglaciation skew slightly old due to a reservoir effect but are generally consistent with regional deglaciation occurring ~11,000 cal yr BP. Neoglacial advance of Kiattuut Sermiat is recorded by deposition of glaciolacustrine sediments in the lower-elevation lake, which we infer was subsumed by an ice-dammed lake that formed along the glacier's margin just after ~3900 cal yr BP. This timing is consistent with several other glacial records in Greenland showing neoglacial cooling driving advance between ~4500–3000 cal yr BP. Given that glaciolacustrine sediments were deposited only in the lower-elevation lake, combined with glacial geomorphological evidence in the valley containing these lakes, we estimate the former ice margin's elevation to have been ~670 m a.s.l., compared with ~420 m a.s.l. today. The ice-dammed lake persisted until the glacier surface fell below this elevation at ~1600 cal yr BP. The retreat timing contrasts with overall evidence for cooling and glacier advance in the region at that time, so we infer that Kiattuut Sermiat's retreat may have resulted from reduced snowfall amounts and/or local glaciological complexity. High sensitivity to precipitation changes could also explain the relatively limited Little Ice Age advance of Kiattuut Sermiat compared with the earlier neoglacial advance.