Study includes 2 other sites which do not meet Holocene age criteria. dDn-C26 is the primary variable used for precipitation interpretation
Study includes 2 other sites which do not meet Holocene age criteria. dDn-C26 is the primary variable used for precipitation interpretation
Study includes 2 other sites which do not meet Holocene age criteria. dDn-C26 is the primary variable used for precipitation interpretation
Study includes 2 other sites which do not meet Holocene age criteria. dDn-C26 is the primary variable used for precipitation interpretation
Study includes 2 other sites which do not meet Holocene age criteria. dDn-C26 is the primary variable used for precipitation interpretation
not publically available
not publically available
not publically available
Entered by K . DeLong, who also did a quick age model of data
Entered by K . DeLong, who also did a quick age model of data
Monthly and Bimonthly d18O measurements of a Porites coral collected from Doangdoangan Besar in the southern Makassar Strait. The d18O data were determined using isotope ratio mass spectrometry (IRMS)
Monthly and Bimonthly d18O measurements of a Porites coral collected from Doangdoangan Besar in the southern Makassar Strait. The d18O data were determined using isotope ratio mass spectrometry (IRMS)
Monthly and Bimonthly d18O measurements of a Porites coral collected from Doangdoangan Besar in the southern Makassar Strait. The d18O data were determined using isotope ratio mass spectrometry (IRMS)
Monthly and Bimonthly d18O measurements of a Porites coral collected from Doangdoangan Besar in the southern Makassar Strait. The d18O data were determined using isotope ratio mass spectrometry (IRMS)
for IS02K Diploastrea heliopora data
for IS02K Diploastrea heliopora data
for IS02K Diploastrea heliopora data
for IS02K Diploastrea heliopora data
for IS02K Diploastrea heliopora data
for IS02K Diploastrea heliopora data
for iso2K, coral name is BON-3-B
for iso2K, coral name is BON-3-B
for iso2K, coral name is BON-3-B
for iso2K, coral name is BON-3-DII
for iso2K, coral name is BON-3-DII
for iso2K, coral name is BON-3-DII
for iso2K, coral name is BON-3-F-B
for iso2K, coral name is BON-3-F-B
for iso2K, coral name is BON-3-F-B
for iso2K, coral name is BON-3-F-C
for iso2K, coral name is BON-3-F-C
for iso2K, coral name is BON-3-F-C
for iso2K, coral name is BON-9-E
for iso2K, coral name is BON-9-E
for iso2K, coral name is BON-9-E
for iso2K, coral name is BON-1-AII
for iso2K, coral name is BON-1-AII
for iso2K, coral name is BON-1-AII
for iso2K, coral name is BON-1-BI
for iso2K, coral name is BON-1-BI
for iso2K, coral name is BON-1-BI
Input by K. DeLong, E. Dassie emailed her data, not on NOAA yet
Input by K. DeLong, E. Dassie emailed her data, not on NOAA yet
K. DeLong put together for ISO2K
K. DeLong put together for ISO2K
K. DeLong put together for ISO2K
K. DeLong put together for ISO2K
K. DeLong put together for ISO2K
K. DeLong put together for ISO2K, Coral D3
K. DeLong put together for ISO2K, Coral D3
K. DeLong put together for ISO2K, Coral D3
K. DeLong put together for ISO2K, Coral D3
K. DeLong put together for ISO2K, Coral D3
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
This is a composite record representing two permafrost cores from the DHP174 peatland (Dempster Highway peatland, near the 174 km marker), and covering the last 13.6 ka. This record is comparable in ways to an ice core, but different in that it accumulates below the surface and traps primarily summer precipitation. Likewise, the temperature reconstruction is linked to the summer season.
Core PLC97-1
Core PLC97-1
Core PLC97-1
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
File updated from "Tibetanus.Hammarlund.2002"
14C data are at: https://doi.org/10.1080/11035899801201059
Revised for Iso2k by D. Kaufman from original file: Sonk11D.Lauterbach.2014
Revised for Iso2k by D. Kaufman from original file: Sonk11D.Lauterbach.2014
Revised for Iso2k by D. Kaufman from original file: Sonk11D.Lauterbach.2014
Revised for Iso2k by D. Kaufman from original file: Sonk11D.Lauterbach.2014
Revised for Iso2k by D. Kaufman from original file: Sonk11D.Lauterbach.2014
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
No depth data for proxy data provided by authors.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
In original online data source, Newton et al only provide Mg/Ca ratios, so these had to be converted to Mg/Ca SST using equations in paper. Also, no agedepth model was provided, though 14C date information was, so a direct pointtopoint linear interpolation age model was generated. All O2KLR records have been qualitycontrolled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement. Dataset recorded in this file is truncated to last 2000 years.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement.
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
All O2K-LR records have been quality-controlled according to protocols published in Nature Geoscience supplement
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
reductive cleaning step; Mg/Ca calibration adjusted to account for 10% reduction in Mg/Ca ratio
turbidite between 170-190 cm, below 2k interval
turbidite between 170-190 cm, below 2k interval
turbidite between 170-190 cm, below 2k interval
turbidite between 170-190 cm, below 2k interval
turbidite between 170-190 cm, below 2k interval
turbidite between 170-190 cm, below 2k interval
A composite d18O time-series representing pooled tree-ring samples (4-6 trees) of Tibetan juniper (Juniperus tibetica)
A composite d18O time-series representing pooled tree-ring samples (4-6 trees) of Tibetan juniper (Juniperus tibetica)
Composite tree-ring d18O record representing the average of up to 8 Rocky Mountain Bristlecone Pine (Pinus aristata) trees in any given year of the composite record.
Composite tree-ring d18O record representing the average of up to 8 Rocky Mountain Bristlecone Pine (Pinus aristata) trees in any given year of the composite record.
Composite d18O record representing 8 Cedrela odorata trees
Composite d18O record representing 8 Cedrela odorata trees
Composite tree-ring d18O record representing up to 5 trees (Mimosa acantholoba) in any given year; mean inter-tree correlation = 0.83 (p < 0.01).
Composite tree-ring d18O record representing up to 5 trees (Mimosa acantholoba) in any given year; mean inter-tree correlation = 0.83 (p < 0.01).
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at the Arcata site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 3 Coast Redwood (Sequoia sempervirens) trees at Jedediah Smith State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Middle-wood and Late-wood d18O records from 4 Coast Redwood (Sequoia sempervirens) trees at Prairie Creek State Park site, NW California.
Composite tree-ring d18O record representing five Pinus uncinata trees
Composite tree-ring d18O record representing five Pinus uncinata trees
Composite d18O record representing 9 Cedrela odorata trees
Composite d18O record representing 9 Cedrela odorata trees
This record represents a regional composite tree-ring d18O record, developed from sub-fossil and living trees from 20 sites in SE Sweden with a spatial range of 57.04-58.59°N and 14.08-16.44°E. The set of coordinates and elevation given for this record correspond to the middle of the total spatial range.
This record represents a regional composite tree-ring d18O record, developed from sub-fossil and living trees from 20 sites in SE Sweden with a spatial range of 57.04-58.59°N and 14.08-16.44°E. The set of coordinates and elevation given for this record correspond to the middle of the total spatial range.
A composite d18O time-series representing pooled tree-ring samples (up to 8 trees) of Tibetan juniper (Juniperus tibetica)
A composite d18O time-series representing pooled tree-ring samples (up to 8 trees) of Tibetan juniper (Juniperus tibetica)
Tree-ring chronology from Manali, India
Tree-ring chronology from Manali, India
The is a composite d18O record representing seven individual Nothofagus pumilio trees
The is a composite d18O record representing seven individual Nothofagus pumilio trees
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Liriodendron tulipifera trees, and site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Quercus rubra trees.
Site-averaged latewood d18O record representing 5 Quercus rubra trees.