Version history for eFCNDlR71j01xuy6XEpB - ParuCo.Bird.2014
Version: 1.0.14
- lastVersion: 1.0.13
- curator: nicholas
- timestamp: 2023-08-10 23:10:51 UTC
- changes:
- Base metadata:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_proxy: ‘((( PCA ))) deleteMe ///
multiproxy’ has been replaced by ‘multiproxy’
Version: 1.0.13
- lastVersion: 1.0.12
- curator: nicholas
- timestamp: 2023-07-05 00:53:37 UTC
- changes:
- Publication metadata:
- pub1_doi: ‘10..1016/j.epsl.2014.05.017’ has been replaced by
‘10.1016/j.epsl.2014.05.017’
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_proxy: ‘multiproxy’ has been replaced
by ‘((( PCA ))) deleteMe /// multiproxy’
- Paleo Interpretation metadata:
Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-05-31 20:39:58 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_notes: ‘((( ((( ““We suggest that PC1
reflects oscillations between two end member depositional environments
with fines indicative of deep lake conditions and coarser material
reflective of shallower lake conditions (i.e., littoral zone
sediments)…onsistent with the grain-size lake-level model, very fine to
fine sand abundances increased during the middle Holocene as ��Dwax
increased and PC1 and lithic flux decreased, suggesting diminished ISM
rainfall reduced clastic (i.e., silt) deposition and lowered lake
level”; paleoData_method has been standardized; paleoData_proxy updated
))) ““We suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized /// ““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized ))) ““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as dDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized /// ““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized’ has been
replaced by ‘““We suggest that PC1 reflects oscillations between two end
member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as dDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized’
Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-05-30 15:50:11 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_notes: ‘““We suggest that PC1 reflects
oscillations between two end member depositional environments with fines
indicative of deep lake conditions and coarser material reflective of
shallower lake conditions (i.e., littoral zone sediments)…onsistent with
the grain-size lake-level model, very fine to fine sand abundances
increased during the middle Holocene as δDwax increased and PC1 and
lithic flux decreased, suggesting diminished ISM rainfall reduced
clastic (i.e., silt) deposition and lowered lake level”;
paleoData_method has been standardized’ has been replaced by ‘((( (((
““We suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as ��Dwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized;
paleoData_proxy updated ))) ““We suggest that PC1 reflects oscillations
between two end member depositional environments with fines indicative
of deep lake conditions and coarser material reflective of shallower
lake conditions (i.e., littoral zone sediments)…onsistent with the
grain-size lake-level model, very fine to fine sand abundances increased
during the middle Holocene as δDwax increased and PC1 and lithic flux
decreased, suggesting diminished ISM rainfall reduced clastic (i.e.,
silt) deposition and lowered lake level”; paleoData_method has been
standardized /// ““We suggest that PC1 reflects oscillations between two
end member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as δDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized ))) ““We suggest that PC1 reflects oscillations between two
end member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as dDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized /// ““We suggest that PC1 reflects oscillations between two
end member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as δDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized’
- PC1 (WEB88f459b8): paleoData_QCCertification: NULL has been replaced
by ‘CR’
Version: 1.0.10
- lastVersion: 1.0.9
- curator: nicholas
- timestamp: 2023-05-12 22:07:18 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_notes: ‘((( ““We suggest that PC1
reflects oscillations between two end member depositional environments
with fines indicative of deep lake conditions and coarser material
reflective of shallower lake conditions (i.e., littoral zone
sediments)…onsistent with the grain-size lake-level model, very fine to
fine sand abundances increased during the middle Holocene as ��Dwax
increased and PC1 and lithic flux decreased, suggesting diminished ISM
rainfall reduced clastic (i.e., silt) deposition and lowered lake
level”; paleoData_method has been standardized; paleoData_proxy updated
))) ““We suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized /// ““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized’ has been
replaced by ‘““We suggest that PC1 reflects oscillations between two end
member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as δDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized’
Version: 1.0.9
- lastVersion: 1.0.8
- curator: nicholas
- timestamp: 2023-03-24 22:26:01 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_proxyGeneral: ‘hybrid’ has been
replaced by ‘multiproxy’
- PC1 (WEB88f459b8): paleoData_proxy: NULL has been replaced by
‘multiproxy’
- Paleo Interpretation metadata:
- PC1 (WEB88f459b8): interpretation1_variable: ‘P-E’ has been replaced
by ‘effectivePrecipitation’
Version: 1.0.8
- lastVersion: 1.0.7
- curator: nicholas
- timestamp: 2023-02-13 23:54:04 UTC
- changes:
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_notes: ‘““We suggest that PC1 reflects
oscillations between two end member depositional environments with fines
indicative of deep lake conditions and coarser material reflective of
shallower lake conditions (i.e., littoral zone sediments)…onsistent with
the grain-size lake-level model, very fine to fine sand abundances
increased during the middle Holocene as δDwax increased and PC1 and
lithic flux decreased, suggesting diminished ISM rainfall reduced
clastic (i.e., silt) deposition and lowered lake level”;
paleoData_method has been standardized’ has been replaced by ‘((( ““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as ��Dwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”; paleoData_method has been standardized;
paleoData_proxy updated ))) ““We suggest that PC1 reflects oscillations
between two end member depositional environments with fines indicative
of deep lake conditions and coarser material reflective of shallower
lake conditions (i.e., littoral zone sediments)…onsistent with the
grain-size lake-level model, very fine to fine sand abundances increased
during the middle Holocene as δDwax increased and PC1 and lithic flux
decreased, suggesting diminished ISM rainfall reduced clastic (i.e.,
silt) deposition and lowered lake level”; paleoData_method has been
standardized /// ““We suggest that PC1 reflects oscillations between two
end member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as δDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized’
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2023-02-09 16:08:42 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘4845’
- Paleo Column metadata:
- lithics (WEB1e2bd571): paleoData_notes: NULL has been replaced by
‘NA; paleoData_measurementMaterial has been standardized’
- lithics (WEB1e2bd571): paleoData_variableName: ‘Lithics’ has been
replaced by ‘lithics’
- lithics (WEB1e2bd571): paleoData_measurementMaterial: NULL has been
replaced by ‘lithics’
- lithics (WEB39ef1ed2): paleoData_notes: NULL has been replaced by
‘NA; paleoData_summaryStatistic has been standardized;
paleoData_measurementMaterial has been standardized’
- lithics (WEB39ef1ed2): paleoData_units: ‘g/cm^2/y’ has been replaced
by ‘g/cm2/yr’
- lithics (WEB39ef1ed2): paleoData_variableName: ‘Lithic Flux’ has
been replaced by ‘lithics’
- lithics (WEB39ef1ed2): paleoData_measurementMaterial: NULL has been
replaced by ‘lithics’
- lithics (WEB39ef1ed2): paleoData_summaryStatistic: NULL has been
replaced by ‘flux’
- BSi (WEB5b6c141d): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_method has been standardized’
- BSi (WEB5b6c141d): paleoData_variableName: ‘Inferred BSi’ has been
replaced by ‘BSi’
- BSi (WEB5b6c141d): paleoData_method: NULL has been replaced by
‘inferred’
- PC1 (WEB88f459b8): paleoData_notes: ‘““We suggest that PC1 reflects
oscillations between two end member depositional environments with fines
indicative of deep lake conditions and coarser material reflective of
shallower lake conditions (i.e., littoral zone sediments)…onsistent with
the grain-size lake-level model, very fine to fine sand abundances
increased during the middle Holocene as δDwax increased and PC1 and
lithic flux decreased, suggesting diminished ISM rainfall reduced
clastic (i.e., silt) deposition and lowered lake level”’ has been
replaced by ‘““We suggest that PC1 reflects oscillations between two end
member depositional environments with fines indicative of deep lake
conditions and coarser material reflective of shallower lake conditions
(i.e., littoral zone sediments)…onsistent with the grain-size lake-level
model, very fine to fine sand abundances increased during the middle
Holocene as δDwax increased and PC1 and lithic flux decreased,
suggesting diminished ISM rainfall reduced clastic (i.e., silt)
deposition and lowered lake level”; paleoData_method has been
standardized’
- PC1 (WEB88f459b8): paleoData_proxy: ‘PCA’ has been replaced by
NULL
- PC1 (WEB88f459b8): paleoData_method: NULL has been replaced by
‘principal components’
- dryBulkDensity (WEB99c4425f): paleoData_units: ‘g/cc’ has been
replaced by ‘g/cm3’
- dryBulkDensity (WEB99c4425f): paleoData_variableName: ‘Dry Bulk
Density’ has been replaced by ‘dryBulkDensity’
- age (WEBe9bf2e19): paleoData_datum: NULL has been replaced by
‘1950’
- age (WEBe9bf2e19): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized; paleoData_datum has been
standardized’
- age (WEBe9bf2e19): paleoData_units: ‘BP’ has been replaced by ‘yr
BP’
- age (WEBe9bf2e19): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- depth (WEBf197c5b3): paleoData_notes: NULL has been replaced by ‘NA;
paleoData_isPrimary has been standardized’
- depth (WEBf197c5b3): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- organicMatter (WEBf6f06516): paleoData_variableName: ‘OM’ has been
replaced by ‘organicMatter’
- Paleo Interpretation metadata:
- PC1 (WEB88f459b8): interpretation1_seasonality:
‘1,2,3,4,5,6,7,8,9,10,11,12’ has been replaced by ‘Annual’
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2022-07-28 17:39:15 UTC
- changes:
- Geographic metadata:
- geo_elevation: ‘4845’ has been replaced by NULL
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2022-07-15 23:08:24 UTC
- changes:
- Base metadata:
- Publication metadata:
- Paleo Interpretation metadata:
- Lithics (WEB1e2bd571): interpretation1_scope: NULL has been replaced
by ‘climate’
- Lithic Flux (WEB39ef1ed2): interpretation1_scope: NULL has been
replaced by ‘climate’
- Inferred BSi (WEB5b6c141d): interpretation1_scope: NULL has been
replaced by ‘climate’
- Dry Bulk Density (WEB99c4425f): interpretation1_scope: NULL has been
replaced by ‘climate’
- PC2 (WEBf1800d04): interpretation1_scope: NULL has been replaced by
‘climate’
- OM (WEBf6f06516): interpretation1_scope: NULL has been replaced by
‘climate’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2022-05-18 00:29:02 UTC
- changes:
- Base metadata:
- archiveType: ‘Lake Sediment’ has been replaced by
‘LakeSediment’
- Paleo Column metadata:
- Lithics (WEB1e2bd571): paleoData_archiveType: ‘Lake Sediment’ has
been replaced by ‘LakeSediment’
- Lithics (WEB1e2bd571): paleoData_units: ‘%’ has been replaced by
‘percent’
- Lithics (WEB1e2bd571): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- Lithics (WEB1e2bd571): paleoData_unitsOriginal: NULL has been
replaced by ‘%’
- Lithic Flux (WEB39ef1ed2): paleoData_archiveType: ‘Lake Sediment’
has been replaced by ‘LakeSediment’
- Lithic Flux (WEB39ef1ed2): paleoData_archiveTypeOriginal: NULL has
been replaced by ‘Lake Sediment’
- Inferred BSi (WEB5b6c141d): paleoData_archiveType: ‘Lake Sediment’
has been replaced by ‘LakeSediment’
- Inferred BSi (WEB5b6c141d): paleoData_units: ‘%’ has been replaced
by ‘percent’
- Inferred BSi (WEB5b6c141d): paleoData_archiveTypeOriginal: NULL has
been replaced by ‘Lake Sediment’
- Inferred BSi (WEB5b6c141d): paleoData_unitsOriginal: NULL has been
replaced by ‘%’
- PC1 (WEB88f459b8): paleoData_archiveType: ‘Lake Sediment’ has been
replaced by ‘LakeSediment’
- PC1 (WEB88f459b8): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- PC1 (WEB88f459b8): paleoData_proxyLumps: NULL has been replaced by
‘PCA’
- Dry Bulk Density (WEB99c4425f): paleoData_archiveType: ‘Lake
Sediment’ has been replaced by ‘LakeSediment’
- Dry Bulk Density (WEB99c4425f): paleoData_archiveTypeOriginal: NULL
has been replaced by ‘Lake Sediment’
- age (WEBe9bf2e19): paleoData_archiveType: ‘Lake Sediment’ has been
replaced by ‘LakeSediment’
- age (WEBe9bf2e19): paleoData_units: ‘yr BP’ has been replaced by
‘BP’
- age (WEBe9bf2e19): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- age (WEBe9bf2e19): paleoData_unitsOriginal: NULL has been replaced
by ‘yr BP’
- PC2 (WEBf1800d04): paleoData_archiveType: ‘Lake Sediment’ has been
replaced by ‘LakeSediment’
- PC2 (WEBf1800d04): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- depth (WEBf197c5b3): paleoData_archiveType: ‘Lake Sediment’ has been
replaced by ‘LakeSediment’
- depth (WEBf197c5b3): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- OM (WEBf6f06516): paleoData_archiveType: ‘Lake Sediment’ has been
replaced by ‘LakeSediment’
- OM (WEBf6f06516): paleoData_units: ‘%’ has been replaced by
‘percent’
- OM (WEBf6f06516): paleoData_archiveTypeOriginal: NULL has been
replaced by ‘Lake Sediment’
- OM (WEBf6f06516): paleoData_unitsOriginal: NULL has been replaced by
‘%’
- Paleo Interpretation metadata:
- Lithics (WEB1e2bd571): interpretation1_scope: ‘climate’ has been
replaced by NULL
- Lithic Flux (WEB39ef1ed2): interpretation1_scope: ‘climate’ has been
replaced by NULL
- Inferred BSi (WEB5b6c141d): interpretation1_scope: ‘climate’ has
been replaced by NULL
- PC1 (WEB88f459b8): interpretation1_variableGroup: NULL has been
replaced by ‘P-E’
- Dry Bulk Density (WEB99c4425f): interpretation1_scope: ‘climate’ has
been replaced by NULL
- PC2 (WEBf1800d04): interpretation1_scope: ‘climate’ has been
replaced by NULL
- OM (WEBf6f06516): interpretation1_scope: ‘climate’ has been replaced
by NULL
- Chron Column metadata:
- material (WEB8bfdbc85): chronData_variableName: ‘Material’ has been
replaced by ‘material’
- material (WEB8bfdbc85): chronData_variableNameOriginal: NULL has
been replaced by ‘Material’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2021-11-19 21:09:53 UTC
- changes:
- Paleo Interpretation metadata:
- PC1 (WEB88f459b8): interpretation1_seasonality: ‘Annual’ has been
replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’
- PC1 (WEB88f459b8): interpretation1_seasonalityGeneral: NULL has been
replaced by ‘Annual’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2021-11-17 02:09:23 UTC
- changes:
- Geographic metadata:
- geo_gcmdLocation: NULL has been replaced by ‘Asia>Eastern
Asia>China’
- Paleo Column metadata:
- PC1 (WEB88f459b8): paleoData_proxy: ‘sediment’ has been replaced by
‘PCA’
- PC1 (WEB88f459b8): paleoData_datum: NULL has been replaced by
‘anom’
- PC1 (WEB88f459b8): paleoData_notes: NULL has been replaced by ‘““We
suggest that PC1 reflects oscillations between two end member
depositional environments with fines indicative of deep lake conditions
and coarser material reflective of shallower lake conditions (i.e.,
littoral zone sediments)…onsistent with the grain-size lake-level model,
very fine to fine sand abundances increased during the middle Holocene
as δDwax increased and PC1 and lithic flux decreased, suggesting
diminished ISM rainfall reduced clastic (i.e., silt) deposition and
lowered lake level”’
- PC1 (WEB88f459b8): paleoData_proxyDetail: NULL has been replaced by
‘PCA’
- PC1 (WEB88f459b8): paleoData_proxyGeneral: NULL has been replaced by
‘hybrid’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2021-10-05 21:42:09 UTC
- changes:
- Publication metadata:
- pub1_author: ‘list(list(name = “Bird, Broxton W.”), list(name =
“Polisar, Pratigya J.”), list(name = “Lei, Yanbin”), list(name =
“Thompson, Lonnie G.”), list(name = “Yao, Tandong”), list(name =
“Finney, Bruce P.”), list(name = “Bain, Daniel J.”), list(name =
“Pompeani, David P.”), list(name = “Steinman, Byron A.”))’ has been
replaced by ‘Bird, Broxton W.’
- Paleo Interpretation metadata:
- Lithics (WEB1e2bd571): interpretation1_scope: NULL has been replaced
by ‘climate’
- Lithic Flux (WEB39ef1ed2): interpretation1_scope: NULL has been
replaced by ‘climate’
- Inferred BSi (WEB5b6c141d): interpretation1_scope: NULL has been
replaced by ‘climate’
- Dry Bulk Density (WEB99c4425f): interpretation1_scope: NULL has been
replaced by ‘climate’
- PC2 (WEBf1800d04): interpretation1_scope: NULL has been replaced by
‘climate’
- OM (WEBf6f06516): interpretation1_scope: NULL has been replaced by
‘climate’
Version: 1.0.0
- curator: nick
- timestamp: 2021-06-08 03:08:57 UTC
- notes: Added to lipdverse database.