Version history for mcaveMswFlyBnKzjKnYC - LS14FEZA
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2025-04-17 20:04:40.204191 UTC
- changes:
- Paleo Column metadata:
- uncertainty (LPD8ec8baf1): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- uncertainty (LPD9e7bf79e): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- uncertainty (LPD9e7bf79e2): paleoData_primaryAgeColumn: NULL has
been replaced by ‘FALSE’
- uncertainty (LPDd239c465): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- uncertainty (LPDd239c4652): paleoData_primaryAgeColumn: NULL has
been replaced by ‘FALSE’
- uncertainty (LPDd72fd146): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01A): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01A): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01B): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01B): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01C): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01C): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01D): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01D): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01E): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01E): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- d2H (LS14FEZA01F): paleoData_isPrimary: NULL has been replaced by
‘FALSE’
- d2H (LS14FEZA01F): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
- year (MAT0ee6aa23ee): paleoData_isPrimary: NULL has been replaced by
‘TRUE’
- year (MAT0ee6aa23ee): paleoData_primaryAgeColumn: NULL has been
replaced by ‘TRUE’
- depth (MATe175dfba95): paleoData_isPrimary: NULL has been replaced
by ‘FALSE’
- depth (MATe175dfba95): paleoData_primaryAgeColumn: NULL has been
replaced by ‘FALSE’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2025-04-11 16:26:58.563513 UTC
- changes:
- Paleo Interpretation metadata:
- uncertainty (LPD8ec8baf1): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD8ec8baf1): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD8ec8baf1): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD8ec8baf1): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD8ec8baf1): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD8ec8baf1): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD8ec8baf1): interpretation7_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e): interpretation7_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e2): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e2): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e2): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e2): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPD9e7bf79e2): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e2): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPD9e7bf79e2): interpretation7_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c465): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c465): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c465): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c465): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c465): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c465): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c465): interpretation7_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c4652): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c4652): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c4652): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c4652): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd239c4652): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c4652): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd239c4652): interpretation7_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd72fd146): interpretation1_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd72fd146): interpretation2_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd72fd146): interpretation3_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd72fd146): interpretation4_scope: NULL has been
replaced by ‘climate’
- uncertainty (LPDd72fd146): interpretation5_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd72fd146): interpretation6_scope: NULL has been
replaced by ‘isotope’
- uncertainty (LPDd72fd146): interpretation7_scope: NULL has been
replaced by ‘isotope’
- d2H (LS14FEZA01A): interpretation1_basis: ‘Downcore variation
involved subtle changes in distribution, C22 and C24 covarying and
suggesting a similar source, perhaps partially aquatic, with an increase
in recent decades perhaps related to indirect fertilization of the lake
(Fig. 5a).’ has been replaced by NULL
- d2H (LS14FEZA01A): interpretation1_inferredMaterial: ‘lake water and
soil water’ has been replaced by NULL
- d2H (LS14FEZA01A): interpretation1_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FEZA01A): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01A): interpretation1_variable: ‘deleteMe’ has been
replaced by NULL
- d2H (LS14FEZA01A): interpretation1_variableGroup: ‘Veg’ has been
replaced by NULL
- d2H (LS14FEZA01A): interpretation2_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01A): interpretation3_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01A): interpretation4_basis: NULL has been replaced by
‘Downcore variation involved subtle changes in distribution, C22 and C24
covarying and suggesting a similar source, perhaps partially aquatic,
with an increase in recent decades perhaps related to indirect
fertilization of the lake (Fig. 5a).’
- d2H (LS14FEZA01A): interpretation4_rank: NULL has been replaced by
‘1’
- d2H (LS14FEZA01A): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01A): interpretation4_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01A): interpretation4_variableGroup: NULL has been
replaced by ‘Veg’
- d2H (LS14FEZA01A): interpretation4_inferredMaterial: NULL has been
replaced by ‘lake water and soil water’
- d2H (LS14FEZA01A): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01A): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01B): interpretation1_basis: ‘Downcore variation
involved subtle changes in distribution, C22 and C24 covarying and
suggesting a similar source, perhaps partially aquatic, with an increase
in recent decades perhaps related to indirect fertilization of the lake
(Fig. 5a).’ has been replaced by NULL
- d2H (LS14FEZA01B): interpretation1_inferredMaterial: ‘lake water and
soil water’ has been replaced by NULL
- d2H (LS14FEZA01B): interpretation1_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FEZA01B): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01B): interpretation1_variable: ‘deleteMe’ has been
replaced by NULL
- d2H (LS14FEZA01B): interpretation1_variableGroup: ‘Veg’ has been
replaced by NULL
- d2H (LS14FEZA01B): interpretation2_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01B): interpretation3_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01B): interpretation4_basis: NULL has been replaced by
‘Downcore variation involved subtle changes in distribution, C22 and C24
covarying and suggesting a similar source, perhaps partially aquatic,
with an increase in recent decades perhaps related to indirect
fertilization of the lake (Fig. 5a).’
- d2H (LS14FEZA01B): interpretation4_rank: NULL has been replaced by
‘1’
- d2H (LS14FEZA01B): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01B): interpretation4_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01B): interpretation4_variableGroup: NULL has been
replaced by ‘Veg’
- d2H (LS14FEZA01B): interpretation4_inferredMaterial: NULL has been
replaced by ‘lake water and soil water’
- d2H (LS14FEZA01B): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01B): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01C): interpretation2_basis: ‘SEASONALITY: “First,
during water uptake, plants are expected to sample the spring growing
season precipitation, at the end of the wet season [October-March], as
the temperature warms up and before the dry summer months (Feakins and
Sessions, 2010; Kahmen et al., 2011; Tipple et al., 2013). During this
time, the plants may record the isotopic signature of just a few storms
each year heightening variability; however, sedimentary samples
integrating a decade might average the signal from > 20 storms.”
PARAMETER: “Paleoclimatic interpretation of the precipitation isotopic
history recorded in the Crystal Cave has been suggested to record
changes in moisture source primarily and local amount effect secondarily
(McCabe-Glynn et al., 2013). … Our record provides an extension of the
Crystal Cave isotopic record, from a more southerly coastal location,
but likely also records interdecadal variability in the same processes.
… We suggest that the plant leaf wax record preferentially captures
spring precipitation isotopic anomalies integrated over decades,
providing a sensitive record of atmospheric circulation and moisture
source changes.”’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14FEZA01C): interpretation2_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_integrationTimeBasis: ‘Rapid
transfer from plant to sediment is likely within the small, steep-sided
watershed, suggesting that the leaf wax record would be capable of
reconstructing up to decadal resolution variation in leaf wax dD
values.’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_integrationTimeUnits: ‘years’ has
been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FEZA01C): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01C): interpretation2_seasonality: ‘Spring’ has been
replaced by NULL
- d2H (LS14FEZA01C): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14FEZA01C): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation3_basis: ‘SEASONALITY: “First,
during water uptake, plants are expected to sample the spring growing
season precipitation, at the end of the wet season [October-March], as
the temperature warms up and before the dry summer months (Feakins and
Sessions, 2010; Kahmen et al., 2011; Tipple et al., 2013). During this
time, the plants may record the isotopic signature of just a few storms
each year heightening variability; however, sedimentary samples
integrating a decade might average the signal from > 20 storms.”
PARAMETER: “Paleoclimatic interpretation of the precipitation isotopic
history recorded in the Crystal Cave has been suggested to record
changes in moisture source primarily and local amount effect secondarily
(McCabe-Glynn et al., 2013). … Our record provides an extension of the
Crystal Cave isotopic record, from a more southerly coastal location,
but likely also records interdecadal variability in the same
processes.”’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation3_rank: ‘2’ has been replaced by
NULL
- d2H (LS14FEZA01C): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01C): interpretation3_seasonality: ‘Spring’ has been
replaced by NULL
- d2H (LS14FEZA01C): interpretation3_variable: ‘precipitation’ has
been replaced by NULL
- d2H (LS14FEZA01C): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d2H (LS14FEZA01C): interpretation3_variableGroupOriginal: ‘P_amount’
has been replaced by NULL
- d2H (LS14FEZA01C): interpretation4_basis: ‘Secondly, plant community
changes in the catchment (or other ecological changes) may influence the
dD record. Vegetation changes could reasonably have an influence on the
mean catchment ewax/precip that lasts for decades, so this mecha- nism
might operate too slowly to explain sample-to-sample vari- ability in
the sediment, although it may contribute to the multi- decadal
variability. We observed abundance variation in homo- logues downcore
(Fig. 5), which could be consistent with ecological changes influencing
dD values; however, the non-unique chain length distributions of
different plant species (Bush and McIner- ney, 2013) make it impossible
to draw unique solutions here.’ has been replaced by ‘SEASONALITY:
“First, during water uptake, plants are expected to sample the spring
growing season precipitation, at the end of the wet season
[October-March], as the temperature warms up and before the dry summer
months (Feakins and Sessions, 2010; Kahmen et al., 2011; Tipple et al.,
2013). During this time, the plants may record the isotopic signature of
just a few storms each year heightening variability; however,
sedimentary samples integrating a decade might average the signal from
> 20 storms.” PARAMETER: “Paleoclimatic interpretation of the
precipitation isotopic history recorded in the Crystal Cave has been
suggested to record changes in moisture source primarily and local
amount effect secondarily (McCabe-Glynn et al., 2013). … Our record
provides an extension of the Crystal Cave isotopic record, from a more
southerly coastal location, but likely also records interdecadal
variability in the same processes. … We suggest that the plant leaf wax
record preferentially captures spring precipitation isotopic anomalies
integrated over decades, providing a sensitive record of atmospheric
circulation and moisture source changes.”’
- d2H (LS14FEZA01C): interpretation4_rank: ‘3’ has been replaced by
‘1’
- d2H (LS14FEZA01C): interpretation4_variable: ‘deleteMe’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01C): interpretation4_variableGroup: ‘plant community
composition’ has been replaced by ‘P_isotope’
- d2H (LS14FEZA01C): interpretation4_direction: NULL has been replaced
by ‘positive’
- d2H (LS14FEZA01C): interpretation4_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14FEZA01C): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Rapid transfer from plant to sediment is likely within
the small, steep-sided watershed, suggesting that the leaf wax record
would be capable of reconstructing up to decadal resolution variation in
leaf wax dD values.’
- d2H (LS14FEZA01C): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘years’
- d2H (LS14FEZA01C): interpretation4_seasonality: NULL has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation4_variableGroupDirection: NULL has
been replaced by ‘positive’
- d2H (LS14FEZA01C): interpretation5_basis: NULL has been replaced by
‘SEASONALITY: “First, during water uptake, plants are expected to sample
the spring growing season precipitation, at the end of the wet season
[October-March], as the temperature warms up and before the dry summer
months (Feakins and Sessions, 2010; Kahmen et al., 2011; Tipple et al.,
2013). During this time, the plants may record the isotopic signature of
just a few storms each year heightening variability; however,
sedimentary samples integrating a decade might average the signal from
> 20 storms.” PARAMETER: “Paleoclimatic interpretation of the
precipitation isotopic history recorded in the Crystal Cave has been
suggested to record changes in moisture source primarily and local
amount effect secondarily (McCabe-Glynn et al., 2013). … Our record
provides an extension of the Crystal Cave isotopic record, from a more
southerly coastal location, but likely also records interdecadal
variability in the same processes.”’
- d2H (LS14FEZA01C): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14FEZA01C): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01C): interpretation5_seasonality: NULL has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation5_variable: NULL has been replaced
by ‘precipitation’
- d2H (LS14FEZA01C): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14FEZA01C): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14FEZA01C): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘P_amount’
- d2H (LS14FEZA01C): interpretation6_basis: NULL has been replaced by
‘Secondly, plant community changes in the catchment (or other ecological
changes) may influence the dD record. Vegetation changes could
reasonably have an influence on the mean catchment ewax/precip that
lasts for decades, so this mecha- nism might operate too slowly to
explain sample-to-sample vari- ability in the sediment, although it may
contribute to the multi- decadal variability. We observed abundance
variation in homo- logues downcore (Fig. 5), which could be consistent
with ecological changes influencing dD values; however, the non-unique
chain length distributions of different plant species (Bush and McIner-
ney, 2013) make it impossible to draw unique solutions here.’
- d2H (LS14FEZA01C): interpretation6_rank: NULL has been replaced by
‘3’
- d2H (LS14FEZA01C): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01C): interpretation6_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01C): interpretation6_variableGroup: NULL has been
replaced by ‘plant community composition’
- d2H (LS14FEZA01D): interpretation2_basis: ‘SEASONALITY: “First,
during water uptake, plants are expected to sample the spring growing
season precipitation, at the end of the wet season [October-March], as
the temperature warms up and before the dry summer months (Feakins and
Sessions, 2010; Kahmen et al., 2011; Tipple et al., 2013). During this
time, the plants may record the isotopic signature of just a few storms
each year heightening variability; however, sedimentary samples
integrating a decade might average the signal from > 20 storms.”
PARAMETER: “Paleoclimatic interpretation of the precipitation isotopic
history recorded in the Crystal Cave has been suggested to record
changes in moisture source primarily and local amount effect secondarily
(McCabe-Glynn et al., 2013). … Our record provides an extension of the
Crystal Cave isotopic record, from a more southerly coastal location,
but likely also records interdecadal variability in the same processes.
… We suggest that the plant leaf wax record preferentially captures
spring precipitation isotopic anomalies integrated over decades,
providing a sensitive record of atmospheric circulation and moisture
source changes.”’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_direction: ‘positive’ has been
replaced by NULL
- d2H (LS14FEZA01D): interpretation2_inferredMaterial: ‘soil water’
has been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_integrationTimeBasis: ‘Rapid
transfer from plant to sediment is likely within the small, steep-sided
watershed, suggesting that the leaf wax record would be capable of
reconstructing up to decadal resolution variation in leaf wax dD
values.’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_integrationTimeUnits: ‘years’ has
been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_rank: ‘1’ has been replaced by
NULL
- d2H (LS14FEZA01D): interpretation2_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01D): interpretation2_seasonality: ‘Oct-Mar’ has been
replaced by NULL
- d2H (LS14FEZA01D): interpretation2_variable: ‘precipitationIsotope’
has been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_variableGroup: ‘P_isotope’ has
been replaced by NULL
- d2H (LS14FEZA01D): interpretation2_variableGroupDirection:
‘positive’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation3_basis: ‘SEASONALITY: “First,
during water uptake, plants are expected to sample the spring growing
season precipitation, at the end of the wet season [October-March], as
the temperature warms up and before the dry summer months (Feakins and
Sessions, 2010; Kahmen et al., 2011; Tipple et al., 2013). During this
time, the plants may record the isotopic signature of just a few storms
each year heightening variability; however, sedimentary samples
integrating a decade might average the signal from > 20 storms.”
PARAMETER: “Paleoclimatic interpretation of the precipitation isotopic
history recorded in the Crystal Cave has been suggested to record
changes in moisture source primarily and local amount effect secondarily
(McCabe-Glynn et al., 2013). … Our record provides an extension of the
Crystal Cave isotopic record, from a more southerly coastal location,
but likely also records interdecadal variability in the same
processes.”’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation3_rank: ‘2’ has been replaced by
NULL
- d2H (LS14FEZA01D): interpretation3_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01D): interpretation3_seasonality: ‘Spring’ has been
replaced by NULL
- d2H (LS14FEZA01D): interpretation3_variable: ‘precipitation’ has
been replaced by NULL
- d2H (LS14FEZA01D): interpretation3_variableGroup:
‘EffectiveMoisture’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation3_variableGroupDirection:
‘negative’ has been replaced by NULL
- d2H (LS14FEZA01D): interpretation3_variableGroupOriginal: ‘P_amount’
has been replaced by NULL
- d2H (LS14FEZA01D): interpretation4_basis: ‘Secondly, plant community
changes in the catchment (or other ecological changes) may influence the
dD record. Vegetation changes could reasonably have an influence on the
mean catchment ewax/precip that lasts for decades, so this mecha- nism
might operate too slowly to explain sample-to-sample vari- ability in
the sediment, although it may contribute to the multi- decadal
variability. We observed abundance variation in homo- logues downcore
(Fig. 5), which could be consistent with ecological changes influencing
dD values; however, the non-unique chain length distributions of
different plant species (Bush and McIner- ney, 2013) make it impossible
to draw unique solutions here.’ has been replaced by ‘SEASONALITY:
“First, during water uptake, plants are expected to sample the spring
growing season precipitation, at the end of the wet season
[October-March], as the temperature warms up and before the dry summer
months (Feakins and Sessions, 2010; Kahmen et al., 2011; Tipple et al.,
2013). During this time, the plants may record the isotopic signature of
just a few storms each year heightening variability; however,
sedimentary samples integrating a decade might average the signal from
> 20 storms.” PARAMETER: “Paleoclimatic interpretation of the
precipitation isotopic history recorded in the Crystal Cave has been
suggested to record changes in moisture source primarily and local
amount effect secondarily (McCabe-Glynn et al., 2013). … Our record
provides an extension of the Crystal Cave isotopic record, from a more
southerly coastal location, but likely also records interdecadal
variability in the same processes. … We suggest that the plant leaf wax
record preferentially captures spring precipitation isotopic anomalies
integrated over decades, providing a sensitive record of atmospheric
circulation and moisture source changes.”’
- d2H (LS14FEZA01D): interpretation4_rank: ‘3’ has been replaced by
‘1’
- d2H (LS14FEZA01D): interpretation4_variable: ‘deleteMe’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01D): interpretation4_variableGroup: ‘plant community
composition’ has been replaced by ‘P_isotope’
- d2H (LS14FEZA01D): interpretation4_direction: NULL has been replaced
by ‘positive’
- d2H (LS14FEZA01D): interpretation4_inferredMaterial: NULL has been
replaced by ‘soil water’
- d2H (LS14FEZA01D): interpretation4_integrationTimeBasis: NULL has
been replaced by ‘Rapid transfer from plant to sediment is likely within
the small, steep-sided watershed, suggesting that the leaf wax record
would be capable of reconstructing up to decadal resolution variation in
leaf wax dD values.’
- d2H (LS14FEZA01D): interpretation4_integrationTimeUnits: NULL has
been replaced by ‘years’
- d2H (LS14FEZA01D): interpretation4_seasonality: NULL has been
replaced by ‘Oct-Mar’
- d2H (LS14FEZA01D): interpretation4_variableGroupDirection: NULL has
been replaced by ‘positive’
- d2H (LS14FEZA01D): interpretation5_basis: NULL has been replaced by
‘SEASONALITY: “First, during water uptake, plants are expected to sample
the spring growing season precipitation, at the end of the wet season
[October-March], as the temperature warms up and before the dry summer
months (Feakins and Sessions, 2010; Kahmen et al., 2011; Tipple et al.,
2013). During this time, the plants may record the isotopic signature of
just a few storms each year heightening variability; however,
sedimentary samples integrating a decade might average the signal from
> 20 storms.” PARAMETER: “Paleoclimatic interpretation of the
precipitation isotopic history recorded in the Crystal Cave has been
suggested to record changes in moisture source primarily and local
amount effect secondarily (McCabe-Glynn et al., 2013). … Our record
provides an extension of the Crystal Cave isotopic record, from a more
southerly coastal location, but likely also records interdecadal
variability in the same processes.”’
- d2H (LS14FEZA01D): interpretation5_rank: NULL has been replaced by
‘2’
- d2H (LS14FEZA01D): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01D): interpretation5_seasonality: NULL has been
replaced by ‘Spring’
- d2H (LS14FEZA01D): interpretation5_variable: NULL has been replaced
by ‘precipitation’
- d2H (LS14FEZA01D): interpretation5_variableGroup: NULL has been
replaced by ‘EffectiveMoisture’
- d2H (LS14FEZA01D): interpretation5_variableGroupDirection: NULL has
been replaced by ‘negative’
- d2H (LS14FEZA01D): interpretation5_variableGroupOriginal: NULL has
been replaced by ‘P_amount’
- d2H (LS14FEZA01D): interpretation6_basis: NULL has been replaced by
‘Secondly, plant community changes in the catchment (or other ecological
changes) may influence the dD record. Vegetation changes could
reasonably have an influence on the mean catchment ewax/precip that
lasts for decades, so this mecha- nism might operate too slowly to
explain sample-to-sample vari- ability in the sediment, although it may
contribute to the multi- decadal variability. We observed abundance
variation in homo- logues downcore (Fig. 5), which could be consistent
with ecological changes influencing dD values; however, the non-unique
chain length distributions of different plant species (Bush and McIner-
ney, 2013) make it impossible to draw unique solutions here.’
- d2H (LS14FEZA01D): interpretation6_rank: NULL has been replaced by
‘3’
- d2H (LS14FEZA01D): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01D): interpretation6_variable: NULL has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01D): interpretation6_variableGroup: NULL has been
replaced by ‘plant community composition’
- d2H (LS14FEZA01E): interpretation1_inferredMaterial: ‘not
interpreted’ has been replaced by NULL
- d2H (LS14FEZA01E): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01E): interpretation2_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01E): interpretation3_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01E): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01E): interpretation4_inferredMaterial: NULL has been
replaced by ‘not interpreted’
- d2H (LS14FEZA01E): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01E): interpretation6_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01F): interpretation1_inferredMaterial: ‘not
interpreted’ has been replaced by NULL
- d2H (LS14FEZA01F): interpretation1_scope: ‘isotope’ has been
replaced by ‘climate’
- d2H (LS14FEZA01F): interpretation2_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01F): interpretation3_scope: NULL has been replaced by
‘climate’
- d2H (LS14FEZA01F): interpretation4_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01F): interpretation4_inferredMaterial: NULL has been
replaced by ‘not interpreted’
- d2H (LS14FEZA01F): interpretation5_scope: NULL has been replaced by
‘isotope’
- d2H (LS14FEZA01F): interpretation6_scope: NULL has been replaced by
‘isotope’
- year (MAT0ee6aa23ee): interpretation1_scope: NULL has been replaced
by ‘climate’
- year (MAT0ee6aa23ee): interpretation2_scope: NULL has been replaced
by ‘climate’
- year (MAT0ee6aa23ee): interpretation3_scope: NULL has been replaced
by ‘climate’
- year (MAT0ee6aa23ee): interpretation4_scope: NULL has been replaced
by ‘climate’
- depth (MATe175dfba95): interpretation1_scope: NULL has been replaced
by ‘climate’
- depth (MATe175dfba95): interpretation2_scope: NULL has been replaced
by ‘climate’
- depth (MATe175dfba95): interpretation3_scope: NULL has been replaced
by ‘climate’
- depth (MATe175dfba95): interpretation4_scope: NULL has been replaced
by ‘climate’
Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2025-04-09 20:48:16.940466 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Paleo Interpretation metadata:
- d2H (LS14FEZA01A): interpretation1_variable: ‘Veg’ has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01B): interpretation1_variable: ‘Veg’ has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01C): interpretation1_variable: ‘Moisture flux from the
subtropical North Pacific (driven by SST anomalies in the Kuroshio
Extension region)’ has been replaced by ‘circulationVariable’
- d2H (LS14FEZA01C): interpretation2_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01C): interpretation3_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation3_variable: ‘P_amount’ has been
replaced by ‘precipitation’
- d2H (LS14FEZA01C): interpretation4_variable: ‘plant community
composition’ has been replaced by ‘deleteMe’
- d2H (LS14FEZA01D): interpretation1_variable: ‘Moisture flux from the
subtropical North Pacific (driven by SST anomalies in the Kuroshio
Extension region)’ has been replaced by ‘circulationVariable’
- d2H (LS14FEZA01D): interpretation2_seasonality: ‘ONDJFM’ has been
replaced by ‘Oct-Mar’
- d2H (LS14FEZA01D): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01D): interpretation3_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01D): interpretation3_variable: ‘P_amount’ has been
replaced by ‘precipitation’
- d2H (LS14FEZA01D): interpretation4_variable: ‘plant community
composition’ has been replaced by ‘deleteMe’
Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2025-04-09 18:35:13.113156 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Interpretation metadata:
- d2H (LS14FEZA01A): interpretation1_variable: ‘Veg’ has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01B): interpretation1_variable: ‘Veg’ has been replaced
by ‘deleteMe’
- d2H (LS14FEZA01C): interpretation1_variable: ‘Moisture flux from the
subtropical North Pacific (driven by SST anomalies in the Kuroshio
Extension region)’ has been replaced by ‘circulationVariable’
- d2H (LS14FEZA01C): interpretation2_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01C): interpretation3_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01C): interpretation3_variable: ‘P_amount’ has been
replaced by ‘precipitation’
- d2H (LS14FEZA01C): interpretation4_variable: ‘plant community
composition’ has been replaced by ‘deleteMe’
- d2H (LS14FEZA01D): interpretation1_variable: ‘Moisture flux from the
subtropical North Pacific (driven by SST anomalies in the Kuroshio
Extension region)’ has been replaced by ‘circulationVariable’
- d2H (LS14FEZA01D): interpretation2_seasonality: ‘ONDJFM’ has been
replaced by ‘Oct-Mar’
- d2H (LS14FEZA01D): interpretation2_variable: ‘P_isotope’ has been
replaced by ‘precipitationIsotope’
- d2H (LS14FEZA01D): interpretation3_seasonality: ‘spring’ has been
replaced by ‘Spring’
- d2H (LS14FEZA01D): interpretation3_variable: ‘P_amount’ has been
replaced by ‘precipitation’
- d2H (LS14FEZA01D): interpretation4_variable: ‘plant community
composition’ has been replaced by ‘deleteMe’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2025-04-08 17:32:59.224375 UTC
- notes: Changes made as part of LiPDverse vocabulary
standardization process
- changes:
- Paleo Column metadata:
- uncertainty (LPD8ec8baf1): paleoData_measurementMaterial: NULL has
been replaced by ‘d2H’
- uncertainty (LPD8ec8baf1): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPD8ec8baf1): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPD8ec8baf1): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- uncertainty (LPD9e7bf79e): paleoData_measurementMaterial:
‘n-alkanoic acid’ has been replaced by ‘d2H’
- uncertainty (LPD9e7bf79e): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPD9e7bf79e): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPD9e7bf79e): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- uncertainty (LPD9e7bf79e2): paleoData_measurementMaterial:
‘n-alkanoic acid’ has been replaced by ‘d2H’
- uncertainty (LPD9e7bf79e2): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPD9e7bf79e2): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPD9e7bf79e2): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- uncertainty (LPDd239c465): paleoData_measurementMaterial:
‘n-alkanoic acid’ has been replaced by ‘d2H’
- uncertainty (LPDd239c465): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPDd239c465): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPDd239c465): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- uncertainty (LPDd239c4652): paleoData_measurementMaterial:
‘n-alkanoic acid’ has been replaced by ‘d2H’
- uncertainty (LPDd239c4652): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPDd239c4652): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPDd239c4652): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- uncertainty (LPDd72fd146): paleoData_measurementMaterial:
‘n-alkanoic acid’ has been replaced by ‘d2H’
- uncertainty (LPDd72fd146): paleoData_variableName: ‘dDUncertainty’
has been replaced by ‘uncertainty’
- uncertainty (LPDd72fd146): paleoData_isPrimary: NULL has been
replaced by ‘FALSE’
- uncertainty (LPDd72fd146): paleoData_longName: NULL has been
replaced by ‘dDUncertainty’
- d2H (LS14FEZA01A): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- d2H (LS14FEZA01B): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- d2H (LS14FEZA01C): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- d2H (LS14FEZA01D): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- d2H (LS14FEZA01E): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- d2H (LS14FEZA01F): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- year (MAT0ee6aa23ee): paleoData_units: ‘AD’ has been replaced by ‘yr
AD’
- year (MAT0ee6aa23ee): paleoData_longName: NULL has been replaced by
‘dDUncertainty’
- depth (MATe175dfba95): paleoData_longName: NULL has been replaced by
‘dDUncertainty’