uncertainty (LPD8ec8baf1): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPD8ec8baf1): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPD8ec8baf1): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPD8ec8baf1): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPD8ec8baf1): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPD8ec8baf1): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPD8ec8baf1): interpretation7_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e): interpretation7_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e2): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e2): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e2): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e2): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPD9e7bf79e2): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e2): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPD9e7bf79e2): interpretation7_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c465): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c465): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c465): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c465): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c465): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c465): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c465): interpretation7_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c4652): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c4652): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c4652): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c4652): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPDd239c4652): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c4652): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPDd239c4652): interpretation7_scope: '' has been replaced by 'isotope'
uncertainty (LPDd72fd146): interpretation1_scope: '' has been replaced by 'climate'
uncertainty (LPDd72fd146): interpretation2_scope: '' has been replaced by 'climate'
uncertainty (LPDd72fd146): interpretation3_scope: '' has been replaced by 'climate'
uncertainty (LPDd72fd146): interpretation4_scope: '' has been replaced by 'climate'
uncertainty (LPDd72fd146): interpretation5_scope: '' has been replaced by 'isotope'
uncertainty (LPDd72fd146): interpretation6_scope: '' has been replaced by 'isotope'
uncertainty (LPDd72fd146): interpretation7_scope: '' 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 ''
d2H (LS14FEZA01A): interpretation1_inferredMaterial: 'lake water and soil water' has been replaced by ''
d2H (LS14FEZA01A): interpretation1_rank: '1' has been replaced by ''
d2H (LS14FEZA01A): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01A): interpretation1_variable: 'deleteMe' has been replaced by ''
d2H (LS14FEZA01A): interpretation1_variableGroup: 'Veg' has been replaced by ''
d2H (LS14FEZA01A): interpretation2_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01A): interpretation3_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01A): interpretation4_basis: '' 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: '' has been replaced by '1'
d2H (LS14FEZA01A): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01A): interpretation4_variable: '' has been replaced by 'deleteMe'
d2H (LS14FEZA01A): interpretation4_variableGroup: '' has been replaced by 'Veg'
d2H (LS14FEZA01A): interpretation4_inferredMaterial: '' has been replaced by 'lake water and soil water'
d2H (LS14FEZA01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01A): interpretation6_scope: '' 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 ''
d2H (LS14FEZA01B): interpretation1_inferredMaterial: 'lake water and soil water' has been replaced by ''
d2H (LS14FEZA01B): interpretation1_rank: '1' has been replaced by ''
d2H (LS14FEZA01B): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01B): interpretation1_variable: 'deleteMe' has been replaced by ''
d2H (LS14FEZA01B): interpretation1_variableGroup: 'Veg' has been replaced by ''
d2H (LS14FEZA01B): interpretation2_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01B): interpretation3_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01B): interpretation4_basis: '' 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: '' has been replaced by '1'
d2H (LS14FEZA01B): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01B): interpretation4_variable: '' has been replaced by 'deleteMe'
d2H (LS14FEZA01B): interpretation4_variableGroup: '' has been replaced by 'Veg'
d2H (LS14FEZA01B): interpretation4_inferredMaterial: '' has been replaced by 'lake water and soil water'
d2H (LS14FEZA01B): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01B): interpretation6_scope: '' 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 ''
d2H (LS14FEZA01C): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
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 ''
d2H (LS14FEZA01C): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_rank: '1' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01C): interpretation2_seasonality: 'Spring' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14FEZA01C): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
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 ''
d2H (LS14FEZA01C): interpretation3_rank: '2' has been replaced by ''
d2H (LS14FEZA01C): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01C): interpretation3_seasonality: 'Spring' has been replaced by ''
d2H (LS14FEZA01C): interpretation3_variable: 'precipitation' has been replaced by ''
d2H (LS14FEZA01C): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS14FEZA01C): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS14FEZA01C): interpretation3_variableGroupOriginal: 'P_amount' has been replaced by ''
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: '' has been replaced by 'positive'
d2H (LS14FEZA01C): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14FEZA01C): interpretation4_integrationTimeBasis: '' 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: '' has been replaced by 'years'
d2H (LS14FEZA01C): interpretation4_seasonality: '' has been replaced by 'Spring'
d2H (LS14FEZA01C): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS14FEZA01C): interpretation5_basis: '' 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: '' has been replaced by '2'
d2H (LS14FEZA01C): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01C): interpretation5_seasonality: '' has been replaced by 'Spring'
d2H (LS14FEZA01C): interpretation5_variable: '' has been replaced by 'precipitation'
d2H (LS14FEZA01C): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14FEZA01C): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14FEZA01C): interpretation5_variableGroupOriginal: '' has been replaced by 'P_amount'
d2H (LS14FEZA01C): interpretation6_basis: '' 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: '' has been replaced by '3'
d2H (LS14FEZA01C): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01C): interpretation6_variable: '' has been replaced by 'deleteMe'
d2H (LS14FEZA01C): interpretation6_variableGroup: '' 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 ''
d2H (LS14FEZA01D): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
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 ''
d2H (LS14FEZA01D): interpretation2_integrationTimeUnits: 'years' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_rank: '1' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01D): interpretation2_seasonality: 'Oct-Mar' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS14FEZA01D): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
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 ''
d2H (LS14FEZA01D): interpretation3_rank: '2' has been replaced by ''
d2H (LS14FEZA01D): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01D): interpretation3_seasonality: 'Spring' has been replaced by ''
d2H (LS14FEZA01D): interpretation3_variable: 'precipitation' has been replaced by ''
d2H (LS14FEZA01D): interpretation3_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS14FEZA01D): interpretation3_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS14FEZA01D): interpretation3_variableGroupOriginal: 'P_amount' has been replaced by ''
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: '' has been replaced by 'positive'
d2H (LS14FEZA01D): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS14FEZA01D): interpretation4_integrationTimeBasis: '' 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: '' has been replaced by 'years'
d2H (LS14FEZA01D): interpretation4_seasonality: '' has been replaced by 'Oct-Mar'
d2H (LS14FEZA01D): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS14FEZA01D): interpretation5_basis: '' 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: '' has been replaced by '2'
d2H (LS14FEZA01D): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01D): interpretation5_seasonality: '' has been replaced by 'Spring'
d2H (LS14FEZA01D): interpretation5_variable: '' has been replaced by 'precipitation'
d2H (LS14FEZA01D): interpretation5_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS14FEZA01D): interpretation5_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS14FEZA01D): interpretation5_variableGroupOriginal: '' has been replaced by 'P_amount'
d2H (LS14FEZA01D): interpretation6_basis: '' 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: '' has been replaced by '3'
d2H (LS14FEZA01D): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01D): interpretation6_variable: '' has been replaced by 'deleteMe'
d2H (LS14FEZA01D): interpretation6_variableGroup: '' has been replaced by 'plant community composition'
d2H (LS14FEZA01E): interpretation1_inferredMaterial: 'not interpreted' has been replaced by ''
d2H (LS14FEZA01E): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01E): interpretation2_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01E): interpretation3_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01E): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01E): interpretation4_inferredMaterial: '' has been replaced by 'not interpreted'
d2H (LS14FEZA01E): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01E): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01F): interpretation1_inferredMaterial: 'not interpreted' has been replaced by ''
d2H (LS14FEZA01F): interpretation1_scope: 'isotope' has been replaced by 'climate'
d2H (LS14FEZA01F): interpretation2_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01F): interpretation3_scope: '' has been replaced by 'climate'
d2H (LS14FEZA01F): interpretation4_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01F): interpretation4_inferredMaterial: '' has been replaced by 'not interpreted'
d2H (LS14FEZA01F): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS14FEZA01F): interpretation6_scope: '' has been replaced by 'isotope'
year (MAT0ee6aa23ee): interpretation1_scope: '' has been replaced by 'climate'
year (MAT0ee6aa23ee): interpretation2_scope: '' has been replaced by 'climate'
year (MAT0ee6aa23ee): interpretation3_scope: '' has been replaced by 'climate'
year (MAT0ee6aa23ee): interpretation4_scope: '' has been replaced by 'climate'
depth (MATe175dfba95): interpretation1_scope: '' has been replaced by 'climate'
depth (MATe175dfba95): interpretation2_scope: '' has been replaced by 'climate'
depth (MATe175dfba95): interpretation3_scope: '' has been replaced by 'climate'
depth (MATe175dfba95): interpretation4_scope: '' has been replaced by 'climate'