depth (LPD28794972): interpretation1_scope: '' has been replaced by 'climate'
depth (LPD28794972): interpretation2_scope: '' has been replaced by 'climate'
year (LPDcb260002): interpretation1_scope: '' has been replaced by 'climate'
year (LPDcb260002): interpretation2_scope: '' has been replaced by 'climate'
d2H (LS09RUWA01A): interpretation2_basis: 'The ?D of long-chain, terrestrially derived fatty acids is controlled by the ?D of the water used by plants, transpiration from leaf surfaces, and kinetic fractionation during biosynthesis (Hou et al., 2008; Sessions et al., 1999).  ... "Thus, although the first-order control on leaf wax ?D in the tropics is the ?D of meteoric waters, interactions between climate and vegetation suggest the potential for complex, non-linear responses of leaf wax ?D to rainfall variability."' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_direction: 'positive' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_inferredMaterial: 'soil water' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_mathematicalRelation: 'linear' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_rank: '1' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01A): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_variable: 'precipitationIsotope' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_variableGroup: 'P_isotope' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_variableGroupDirection: 'positive' has been replaced by ''
d2H (LS09RUWA01A): interpretation2_variableGroupOriginal: 'P_isotope & Veg' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_basis: 'If changes in vegetation surrounding Lake Wandakara were mainly driven by rainfall, ?13CC30 and ?DC30 should also be positively correlated: during intervals of drought shifts toward C4 ecosystems would occur, recorded by enriched ?DC30 values. However, ?13CC30 and ?DC30 are clearly negatively correlated (Fig. 5). In fact, large positive shifts in ?13CC30 are associated with depleted ?DC30 values, and peak ?13CC30 from AD 1200 to 1440 occurs during an interval of regionally wet climate conditions (Russell et al., 2007, Russell and Johnson, 2007). This suggests that the abrupt shifts toward C4 vegetation were not caused by climate but instead by human activities on the landscape, presumably forest clearance for agriculture (Ssemmanda et al., 2005).' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_mathematicalRelation: 'nonlinear' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_rank: '2' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01A): interpretation3_seasonality: 'Annual' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_variable: 'deleteMe' has been replaced by ''
d2H (LS09RUWA01A): interpretation3_variableGroup: 'Human-induced changes in vegetation type' has been replaced by ''
d2H (LS09RUWA01A): interpretation4_rank: '' has been replaced by '1'
d2H (LS09RUWA01A): interpretation4_basis: '' has been replaced by 'The ?D of long-chain, terrestrially derived fatty acids is controlled by the ?D of the water used by plants, transpiration from leaf surfaces, and kinetic fractionation during biosynthesis (Hou et al., 2008; Sessions et al., 1999).  ... "Thus, although the first-order control on leaf wax ?D in the tropics is the ?D of meteoric waters, interactions between climate and vegetation suggest the potential for complex, non-linear responses of leaf wax ?D to rainfall variability."'
d2H (LS09RUWA01A): interpretation4_direction: '' has been replaced by 'positive'
d2H (LS09RUWA01A): interpretation4_inferredMaterial: '' has been replaced by 'soil water'
d2H (LS09RUWA01A): interpretation4_mathematicalRelation: '' has been replaced by 'linear'
d2H (LS09RUWA01A): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS09RUWA01A): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09RUWA01A): interpretation4_variable: '' has been replaced by 'precipitationIsotope'
d2H (LS09RUWA01A): interpretation4_variableGroup: '' has been replaced by 'P_isotope'
d2H (LS09RUWA01A): interpretation4_variableGroupDirection: '' has been replaced by 'positive'
d2H (LS09RUWA01A): interpretation4_variableGroupOriginal: '' has been replaced by 'P_isotope & Veg'
d2H (LS09RUWA01A): interpretation5_basis: '' has been replaced by 'If changes in vegetation surrounding Lake Wandakara were mainly driven by rainfall, ?13CC30 and ?DC30 should also be positively correlated: during intervals of drought shifts toward C4 ecosystems would occur, recorded by enriched ?DC30 values. However, ?13CC30 and ?DC30 are clearly negatively correlated (Fig. 5). In fact, large positive shifts in ?13CC30 are associated with depleted ?DC30 values, and peak ?13CC30 from AD 1200 to 1440 occurs during an interval of regionally wet climate conditions (Russell et al., 2007, Russell and Johnson, 2007). This suggests that the abrupt shifts toward C4 vegetation were not caused by climate but instead by human activities on the landscape, presumably forest clearance for agriculture (Ssemmanda et al., 2005).'
d2H (LS09RUWA01A): interpretation5_mathematicalRelation: '' has been replaced by 'nonlinear'
d2H (LS09RUWA01A): interpretation5_rank: '' has been replaced by '2'
d2H (LS09RUWA01A): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS09RUWA01A): interpretation5_seasonality: '' has been replaced by 'Annual'
d2H (LS09RUWA01A): interpretation5_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09RUWA01A): interpretation5_variable: '' has been replaced by 'deleteMe'
d2H (LS09RUWA01A): interpretation5_variableGroup: '' has been replaced by 'Human-induced changes in vegetation type'
d2H (LS09RUWA01A): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS09RUWA01B): interpretation2_basis: 'Short-chain (C16?C18) fatty acids in lake sediments are derived primarily from aquatic sources (Eglinton and Hamilton, 1967; Huang et al., 2002), and the principal control on their ?D is the ?D of lake water (Huang et al., 2002, 2004). ... "The ?D of closed-basin tropical lakes such as Wandakara reflects the hydrologic balance of the lake, with drier conditions causing isotopically enriched lake water due to both the amount effect on precipitation and kinetic fractionation during evaporation from the lake surface, which favors the retention of deuterium relative to hydrogen in the lake water (Craig, 1961). "' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_direction: 'negative' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_rank: '1' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01B): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_variable: 'hydrologicBalance' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS09RUWA01B): interpretation2_variableGroupOriginal: 'I_E' has been replaced by ''
d2H (LS09RUWA01B): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01B): interpretation4_rank: '' has been replaced by '1'
d2H (LS09RUWA01B): interpretation4_basis: '' has been replaced by 'Short-chain (C16?C18) fatty acids in lake sediments are derived primarily from aquatic sources (Eglinton and Hamilton, 1967; Huang et al., 2002), and the principal control on their ?D is the ?D of lake water (Huang et al., 2002, 2004). ... "The ?D of closed-basin tropical lakes such as Wandakara reflects the hydrologic balance of the lake, with drier conditions causing isotopically enriched lake water due to both the amount effect on precipitation and kinetic fractionation during evaporation from the lake surface, which favors the retention of deuterium relative to hydrogen in the lake water (Craig, 1961). "'
d2H (LS09RUWA01B): interpretation4_direction: '' has been replaced by 'negative'
d2H (LS09RUWA01B): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS09RUWA01B): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS09RUWA01B): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09RUWA01B): interpretation4_variable: '' has been replaced by 'hydrologicBalance'
d2H (LS09RUWA01B): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS09RUWA01B): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS09RUWA01B): interpretation4_variableGroupOriginal: '' has been replaced by 'I_E'
d2H (LS09RUWA01B): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS09RUWA01B): interpretation6_scope: '' has been replaced by 'isotope'
d2H (LS09RUWA01B2): interpretation2_basis: 'Short-chain (C16?C18) fatty acids in lake sediments are derived primarily from aquatic sources (Eglinton and Hamilton, 1967; Huang et al., 2002), and the principal control on their ?D is the ?D of lake water (Huang et al., 2002, 2004). ... "The ?D of closed-basin tropical lakes such as Wandakara reflects the hydrologic balance of the lake, with drier conditions causing isotopically enriched lake water due to both the amount effect on precipitation and kinetic fractionation during evaporation from the lake surface, which favors the retention of deuterium relative to hydrogen in the lake water (Craig, 1961). "' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_direction: 'negative' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_inferredMaterial: 'lake water' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_rank: '1' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01B2): interpretation2_seasonality: 'Annual' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_seasonalityOriginal: 'Annual' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_variable: 'hydrologicBalance' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_variableGroup: 'EffectiveMoisture' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_variableGroupDirection: 'negative' has been replaced by ''
d2H (LS09RUWA01B2): interpretation2_variableGroupOriginal: 'I_E' has been replaced by ''
d2H (LS09RUWA01B2): interpretation3_scope: 'isotope' has been replaced by 'climate'
d2H (LS09RUWA01B2): interpretation4_rank: '' has been replaced by '1'
d2H (LS09RUWA01B2): interpretation4_basis: '' has been replaced by 'Short-chain (C16?C18) fatty acids in lake sediments are derived primarily from aquatic sources (Eglinton and Hamilton, 1967; Huang et al., 2002), and the principal control on their ?D is the ?D of lake water (Huang et al., 2002, 2004). ... "The ?D of closed-basin tropical lakes such as Wandakara reflects the hydrologic balance of the lake, with drier conditions causing isotopically enriched lake water due to both the amount effect on precipitation and kinetic fractionation during evaporation from the lake surface, which favors the retention of deuterium relative to hydrogen in the lake water (Craig, 1961). "'
d2H (LS09RUWA01B2): interpretation4_direction: '' has been replaced by 'negative'
d2H (LS09RUWA01B2): interpretation4_inferredMaterial: '' has been replaced by 'lake water'
d2H (LS09RUWA01B2): interpretation4_seasonality: '' has been replaced by 'Annual'
d2H (LS09RUWA01B2): interpretation4_seasonalityOriginal: '' has been replaced by 'Annual'
d2H (LS09RUWA01B2): interpretation4_variable: '' has been replaced by 'hydrologicBalance'
d2H (LS09RUWA01B2): interpretation4_variableGroup: '' has been replaced by 'EffectiveMoisture'
d2H (LS09RUWA01B2): interpretation4_variableGroupDirection: '' has been replaced by 'negative'
d2H (LS09RUWA01B2): interpretation4_variableGroupOriginal: '' has been replaced by 'I_E'
d2H (LS09RUWA01B2): interpretation5_scope: '' has been replaced by 'isotope'
d2H (LS09RUWA01B2): interpretation6_scope: '' has been replaced by 'isotope'