Version history for XMiz8wKPdQIwOWRZzJ2x - Villarscave.D.Genty.
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nick
- timestamp: 2021-01-12 02:29:55 UTC
- changes:
- Paleo Interpretation metadata:
- d18OPrecision (S2LR1rddStBR04): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR1rMgFn0lwh): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LR1TxJYnRTjV): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR27gTENlWBq): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LR4AXa4FnbDR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LR7fTxW5FmMs): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LR99BnSfrkQS): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LR9CMNgIa4y5): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LR9FLJjpdEeB): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OPrecision (S2LRaGzG2MeA6s): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRB4YMb8nJX9): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRbLMBtRSW52): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRbmzZ3oPLaR): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRbPD6RH65SZ): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogy (S2LRbPjqKrwVos): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRc2GmyUEf4a): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRccepFxWpY4): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRCmm1Rr0lYR): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecisionComposite (S2LReHQeI9HS39): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRFH8LMNJV7S): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRfK83QKfYkk): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandard (S2LRfNe6NWgn58): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRFTcMfpMSCi): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRGaaHsNnVk6): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRgobWyMcQra): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRGRAA0NyB6K): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRgtIAJMgQKm): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRguf0WlEbDS): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRHT4rT6IgGG): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRicR32s8P0D): interpretation1_scope: NULL has been replaced
by ‘climate’
- d13C (S2LRIoL0ftB6A9): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRIsPbkUP2Ft): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRiUzGJvSXxn): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRj04IREggbx): interpretation1_scope: NULL has been
replaced by ‘climate’
- entityName (S2LRjAIwIoI0YY): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRjpo9oX7HID): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRJzZ65XC2P1): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRk6ihlvDZaR): interpretation1_scope: NULL has been replaced
by ‘climate’
- thickness (S2LRKkmlb0b8AI): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRlfraoSeoVw): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRlGrJWqFEpB): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18O (S2LRluQHyUNHo2): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRLVET1EI6Sj): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRMc4vZMYxvL): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRMJtbf2EOP0): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandardComposite (S2LRmQATooN0aV): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRMrNQvnOYrc): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRmuqQB6lcYQ): interpretation1_scope: NULL has been replaced
by ‘climate’
- thicknessComposite (S2LRN2GdB926UC): interpretation1_scope: NULL has
been replaced by ‘climate’
- d18OPrecision (S2LRn6iCVVGdru): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRnMXuEqWfJX): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRNNwf7REQCu): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecisionComposite (S2LRNqRtgTq1iA): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRnYpJwDd8qK): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandard (S2LROTQThuPgSf): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRoVbXH7BR7x): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRoyLh1TOLbR): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRp3s6k43817): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandardComposite (S2LRpyNer8aJWS): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandard (S2LRpzkDo2UBdi): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRQDodyRS6lb): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRQhBhxxe0FK): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRqpSpLsB1MX): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRqR3i4NSG2F): interpretation1_scope: NULL has
been replaced by ‘climate’
- hasAragoniteCorrection (S2LRr5LETk9CNM): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRr65BIQJZTo): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRRDqDvKnAP5): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRRHco9nHpt5): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRsGi5lIZXHH): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRSwwBW0lb3E): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OComposite (S2LRTr7ZDhqUqi): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRtRVVomxeNU): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRTXaTk6oDkt): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRU1ZioGYCue): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CComposite (S2LRuc3ddbau9a): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRUKbTSKljyT): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRukxu5zMRoG): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRV8aIHy6bbJ): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasAragoniteCorrection (S2LRwiZAOOv3qA): interpretation1_scope: NULL
has been replaced by ‘climate’
- hasHiatusComposite (S2LRWYQUWKs3Z0): interpretation1_scope: NULL has
been replaced by ‘climate’
- d13C (S2LRX6iz8wd5fr): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasHiatus (S2LRxNDNEW3g3K): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRYdoJbT6c8F): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRytLgW31f3d):
interpretation1_scope: NULL has been replaced by ‘climate’
- d13CStandard (S2LRZ20XRcEGKf): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogyComposite (S2LRZHZ296T1nz): interpretation1_scope: NULL
has been replaced by ‘climate’
- thickness (S2LRzMOjCOwBqk): interpretation1_scope: NULL has been
replaced by ‘climate’
- Paleo Column metadata:
- d13C (S2LR27gTENlWBq): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d13C (S2LR9FLJjpdEeB): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d13C (S2LRc2GmyUEf4a): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d18O (S2LRguf0WlEbDS): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d18O (S2LRicR32s8P0D): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d13C (S2LRIoL0ftB6A9): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d13C (S2LRjpo9oX7HID): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d18O (S2LRk6ihlvDZaR): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d18O (S2LRlGrJWqFEpB): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d18O (S2LRluQHyUNHo2): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d18O (S2LRmuqQB6lcYQ): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d13C (S2LRoyLh1TOLbR): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
- d18O (S2LRukxu5zMRoG): paleoData_notes: NULL has been replaced by
‘“1) the deglaciation is not visible in the Villars stalagmite where the
d18O remains relatively stable within a 1% variation; (2) the d18O does
not clearly show the YD in the Villars and La Mine samples. However, the
d18O record of the Chau-stm6 sample is very similar to the d13C: it
recorded the BA transition, the cold episode during the BA period and
the YD. This raises the question of why the stalagmite d13C records
climate change in all three stalagmites while the d18O displays a marked
climatic signal only in the Chauvet Cave sample.” (Gentry et al.,
2006)’
- d13C (S2LRX6iz8wd5fr): paleoData_notes: NULL has been replaced by
‘“The overall d13C speleothem record seems to follow a baseline
temperature increase controlled by the increase in insolation and
punctuated by cold events possibly due to the N-America freshwater lake
discharges….the d13C is mainly controlled by the soil biogenic
production (plant root respiration and microbial activity of the soil
and the epikarst zone), which is linked to climatic factors such as
temperature and humidity…the d13C variations are attributed to changes
in soil and vegetation activity induced by temperature and humidity
change” (Gentry et al. 2006)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:23:32 UTC
- notes: Created from SISALv2