Version history for MBKdLAR2spY6hc56OHM0 -
Bunkercave.Fohlmeister.2012
Version: 1.0.15
- lastVersion: 1.0.14
- curator: nicholas
- timestamp: 2025-06-25 22:45:58.399916 UTC
- changes:
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/// deleteMe’ has been replaced by ‘deleteMe’
Version: 1.0.14
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- curator: nicholas
- timestamp: 2025-06-25 21:21:38.151862 UTC
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detrended and smoothed time series of Mg/Ca and δ13C for Bu4 (Fig. 4a
and b) implies that slow drip rates cor- respond to periods of less
precipitation.” (Fohlmeister et al., 2012) “ore nega- tive d13C values
in the Speleothem are associated with periods of denser vegetation as
well as a thickening of the soil above the cave, increased biological
soil activity and higher drip rates. The most negative d13C values
during MIS 3 are in the range of the d13C values of the Holocene
stalagmites and modern-day calcite samples (Fig. 7). This indicates, at
least for some time intervals of MIS 3, an enhanced biological activity
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al., 2018)’ has been replaced by ‘((( null ))) “Therefore, high δ13C
values are assigned to periods of low drip rates and vice versa. Apart
from periodically appearing differences, the overall similar- ity of the
detrended and smoothed time series of Mg/Ca and δ13C for Bu4 (Fig. 4a
and b) implies that slow drip rates cor- respond to periods of less
precipitation.” (Fohlmeister et al., 2012) “ore nega- tive d13C values
in the speleothem are associated with periods of denser vegetation as
well as a thickening of the soil above the cave, increased biological
soil activity and higher drip rates. The most negative d13C values
during MIS 3 are in the range of the d13C values of the Holocene
stalagmites and modern-day calcite samples (Fig. 7). This indicates, at
least for some time intervals of MIS 3, an enhanced biological activity
above the cave, almost as high as for present-day conditions.” (Weber et
al., 2018) /// “Therefore, high δ13C values are assigned to periods of
low drip rates and vice versa. Apart from periodically appearing
differences, the overall similar- ity of the detrended and smoothed time
series of Mg/Ca and δ13C for Bu4 (Fig. 4a and b) implies that slow drip
rates cor- respond to periods of less precipitation.” (Fohlmeister et
al., 2012) “ore nega- tive d13C values in the Speleothem are associated
with periods of denser vegetation as well as a thickening of the soil
above the cave, increased biological soil activity and higher drip
rates. The most negative d13C values during MIS 3 are in the range of
the d13C values of the Holocene stalagmites and modern-day calcite
samples (Fig. 7). This indicates, at least for some time intervals of
MIS 3, an enhanced biological activity above the cave, almost as high as
for present-day conditions.” (Weber et al., 2018)’
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Version: 1.0.12
- lastVersion: 1.0.11
- curator: nicholas
- timestamp: 2023-08-17 19:02:03 UTC
- changes:
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Version: 1.0.11
- lastVersion: 1.0.10
- curator: nicholas
- timestamp: 2023-08-10 22:44:33 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_author: NULL has been replaced by ‘J. Fohlmeister and A.
Schröder-Ritzrau and D. Scholz and C. Spötl and D. F. C. Riechelmann
and M. Mudelsee and A. Wackerbarth and A. Gerdes and S. Riechelmann and
A. Immenhauser and D. K. Richter and A. Mangini’
- pub1_journal: NULL has been replaced by ‘Climate of the Past’
- pub1_pages: NULL has been replaced by ‘1751–1764’
- pub1_title: NULL has been replaced by ‘Bunker Cave stalagmites: an
archive for central European Holocene climate variability’
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deleteMe /// null’ has been replaced by ‘null’
Version: 1.0.10
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- timestamp: 2023-07-05 00:35:13 UTC
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Version: 1.0.9
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- timestamp: 2023-02-13 23:38:54 UTC
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- curator: nicholas
- timestamp: 2022-07-28 17:28:36 UTC
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Version: 1.0.6
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- curator: nicholas
- timestamp: 2022-07-15 22:58:46 UTC
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Version: 1.0.4
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- timestamp: 2021-11-17 02:05:42 UTC
- changes:
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Version: 1.0.3
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- timestamp: 2021-10-05 21:38:34 UTC
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Version: 1.0.2
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- curator: nick
- timestamp: 2021-03-17 01:52:06 UTC
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Apart from periodically appearing differences, the overall similar- ity
of the detrended and smoothed time series of Mg/Ca and δ13C for Bu4
(Fig. 4a and b) implies that slow drip rates cor- respond to periods of
less precipitation.” (Fohlmeister et al., 2012) “ore nega- tive d13C
values in the speleothem are associated with periods of denser
vegetation as well as a thickening of the soil above the cave, increased
biological soil activity and higher drip rates. The most negative d13C
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Version: 1.0.1
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- timestamp: 2021-01-12 02:28:34 UTC
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replaced by ‘climate’
- d18OPrecision (S2LRg1zQhhxI7E): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRGNjGBxbcXF): interpretation1_scope: NULL
has been replaced by ‘climate’
- thickness (S2LRHmWc2lfVuT): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRHQ9zhEhlw8): interpretation1_scope: NULL has been replaced
by ‘climate’
- d18OStandard (S2LRhtdsL0Gnw0): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRhtub8ilrVE): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRIJYiLDYkEe): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRIRwJU4hKTz): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRixDs1D6pF8): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRjh8gFedsvd): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRK1sg7UvUpM): interpretation1_scope: NULL has been
replaced by ‘climate’
- thickness (S2LRkhJwjysbGZ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRkm4DEIcBXd): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRkqJOLVMAcQ): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRLE10HRondc): interpretation1_scope: NULL has been replaced
by ‘climate’
- entityName (S2LRlnz1FmlGl0): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRMAifXx3MTy): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRmEMB4MUinI): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OStandard (S2LRMGbLAD7vVt): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRmqLqFSdDUt): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRmuN5Zl6Fcv): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrection (S2LRn2CqU7TFqa): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CPrecision (S2LRnlvuPlnG57): interpretation1_scope: NULL has been
replaced by ‘climate’
- depthComposite (S2LRNMGbVGOrAn): interpretation1_scope: NULL has
been replaced by ‘climate’
- hasAragoniteCorrection (S2LRODguDbYm4k): interpretation1_scope: NULL
has been replaced by ‘climate’
- thickness (S2LRoftsOxCklq): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasHiatus (S2LRoLdCyviVZm): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRqhWCyiTNWs): interpretation1_scope: NULL has been
replaced by ‘climate’
- mineralogy (S2LRqyBiQO5hVf): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRqYlHXiZXfx): interpretation1_scope: NULL has been replaced
by ‘climate’
- mineralogy (S2LRT8BYxb9Ytl): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CStandard (S2LRtbdRJ40p9w): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18O (S2LRtCZoNVI7Wr): interpretation1_scope: NULL has been replaced
by ‘climate’
- hasAragoniteCorrection (S2LRugtSiEldAi): interpretation1_scope: NULL
has been replaced by ‘climate’
- sisalSampleID (S2LRv7MhhanKXL): interpretation1_scope: NULL has been
replaced by ‘climate’
- d18OPrecision (S2LRvC1jqAwZNR): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleIDComposite (S2LRVpM3jtFycY): interpretation1_scope: NULL
has been replaced by ‘climate’
- mineralogyComposite (S2LRVZor5xajjZ): interpretation1_scope: NULL
has been replaced by ‘climate’
- d13CStandard (S2LRxkCafbfpXy): interpretation1_scope: NULL has been
replaced by ‘climate’
- hasAragoniteCorrectionComposite (S2LRxqJkD0hant):
interpretation1_scope: NULL has been replaced by ‘climate’
- d13CComposite (S2LRY7rytUwa7G): interpretation1_scope: NULL has been
replaced by ‘climate’
- sisalSampleID (S2LRyZU21TB6EB): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13CPrecision (S2LRz2khYzZ3w7): interpretation1_scope: NULL has been
replaced by ‘climate’
- d13C (S2LRZQk8QMZOrI): interpretation1_scope: NULL has been replaced
by ‘climate’
- Paleo Column metadata:
- d18OComposite (S2LR55l3oDCONY): paleoData_notes: NULL has been
replaced by ‘“More positive δ18O values reflect cold and dry winters,
whereas more negative δ18O values repre- sent warmer and more humid
winters” (Fohlmeister et al., 2012)’
- d18OComposite (S2LR55l3oDCONY): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d18OComposite (S2LR55l3oDCONY): paleoData_QCnotes: NULL has been
replaced by ‘“The temporally overlapping sections allow us to assemble a
composite record…We interpret the short-term variations in the Mg/Ca ra-
tios of the Bunker Cave stalagmites during the Holocene (Fig. 3a) as
precipitation variability above the cave. The de- trended Mg/Ca ratio
(Fig. 4a) is, therefore, interpreted as a proxy for precipitation
amount.”(Fohlmeister et al., 2012)’
- d13CComposite (S2LRY7rytUwa7G): paleoData_notes: NULL has been
replaced by ‘“Therefore, high δ13C values are assigned to periods of low
drip rates and vice versa. Apart from periodically appearing
differences, the overall similar- ity of the detrended and smoothed time
series of Mg/Ca and δ13C for Bu4 (Fig. 4a and b) implies that slow drip
rates cor- respond to periods of less precipitation.” (Fohlmeister et
al., 2012) “ore nega- tive d13C values in the speleothem are associated
with periods of denser vegetation as well as a thickening of the soil
above the cave, increased biological soil activity and higher drip
rates. The most negative d13C values during MIS 3 are in the range of
the d13C values of the Holocene stalagmites and modern-day calcite
samples (Fig. 7). This indicates, at least for some time intervals of
MIS 3, an enhanced biological activity above the cave, almost as high as
for present-day conditions.” (Weber et al., 2018)’
- d13CComposite (S2LRY7rytUwa7G): paleoData_QCCertification: NULL has
been replaced by ‘CH’
- d13CComposite (S2LRY7rytUwa7G): paleoData_QCnotes: NULL has been
replaced by ‘“The temporally overlapping sections allow us to assemble a
composite record…We interpret the short-term variations in the Mg/Ca ra-
tios of the Bunker Cave stalagmites during the Holocene (Fig. 3a) as
precipitation variability above the cave. The de- trended Mg/Ca ratio
(Fig. 4a) is, therefore, interpreted as a proxy for precipitation
amount.”(Fohlmeister et al., 2012)’
Version: 1.0.0
- curator: nick
- timestamp: 2020-09-29 14:26:16 UTC
- notes: Created from SISALv2