Version history for LCad85043fd257004e193465576d7974b9 -
LakeWA01.Ravindra.2009
Version: 1.0.7
- lastVersion: 1.0.6
- curator: nicholas
- timestamp: 2023-08-10 23:02:31 UTC
- changes:
Version: 1.0.6
- lastVersion: 1.0.5
- curator: nicholas
- timestamp: 2023-07-05 00:47:11 UTC
- changes:
- Paleo Interpretation metadata:
Version: 1.0.5
- lastVersion: 1.0.4
- curator: nicholas
- timestamp: 2023-05-25 17:47:54 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
- Geographic metadata:
- geo_elevation: NULL has been replaced by ‘1000’
Version: 1.0.4
- lastVersion: 1.0.3
- curator: nicholas
- timestamp: 2023-02-13 23:48:58 UTC
- changes:
- Paleo Interpretation metadata:
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Version: 1.0.3
- lastVersion: 1.0.2
- curator: nicholas
- timestamp: 2023-02-09 15:54:36 UTC
- notes: Updated lipdverse database entry with a changed
file.
- changes:
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- Paleo Column metadata:
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Version: 1.0.2
- lastVersion: 1.0.1
- curator: nicholas
- timestamp: 2022-09-09 02:09:55 UTC
- changes:
- Paleo Column metadata:
- precipitation (lcRBEvaydIFwOnSZuma): paleoData_QCnotes: ‘Marked in
original compilation as primary P timeseries; Pass age control and data
resolution’ has been replaced by ‘Marked in original compilation as
primary P timeseries; Pass age control and data resolution; pvalue
<0.1’
- Paleo Interpretation metadata:
- precipitation (lcRBEvaydIFwOnSZuma): interpretation1_seasonality:
‘Annual’ has been replaced by ‘1,2,3,4,5,6,7,8,9,10,11,12’
Version: 1.0.1
- lastVersion: 1.0.0
- curator: nicholas
- timestamp: 2022-07-28 17:35:30 UTC
- changes:
- Base metadata:
- Publication metadata:
- pub1_year: NULL has been replaced by ‘2009’
- pub1_author: NULL has been replaced by ‘Ravindra, R.’
- pub1_doi: NULL has been replaced by ‘Ravindra, R., 2009. A
high-resolution vegetation, fire, and climate history from the Aishihik
Region, Yukon Territory, Canada. Master’s thesis. University of Ottawa,
Ottawa, Ontario, Canada.’
- pub1_journal: NULL has been replaced by ‘Master’s thesis. University
of Ottawa’
- pub1_title: NULL has been replaced by ‘A high-resolution vegetation,
fire, and climate history from the Aishihik Region, Yukon Territory,
Canada.’
- pub2_doi: NULL has been replaced by ‘10.5194/essd-2022-38’
- Geographic metadata:
- geo_elevation: ‘1000’ has been replaced by NULL
- geo_gcmdLocation: NULL has been replaced by ‘North
America>Canada>Yukon Territory’
- Paleo Column metadata:
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- temperature (lcR7wdiBBdrwSVan3v6): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
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characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
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Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRAaspP4ZPsRPpNmK3): paleoData_proxyGeneral: NULL has
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be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
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- precipitationUncertainty (lcRACZZn67ECABJEqIp):
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density boreal forests dominated by white spruce (Picea glauca). White
spruce stands in the region tend to be found on well-drained soils and
on the sides and tops of slopes. Stands of poplar and aspen, as well as
birch and alder are also common, particularly in low-lying areas and on
more poorly drained sites. In the understory, the vegetation includes
juniper and willow as well as numerous herbaceous plants such as species
of grasses and sedges, which tend to occur on more poorly drained sites.
Epilobium and Shepherdia also form a small component of the modern
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been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
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Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
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been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
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Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
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been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- precipitation (lcRcxrVNR2nWomdDibe): paleoData_proxyGeneral: NULL
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- precipitation (lcRDLIrQ3r1bza10EP1): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- precipitation (lcRDLIrQ3r1bza10EP1): paleoData_proxyGeneral: NULL
has been replaced by ‘pollen’
- temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_datum: NULL has been
replaced by ‘abs’
- temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxy: NULL has been
replaced by ‘pollen’
- temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRDsQI4d9Vj9NmLyO4): paleoData_proxyGeneral: NULL has
been replaced by ‘pollen’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_datum:
NULL has been replaced by ‘abs’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2): paleoData_proxy:
NULL has been replaced by ‘pollen’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2):
paleoData_proxyDetail: NULL has been replaced by ‘The vegetation
surrounding the study site is characterized by the presence of low
density boreal forests dominated by white spruce (Picea glauca). White
spruce stands in the region tend to be found on well-drained soils and
on the sides and tops of slopes. Stands of poplar and aspen, as well as
birch and alder are also common, particularly in low-lying areas and on
more poorly drained sites. In the understory, the vegetation includes
juniper and willow as well as numerous herbaceous plants such as species
of grasses and sedges, which tend to occur on more poorly drained sites.
Epilobium and Shepherdia also form a small component of the modern
vegetation, and are principally found on well-drained soils.’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- precipitation (lcRey1szXCIV3MDlOQu): paleoData_datum: NULL has been
replaced by ‘abs’
- precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxy: NULL has been
replaced by ‘pollen’
- precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- precipitation (lcRey1szXCIV3MDlOQu): paleoData_proxyGeneral: NULL
has been replaced by ‘pollen’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_datum:
NULL has been replaced by ‘abs’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE): paleoData_proxy:
NULL has been replaced by ‘pollen’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE):
paleoData_proxyDetail: NULL has been replaced by ‘The vegetation
surrounding the study site is characterized by the presence of low
density boreal forests dominated by white spruce (Picea glauca). White
spruce stands in the region tend to be found on well-drained soils and
on the sides and tops of slopes. Stands of poplar and aspen, as well as
birch and alder are also common, particularly in low-lying areas and on
more poorly drained sites. In the understory, the vegetation includes
juniper and willow as well as numerous herbaceous plants such as species
of grasses and sedges, which tend to occur on more poorly drained sites.
Epilobium and Shepherdia also form a small component of the modern
vegetation, and are principally found on well-drained soils.’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRg28xetE4FcERjdJy): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRg28xetE4FcERjdJy):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- precipitation (lcRH5hdhvPNova4q7T8): paleoData_datum: NULL has been
replaced by ‘abs’
- precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxy: NULL has been
replaced by ‘pollen’
- precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- precipitation (lcRH5hdhvPNova4q7T8): paleoData_proxyGeneral: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperature (lcRkWs33uxYMlG8FERV): paleoData_datum: NULL has been
replaced by ‘abs’
- temperature (lcRkWs33uxYMlG8FERV): paleoData_proxy: NULL has been
replaced by ‘pollen’
- temperature (lcRkWs33uxYMlG8FERV): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRkWs33uxYMlG8FERV): paleoData_proxyGeneral: NULL has
been replaced by ‘pollen’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperature (lcRqPq0E2ipc9svss1o): paleoData_datum: NULL has been
replaced by ‘abs’
- temperature (lcRqPq0E2ipc9svss1o): paleoData_proxy: NULL has been
replaced by ‘pollen’
- temperature (lcRqPq0E2ipc9svss1o): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRqPq0E2ipc9svss1o): paleoData_proxyGeneral: NULL has
been replaced by ‘pollen’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_datum:
NULL has been replaced by ‘abs’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1): paleoData_proxy:
NULL has been replaced by ‘pollen’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1):
paleoData_proxyDetail: NULL has been replaced by ‘The vegetation
surrounding the study site is characterized by the presence of low
density boreal forests dominated by white spruce (Picea glauca). White
spruce stands in the region tend to be found on well-drained soils and
on the sides and tops of slopes. Stands of poplar and aspen, as well as
birch and alder are also common, particularly in low-lying areas and on
more poorly drained sites. In the understory, the vegetation includes
juniper and willow as well as numerous herbaceous plants such as species
of grasses and sedges, which tend to occur on more poorly drained sites.
Epilobium and Shepherdia also form a small component of the modern
vegetation, and are principally found on well-drained soils.’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperature (lcRut4aNuph5mDCCvOM): paleoData_datum: NULL has been
replaced by ‘abs’
- temperature (lcRut4aNuph5mDCCvOM): paleoData_proxy: NULL has been
replaced by ‘pollen’
- temperature (lcRut4aNuph5mDCCvOM): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRut4aNuph5mDCCvOM): paleoData_proxyGeneral: NULL has
been replaced by ‘pollen’
- temperature (lcRXwlNyww6riv4ygrW): paleoData_datum: NULL has been
replaced by ‘abs’
- temperature (lcRXwlNyww6riv4ygrW): paleoData_proxy: NULL has been
replaced by ‘pollen’
- temperature (lcRXwlNyww6riv4ygrW): paleoData_proxyDetail: NULL has
been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperature (lcRXwlNyww6riv4ygrW): paleoData_proxyGeneral: NULL has
been replaced by ‘pollen’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_datum: NULL
has been replaced by ‘abs’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_proxy: NULL
has been replaced by ‘pollen’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ): paleoData_proxyDetail:
NULL has been replaced by ‘The vegetation surrounding the study site is
characterized by the presence of low density boreal forests dominated by
white spruce (Picea glauca). White spruce stands in the region tend to
be found on well-drained soils and on the sides and tops of slopes.
Stands of poplar and aspen, as well as birch and alder are also common,
particularly in low-lying areas and on more poorly drained sites. In the
understory, the vegetation includes juniper and willow as well as
numerous herbaceous plants such as species of grasses and sedges, which
tend to occur on more poorly drained sites. Epilobium and Shepherdia
also form a small component of the modern vegetation, and are
principally found on well-drained soils.’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_datum:
NULL has been replaced by ‘abs’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU): paleoData_proxy:
NULL has been replaced by ‘pollen’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU):
paleoData_proxyDetail: NULL has been replaced by ‘The vegetation
surrounding the study site is characterized by the presence of low
density boreal forests dominated by white spruce (Picea glauca). White
spruce stands in the region tend to be found on well-drained soils and
on the sides and tops of slopes. Stands of poplar and aspen, as well as
birch and alder are also common, particularly in low-lying areas and on
more poorly drained sites. In the understory, the vegetation includes
juniper and willow as well as numerous herbaceous plants such as species
of grasses and sedges, which tend to occur on more poorly drained sites.
Epilobium and Shepherdia also form a small component of the modern
vegetation, and are principally found on well-drained soils.’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU):
paleoData_proxyGeneral: NULL has been replaced by ‘pollen’
- Paleo Interpretation metadata:
- temperature (lcR7wdiBBdrwSVan3v6): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcR7wdiBBdrwSVan3v6):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperature (lcRAaspP4ZPsRPpNmK3): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRAaspP4ZPsRPpNmK3):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRaBtvhnbXzd6pYLOD):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRaBtvhnbXzd6pYLOD):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- precipitationUncertainty (lcRACZZn67ECABJEqIp):
interpretation1_variableDetail: ‘precip@surface’ has been replaced by ‘precipitation@surface’
- precipitationUncertainty (lcRACZZn67ECABJEqIp):
interpretation1_direction: NULL has been replaced by ‘positive’
- precipitationUncertainty (lcRACZZn67ECABJEqIp):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitation (lcRBEvaydIFwOnSZuma): interpretation1_variableDetail:
‘precip@surface’ has
been replaced by ‘precipitation@surface’
- precipitation (lcRBEvaydIFwOnSZuma): interpretation1_direction: NULL
has been replaced by ‘positive’
- precipitation (lcRBEvaydIFwOnSZuma):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperature (lcRBUQS8kdbl9IOGHfr): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRBUQS8kdbl9IOGHfr):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- precipitation (lcRcxrVNR2nWomdDibe): interpretation1_variableDetail:
‘precip@surface’ has
been replaced by ‘precipitation@surface’
- precipitation (lcRcxrVNR2nWomdDibe): interpretation1_direction: NULL
has been replaced by ‘positive’
- precipitation (lcRcxrVNR2nWomdDibe):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_variableDetail:
‘precip@surface’ has
been replaced by ‘precipitation@surface’
- precipitation (lcRDLIrQ3r1bza10EP1): interpretation1_direction: NULL
has been replaced by ‘positive’
- precipitation (lcRDLIrQ3r1bza10EP1):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperature (lcRDsQI4d9Vj9NmLyO4): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRDsQI4d9Vj9NmLyO4):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2):
interpretation1_variableDetail: ‘precip@surface’ has been replaced by ‘precipitation@surface’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2):
interpretation1_direction: NULL has been replaced by ‘positive’
- precipitationUncertainty (lcRdtbiak4cBS9UNCl2):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitation (lcRey1szXCIV3MDlOQu): interpretation1_variableDetail:
‘precip@surface’ has
been replaced by ‘precipitation@surface’
- precipitation (lcRey1szXCIV3MDlOQu): interpretation1_direction: NULL
has been replaced by ‘positive’
- precipitation (lcRey1szXCIV3MDlOQu):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE):
interpretation1_variableDetail: ‘precip@surface’ has been replaced by ‘precipitation@surface’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE):
interpretation1_direction: NULL has been replaced by ‘positive’
- precipitationUncertainty (lcRFSEF4OL5Vk4jFuIE):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRg28xetE4FcERjdJy):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRg28xetE4FcERjdJy):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitation (lcRH5hdhvPNova4q7T8): interpretation1_variableDetail:
‘precip@surface’ has
been replaced by ‘precipitation@surface’
- precipitation (lcRH5hdhvPNova4q7T8): interpretation1_direction: NULL
has been replaced by ‘positive’
- precipitation (lcRH5hdhvPNova4q7T8):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRKnRU8BaG89LhHfcI):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRkPFrIQCjycIWczXz):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- temperature (lcRkWs33uxYMlG8FERV): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRkWs33uxYMlG8FERV):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRloO7sekK2UgRzAN6):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRoeTZpvXUXQDYJbUW):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- temperature (lcRqPq0E2ipc9svss1o): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRqPq0E2ipc9svss1o):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1):
interpretation1_variableDetail: ‘precip@surface’ has been replaced by ‘precipitation@surface’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1):
interpretation1_direction: NULL has been replaced by ‘positive’
- precipitationUncertainty (lcRt2tvSndxaHJf95q1):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperature (lcRut4aNuph5mDCCvOM): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRut4aNuph5mDCCvOM):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- temperature (lcRXwlNyww6riv4ygrW): interpretation1_direction: NULL
has been replaced by ‘positive’
- temperature (lcRXwlNyww6riv4ygrW):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRxyCa4XQKzGKkEceF):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ):
interpretation1_direction: NULL has been replaced by ‘positive’
- temperatureUncertainty (lcRyZkdjY6gA9pvlIdZ):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘summer+’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU):
interpretation1_variableDetail: ‘precip@surface’ has been replaced by ‘precipitation@surface’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU):
interpretation1_direction: NULL has been replaced by ‘positive’
- precipitationUncertainty (lcRz8WFv2GH7NS4KdOU):
interpretation1_seasonalityGeneral: NULL has been replaced by
‘Annual’
Version: 1.0.0
- curator: nicholas
- timestamp: 2022-05-26 21:53:11 UTC
- notes: Starting the changelog