8 research outputs found
Cyclic Variation of Residual (CO2 + H2O) and Total Pressure in Conifer Stem and Woody Root Tree Rings
Tree-ring chronologies of stem discs and core samples have been widely used to reconstruct the climatic conditions of tree growth. However, insufficient attention has been given to the fact that root and stem wood accumulate biogenic gases, whose distribution in annual rings can also be related to the climate-dependent features of tree growth. The study of chronologies of gas samples extracted under vacuum from the wood of tree-ring discs of the Siberian stone pine (Pinus sibirica Du Tour), Scots pine (Pinus sylvestris L.), Siberian larch (Larix sibirica Ledeb.) and Siberian spruce (Picea obovata Ledeb.) suggests that annual distributions of CO2 and H2O in the rings and pressure variation in extracted samples follow a cyclic pattern. It was found that the sample pressure and the content of CO2 and H2O in the annual rings in stems and roots of the Siberian stone pine and Scots pine from Tomsk (Russia) area are characterized by varied time cycles, including periods of about 4 and 11 years, the latter corresponding to the period of the solar activity cycle. The four-year cycle in the above chronologies is explained by the presence of similar cycles in temperature and precipitation chronologies, where cyclic variations of CO2 in the rings can be interpreted as a response of the plant to the change in the climatic conditions. The established cyclic variation of the pressure and CO2 content in tree rings in stems and roots indicates that CO2 release into the atmosphere should also follow a cyclic pattern. Therefore, to estimate correctly the release of CO2 by tree stems and large roots, long-term measurements are require
Π¦ΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΠΎΡΡΠ°ΡΠΎΡΠ½ΠΎΠ³ΠΎ (Π‘Π2 + Π2Π) ΠΈ ΠΏΠΎΠ»Π½ΠΎΠ³ΠΎ Π΄Π°Π²Π»Π΅Π½ΠΈΡ Π² Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Π΅ ΠΊΠΎΠ»Π΅Ρ ΡΡΠ²ΠΎΠ»Π° ΠΈ ΠΊΠΎΡΠ½Ρ Ρ Π²ΠΎΠΉΠ½ΡΡ Π΄Π΅ΡΠ΅Π²ΡΠ΅Π²
Tree-ring chronologies of stem discs and core samples have been widely used to reconstruct the
climatic conditions of tree growth. However, insufficient attention has been given to the fact that root
and stem wood accumulate biogenic gases, whose distribution in annual rings can also be related to
the climate-dependent features of tree growth. The study of chronologies of gas samples extracted
under vacuum from the wood of tree-ring discs of the Siberian stone pine (Pinus sibirica Du Tour),
Scots pine (Pinus sylvestris L.), Siberian larch (Larix sibirica Ledeb.) and Siberian spruce (Picea
obovata Ledeb.) suggests that annual distributions of CO2 and H2O in the rings and pressure variation
in extracted samples follow a cyclic pattern. It was found that the sample pressure and the content of
CO2 and H2O in the annual rings in stems and roots of the Siberian stone pine and Scots pine from
Tomsk (Russia) area are characterized by varied time cycles, including periods of about 4 and 11
years, the latter corresponding to the period of the solar activity cycle. The four-year cycle in the
above chronologies is explained by the presence of similar cycles in temperature and precipitation
chronologies, where cyclic variations of CO2 in the rings can be interpreted as a response of the
plant to the change in the climatic conditions. The established cyclic variation of the pressure and
CO2 content in tree rings in stems and roots indicates that CO2 release into the atmosphere should
also follow a cyclic pattern. Therefore, to estimate correctly the release of CO2 by tree stems and large
roots, long-term measurements are requiredΠΡΠ΅Π²Π΅ΡΠ½ΠΎ-ΠΊΠΎΠ»ΡΡΠ΅Π²ΡΠ΅ Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΡΠΏΠΈΠ»ΠΎΠ² ΠΈ ΠΊΠ΅ΡΠ½ΠΎΠ² Π΄Π΅ΡΠ΅Π²ΡΠ΅Π² ΡΠΈΡΠΎΠΊΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΡΡΡΡ Π΄Π»Ρ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΉ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π°. ΠΠ΄Π½Π°ΠΊΠΎ ΠΎΡΡΠ°Π΅ΡΡΡ Π² ΡΡΠΎΡΠΎΠ½Π΅ ΡΠΎΡ ΡΠ°ΠΊΡ, ΡΡΠΎ Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Π°
ΠΊΠΎΡΠ½Π΅ΠΉ ΠΈ ΡΡΠ²ΠΎΠ»ΠΎΠ² ΡΠΎΡ
ΡΠ°Π½ΡΠ΅Ρ Π²Π½ΡΡΡΠΈ ΡΠ΅Π±Ρ Π±ΠΈΠΎΠ³Π΅Π½Π½ΡΠ΅ Π³Π°Π·Ρ, ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΠΊΠΎΡΠΎΡΡΡ
ΠΏΠΎ Π³ΠΎΠ΄ΠΈΡΠ½ΡΠΌ
ΠΊΠΎΠ»ΡΡΠ°ΠΌ ΡΠ°ΠΊΠΆΠ΅ ΠΌΠΎΠΆΠ΅Ρ ΠΎΡΡΠ°ΠΆΠ°ΡΡ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π°. ΠΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅
Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΉ Π³Π°Π·ΠΎΠ²ΡΡ
ΠΏΡΠΎΠ±, ΠΈΠ·Π²Π»Π΅ΠΊΠ°Π΅ΠΌΡΡ
ΠΏΠΎΠ΄ Π²Π°ΠΊΡΡΠΌΠΎΠΌ ΠΈΠ· Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Ρ Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ ΡΠΏΠΈΠ»ΠΎΠ² ΠΊΠ΅Π΄ΡΠ°
(Pinus sibirica Du Tour), ΡΠΎΡΠ½Ρ (Pinus sylvestris L.), Π»ΠΈΡΡΠ²Π΅Π½Π½ΠΈΡΡ (Larix sibirica Ledeb.), Π΅Π»ΠΈ (Picea
obovata Ledeb), ΡΠΊΠ°Π·ΡΠ²Π°Π΅Ρ Π½Π° ΡΠΎ, ΡΡΠΎ ΠΏΠΎΠ³ΠΎΠ΄ΠΈΡΠ½ΡΠ΅ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΡΠΎΡ
ΡΠ°Π½ΠΈΠ²ΡΠΈΡ
ΡΡ Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
Π‘Π2,
Π2Π ΠΈ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Π΄Π°Π²Π»Π΅Π½ΠΈΡ ΠΈΠ·Π²Π»Π΅ΠΊΠ°Π΅ΠΌΠΎΠΉ ΠΏΡΠΎΠ±Ρ Π½ΠΎΡΡΡ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠΉ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ. ΠΠ±Π½Π°ΡΡΠΆΠ΅Π½ΠΎ, ΡΡΠΎ
Π΄Π°Π²Π»Π΅Π½ΠΈΠ΅ ΠΏΡΠΎΠ±Ρ, ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ Π‘Π2 ΠΈ Π2Π Π² Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»ΡΡΠ°Ρ
ΡΡΠ²ΠΎΠ»ΠΎΠ² ΠΈ ΠΊΠΎΡΠ½Π΅ΠΉ ΠΊΠ΅Π΄ΡΠ° ΠΈ ΡΠΎΡΠ½Ρ ΠΈΠ·
ΡΠ°ΠΉΠΎΠ½Π° Π’ΠΎΠΌΡΠΊΠ° (Π ΠΎΡΡΠΈΡ) ΠΈΡΠΏΡΡΡΠ²Π°ΡΡ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
Π²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
ΠΌΠ°ΡΡΡΠ°Π±ΠΎΠ², Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅
Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄Π°ΠΌΠΈ ΠΎΠΊΠΎΠ»ΠΎ 4 ΠΈ 11 Π»Π΅Ρ, ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΠΉ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΡΠ΅Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄Ρ ΡΠΈΠΊΠ»Π° ΡΠΎΠ»Π½Π΅ΡΠ½ΠΎΠΉ
Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ. ΠΠΎΡΠ²Π»Π΅Π½ΠΈΠ΅ ΡΠΈΠΊΠ»Π° Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄ΠΎΠΌ 4 Π³ΠΎΠ΄Π° Π² Π½Π°ΠΉΠ΄Π΅Π½Π½ΡΡ
Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΡ
ΠΎΠ±ΡΡΡΠ½ΡΠ΅ΡΡΡ
ΡΡΡΠ΅ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΏΠΎΠ΄ΠΎΠ±Π½ΡΡ
ΡΠΈΠΊΠ»ΠΎΠ² Π² Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΡ
ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡ ΠΈ ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π° ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠ΅
Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΡΠ΅Π³ΠΈΡΡΡΠΈΡΡΠ΅ΠΌΠΎΠ³ΠΎ Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
Π‘Π2 ΠΌΠΎΠΆΠ½ΠΎ ΡΡΠΈΡΠ°ΡΡ ΡΠ΅Π°ΠΊΡΠΈΠ΅ΠΉ ΡΠ°ΡΡΠ΅Π½ΠΈΡ Π½Π° ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ. ΠΠ· ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½Π½ΠΎΠΉ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΎΠΉ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Π΄Π°Π²Π»Π΅Π½ΠΈΡ ΠΈ Π‘Π2 Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
ΡΠΏΠΈΠ»ΠΎΠ² ΡΡΠ²ΠΎΠ»ΠΎΠ² ΠΈ ΠΊΠΎΡΠ½Π΅ΠΉ Π΄Π΅ΡΠ΅Π²ΡΠ΅Π² ΡΠ»Π΅Π΄ΡΠ΅Ρ, ΡΡΠΎ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΠ΅ Π² Π°ΡΠΌΠΎΡΡΠ΅ΡΡ Π‘Π2 Π΄ΠΎΠ»ΠΆΠ½ΠΎ Π½ΠΎΡΠΈΡΡ
ΡΠ°ΠΊΠΆΠ΅ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠΉ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ, ΠΏΠΎΡΡΠΎΠΌΡ Π΄Π»Ρ ΠΊΠΎΡΡΠ΅ΠΊΡΠ½ΠΎΠΉ ΠΎΡΠ΅Π½ΠΊΠΈ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΡ Π‘Π2 ΡΡΠ²ΠΎΠ»Π°ΠΌΠΈ ΠΈ
ΠΊΡΡΠΏΠ½ΡΠΌΠΈ ΠΊΠΎΡΠ½ΡΠΌΠΈ ΡΠ»Π΅Π΄ΡΠ΅Ρ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΡΡ Π΄Π»ΠΈΡΠ΅Π»ΡΠ½ΡΠ΅ ΠΈΠ·ΠΌΠ΅ΡΠ΅Π½ΠΈ
Π¦ΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠ΅ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΠΎΡΡΠ°ΡΠΎΡΠ½ΠΎΠ³ΠΎ (Π‘Π2 + Π2Π) ΠΈ ΠΏΠΎΠ»Π½ΠΎΠ³ΠΎ Π΄Π°Π²Π»Π΅Π½ΠΈΡ Π² Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Π΅ ΠΊΠΎΠ»Π΅Ρ ΡΡΠ²ΠΎΠ»Π° ΠΈ ΠΊΠΎΡΠ½Ρ Ρ Π²ΠΎΠΉΠ½ΡΡ Π΄Π΅ΡΠ΅Π²ΡΠ΅Π²
Tree-ring chronologies of stem discs and core samples have been widely used to reconstruct the
climatic conditions of tree growth. However, insufficient attention has been given to the fact that root
and stem wood accumulate biogenic gases, whose distribution in annual rings can also be related to
the climate-dependent features of tree growth. The study of chronologies of gas samples extracted
under vacuum from the wood of tree-ring discs of the Siberian stone pine (Pinus sibirica Du Tour),
Scots pine (Pinus sylvestris L.), Siberian larch (Larix sibirica Ledeb.) and Siberian spruce (Picea
obovata Ledeb.) suggests that annual distributions of CO2 and H2O in the rings and pressure variation
in extracted samples follow a cyclic pattern. It was found that the sample pressure and the content of
CO2 and H2O in the annual rings in stems and roots of the Siberian stone pine and Scots pine from
Tomsk (Russia) area are characterized by varied time cycles, including periods of about 4 and 11
years, the latter corresponding to the period of the solar activity cycle. The four-year cycle in the
above chronologies is explained by the presence of similar cycles in temperature and precipitation
chronologies, where cyclic variations of CO2 in the rings can be interpreted as a response of the
plant to the change in the climatic conditions. The established cyclic variation of the pressure and
CO2 content in tree rings in stems and roots indicates that CO2 release into the atmosphere should
also follow a cyclic pattern. Therefore, to estimate correctly the release of CO2 by tree stems and large
roots, long-term measurements are requiredΠΡΠ΅Π²Π΅ΡΠ½ΠΎ-ΠΊΠΎΠ»ΡΡΠ΅Π²ΡΠ΅ Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΡΠΏΠΈΠ»ΠΎΠ² ΠΈ ΠΊΠ΅ΡΠ½ΠΎΠ² Π΄Π΅ΡΠ΅Π²ΡΠ΅Π² ΡΠΈΡΠΎΠΊΠΎ ΠΈΡΠΏΠΎΠ»ΡΠ·ΡΡΡΡΡ Π΄Π»Ρ ΡΠ΅ΠΊΠΎΠ½ΡΡΡΡΠΊΡΠΈΠΉ
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π°. ΠΠ΄Π½Π°ΠΊΠΎ ΠΎΡΡΠ°Π΅ΡΡΡ Π² ΡΡΠΎΡΠΎΠ½Π΅ ΡΠΎΡ ΡΠ°ΠΊΡ, ΡΡΠΎ Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Π°
ΠΊΠΎΡΠ½Π΅ΠΉ ΠΈ ΡΡΠ²ΠΎΠ»ΠΎΠ² ΡΠΎΡ
ΡΠ°Π½ΡΠ΅Ρ Π²Π½ΡΡΡΠΈ ΡΠ΅Π±Ρ Π±ΠΈΠΎΠ³Π΅Π½Π½ΡΠ΅ Π³Π°Π·Ρ, ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΠ΅ ΠΊΠΎΡΠΎΡΡΡ
ΠΏΠΎ Π³ΠΎΠ΄ΠΈΡΠ½ΡΠΌ
ΠΊΠΎΠ»ΡΡΠ°ΠΌ ΡΠ°ΠΊΠΆΠ΅ ΠΌΠΎΠΆΠ΅Ρ ΠΎΡΡΠ°ΠΆΠ°ΡΡ ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠΈ ΡΠΎΡΡΠ° Π΄Π΅ΡΠ΅Π²Π°. ΠΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅
Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΠΉ Π³Π°Π·ΠΎΠ²ΡΡ
ΠΏΡΠΎΠ±, ΠΈΠ·Π²Π»Π΅ΠΊΠ°Π΅ΠΌΡΡ
ΠΏΠΎΠ΄ Π²Π°ΠΊΡΡΠΌΠΎΠΌ ΠΈΠ· Π΄ΡΠ΅Π²Π΅ΡΠΈΠ½Ρ Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»Π΅Ρ ΡΠΏΠΈΠ»ΠΎΠ² ΠΊΠ΅Π΄ΡΠ°
(Pinus sibirica Du Tour), ΡΠΎΡΠ½Ρ (Pinus sylvestris L.), Π»ΠΈΡΡΠ²Π΅Π½Π½ΠΈΡΡ (Larix sibirica Ledeb.), Π΅Π»ΠΈ (Picea
obovata Ledeb), ΡΠΊΠ°Π·ΡΠ²Π°Π΅Ρ Π½Π° ΡΠΎ, ΡΡΠΎ ΠΏΠΎΠ³ΠΎΠ΄ΠΈΡΠ½ΡΠ΅ ΡΠ°ΡΠΏΡΠ΅Π΄Π΅Π»Π΅Π½ΠΈΡ ΡΠΎΡ
ΡΠ°Π½ΠΈΠ²ΡΠΈΡ
ΡΡ Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
Π‘Π2,
Π2Π ΠΈ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Π΄Π°Π²Π»Π΅Π½ΠΈΡ ΠΈΠ·Π²Π»Π΅ΠΊΠ°Π΅ΠΌΠΎΠΉ ΠΏΡΠΎΠ±Ρ Π½ΠΎΡΡΡ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠΉ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ. ΠΠ±Π½Π°ΡΡΠΆΠ΅Π½ΠΎ, ΡΡΠΎ
Π΄Π°Π²Π»Π΅Π½ΠΈΠ΅ ΠΏΡΠΎΠ±Ρ, ΡΠΎΠ΄Π΅ΡΠΆΠ°Π½ΠΈΠ΅ Π‘Π2 ΠΈ Π2Π Π² Π³ΠΎΠ΄ΠΈΡΠ½ΡΡ
ΠΊΠΎΠ»ΡΡΠ°Ρ
ΡΡΠ²ΠΎΠ»ΠΎΠ² ΠΈ ΠΊΠΎΡΠ½Π΅ΠΉ ΠΊΠ΅Π΄ΡΠ° ΠΈ ΡΠΎΡΠ½Ρ ΠΈΠ·
ΡΠ°ΠΉΠΎΠ½Π° Π’ΠΎΠΌΡΠΊΠ° (Π ΠΎΡΡΠΈΡ) ΠΈΡΠΏΡΡΡΠ²Π°ΡΡ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
Π²ΡΠ΅ΠΌΠ΅Π½Π½ΡΡ
ΠΌΠ°ΡΡΡΠ°Π±ΠΎΠ², Π² ΡΠΎΠΌ ΡΠΈΡΠ»Π΅
Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄Π°ΠΌΠΈ ΠΎΠΊΠΎΠ»ΠΎ 4 ΠΈ 11 Π»Π΅Ρ, ΠΏΠΎΡΠ»Π΅Π΄Π½ΠΈΠΉ ΡΠΎΠΎΡΠ²Π΅ΡΡΡΠ²ΡΠ΅Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄Ρ ΡΠΈΠΊΠ»Π° ΡΠΎΠ»Π½Π΅ΡΠ½ΠΎΠΉ
Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ. ΠΠΎΡΠ²Π»Π΅Π½ΠΈΠ΅ ΡΠΈΠΊΠ»Π° Ρ ΠΏΠ΅ΡΠΈΠΎΠ΄ΠΎΠΌ 4 Π³ΠΎΠ΄Π° Π² Π½Π°ΠΉΠ΄Π΅Π½Π½ΡΡ
Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΡ
ΠΎΠ±ΡΡΡΠ½ΡΠ΅ΡΡΡ
ΡΡΡΠ΅ΡΡΠ²ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΏΠΎΠ΄ΠΎΠ±Π½ΡΡ
ΡΠΈΠΊΠ»ΠΎΠ² Π² Ρ
ΡΠΎΠ½ΠΎΠ»ΠΎΠ³ΠΈΡΡ
ΡΠ΅ΠΌΠΏΠ΅ΡΠ°ΡΡΡ ΠΈ ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π° ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠ΅
Π²Π°ΡΠΈΠ°ΡΠΈΠΈ ΡΠ΅Π³ΠΈΡΡΡΠΈΡΡΠ΅ΠΌΠΎΠ³ΠΎ Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
Π‘Π2 ΠΌΠΎΠΆΠ½ΠΎ ΡΡΠΈΡΠ°ΡΡ ΡΠ΅Π°ΠΊΡΠΈΠ΅ΠΉ ΡΠ°ΡΡΠ΅Π½ΠΈΡ Π½Π° ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅
ΠΊΠ»ΠΈΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΡΡΠ»ΠΎΠ²ΠΈΠΉ. ΠΠ· ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½Π½ΠΎΠΉ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΎΠΉ Π²Π°ΡΠΈΠ°ΡΠΈΠΈ Π΄Π°Π²Π»Π΅Π½ΠΈΡ ΠΈ Π‘Π2 Π² ΠΊΠΎΠ»ΡΡΠ°Ρ
ΡΠΏΠΈΠ»ΠΎΠ² ΡΡΠ²ΠΎΠ»ΠΎΠ² ΠΈ ΠΊΠΎΡΠ½Π΅ΠΉ Π΄Π΅ΡΠ΅Π²ΡΠ΅Π² ΡΠ»Π΅Π΄ΡΠ΅Ρ, ΡΡΠΎ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΠ΅ Π² Π°ΡΠΌΠΎΡΡΠ΅ΡΡ Π‘Π2 Π΄ΠΎΠ»ΠΆΠ½ΠΎ Π½ΠΎΡΠΈΡΡ
ΡΠ°ΠΊΠΆΠ΅ ΡΠΈΠΊΠ»ΠΈΡΠ΅ΡΠΊΠΈΠΉ Ρ
Π°ΡΠ°ΠΊΡΠ΅Ρ, ΠΏΠΎΡΡΠΎΠΌΡ Π΄Π»Ρ ΠΊΠΎΡΡΠ΅ΠΊΡΠ½ΠΎΠΉ ΠΎΡΠ΅Π½ΠΊΠΈ Π²ΡΠ΄Π΅Π»Π΅Π½ΠΈΡ Π‘Π2 ΡΡΠ²ΠΎΠ»Π°ΠΌΠΈ ΠΈ
ΠΊΡΡΠΏΠ½ΡΠΌΠΈ ΠΊΠΎΡΠ½ΡΠΌΠΈ ΡΠ»Π΅Π΄ΡΠ΅Ρ ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΡΡ Π΄Π»ΠΈΡΠ΅Π»ΡΠ½ΡΠ΅ ΠΈΠ·ΠΌΠ΅ΡΠ΅Π½ΠΈ
TMC125 exerts similar initial antiviral potency as a five-drug, triple class antiretroviral regimen
Objective: TMC125, a next generation, non-nucleoside reverse transcriptase inhibitor (NNRTI), demonstrated a remarkable decline of plasma HIV-1 RNA during a phase IIa study. We compared the initial rate of decline of plasma HIV-1 RNA achieved by TMC125 monotherapy with that of a triple class, five-drug regimen, containing drugs from all three currently licensed classes (zidovudine, lamivudine, abacavir, indinavir and nevirapine). Methods: The decline in plasma HIV-1 RNA of 12 HIV-1 infected, antiretroviral (ART) naive patients treated for 1 week with TMC125 monotherapy was compared with that observed in the ERA study (n = 11). The plasma HIV-1 RNA elimination rate constant was calculated based on at least four plasma HIV-1 RNA measurements during the first week of treatment (first-order elimination) and compared using the Student's t test. Results: Median ages were 23 and 38 years for TMC125 and ERA patients, respectively (P = 0.001), median baseline plasma HIV-1 RNA levels were 4.2 and 4.8 log10 copies/ml (P = 0.001) and median baseline CD4 T-cell counts were 458 Γ 106 and 360 Γ 106 cells/l (P = 0.08). The median plasma HIV-1 RNA elimination rate constant was 0.68/day in TMC125 treated patients, and 0.56/day in ERA participants (P = 0.24). The median decline in plasma HIV-1 RNA after 7 days was 1.92 and 1.76 log 10 copies (P = 0.77) and the median increase of CD4 T cells was 119 Γ 106 and 60 Γ 106 cells/l, respectively (P = 0.29). Conclusion: Monotherapy with TMC125 in ART-naive, HIV-1-infected individuals resulted in a similar rate of decline of plasma HIV-1 RNA during 1 week of therapy as therapy with a five-drug regimen
TMC125 exerts similar initial antiviral potency as a five-drug, triple class antiretroviral regimen
Objective: TMC125, a next generation, non-nucleoside reverse transcriptase inhibitor (NNRTI), demonstrated a remarkable decline of plasma HIV-1 RNA during a phase IIa study. We compared the initial rate of decline of plasma HIV-1 RNA achieved by TMC125 monotherapy with that of a triple class, five-drug regimen, containing drugs from all three currently licensed classes (zidovudine, lamivudine, abacavir, indinavir and nevirapine). Methods: The decline in plasma HIV-1 RNA of 12 HIV-1 infected, antiretroviral (ART) naive patients treated for 1 week with TMC125 monotherapy was compared with that observed in the ERA study (n = 11). The plasma HIV-1 RNA elimination rate constant was calculated based on at least four plasma HIV-1 RNA measurements during the first week of treatment (first-order elimination) and compared using the Student's t test. Results: Median ages were 23 and 38 years for TMC125 and ERA patients, respectively (P = 0.001), median baseline plasma HIV-1 RNA levels were 4.2 and 4.8 log(10) copies/ml (P = 0.001) and median baseline CD4 T-cell counts were 458 X 10(6) and 360 X 10(6) cells/l (P = 0.08). The median plasma HIV-1 RNA elimination rate constant was 0.68/day in TMC125 treated patients, and 0.56/day in ERA participants (P = 0.24). The median decline in plasma HIV-1 RNA after 7 days was 1.92 and 1.76 log(10) copies (P = 0.77) and the median increase of CD4 T cells was 119 X 10(6) and 60 X 106 cells/l, respectively (P = 0.29). Conclusion: Monotherapy with TMC125 in ART-naive, HIV-1-infected individuals resulted in a similar rate of decline of plasma HIV-1 RNA during 1 week of therapy as therapy with a five-drug regimen. (C) 2003 Lippincott Williams Wilkin
Occurrences of Threatened Species included in the Third Edition of the Red Data Book of the Komi Republic (Russia)
The purpose of the data paper was to introduce into scientific literature the results of scientific work carried out for the third edition of the 'Red Data Book of the Komi Republic'. The article reflects methodological approaches to the formation of a list of rare and in need of protection species and describes the corresponding datasets published in GBIF.Information about 7,187 occurrences of 438 rare species and infraspecies included in the third edition of the 'Red Data Book of the Komi Republic' have been published