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Stalagmites are known to record atmospheric sulphur loads and ecosystem dynamics in karst regions, thus expanding the inventory of trace element proxies extracted from speleothems to a level.

Whereas increasing temperatures in shallow waters may counteract the effect of ocean acidification on carbonate saturation states (Andersson et al., 2008), thermal stress due to ocean warming can.

Whereas increasing temperatures in shallow waters may counteract the effect of ocean acidification on carbonate saturation states (Andersson et al., 2008), thermal stress due to ocean warming can.

Stalagmites are known to record atmospheric sulphur loads and ecosystem dynamics in karst regions, thus expanding the inventory of trace element proxies extracted from speleothems to a level.

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The chemistry of natural waters varies both spatially and temporally and is controlled by factors such as atmospheric deposition, biological activity in soils, and chemical weathering of soils and.

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2007; McIntosh and Walter, 2005; Lemieux et al., 2008b). Some field measurements have also been conducted in Iceland, United States, Switzerland, and Canada using boreholes, piezometers, and electric.

Stem respiration has commonly been underestimated by measurements of stem CO 2 efflux to the atmosphere, as a portion of locally respired CO 2 is carried upward in the tree in the transpiration stream.

The chemistry of natural waters varies both spatially and temporally and is controlled by factors such as atmospheric deposition, biological activity in soils, and chemical weathering of soils and.

Later, similar research has been extended to PbTe-MgTe/ CaTe/BaTe (matrix-nanoprecipitate) system, where promising thermoelectric performances have also been achieved (Ohta et al., 2012; Lo et al.,

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2007; McIntosh and Walter, 2005; Lemieux et al., 2008b). Some field measurements have also been conducted in Iceland, United States, Switzerland, and Canada using boreholes, piezometers, and electric.

Stem respiration has commonly been underestimated by measurements of stem CO 2 efflux to the atmosphere, as a portion of locally respired CO 2 is carried upward in the tree in the transpiration stream.

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Later, similar research has been extended to PbTe-MgTe/ CaTe/BaTe (matrix-nanoprecipitate) system, where promising thermoelectric performances have also been achieved (Ohta et al., 2012; Lo et al.,