Temperate rainforest lichens in New Zealand: high thallus water content can severely limit photosynthetic CO2 exchange

Oecologia ◽  
1993 ◽  
Vol 95 (3) ◽  
pp. 303-313 ◽  
Author(s):  
O. L. Lange ◽  
B. B�del ◽  
U. Heber ◽  
A. Meyer ◽  
H. Zellner ◽  
...  
Keyword(s):  
New Zealand ◽  
Water Content ◽  
Co2 Exchange ◽  
Temperate Rainforest ◽  
Thallus Water Content

A Dielectric-Water Content Relationship for Sandy Volcanic Soils in New Zealand

1999 ◽  
Vol 63 (4) ◽  
pp. 777-781 ◽  
Author(s):  
M. D. Tomer ◽  
B. E. Clothier ◽  
I. Vogeler ◽  
S. Green
Keyword(s):  
New Zealand ◽  
Water Content ◽  
Volcanic Soils

Holocene to Middle Last Glaciation vegetation history at Tullabardine Dam, western Tasmania

1986 ◽  
Vol 229 (1255) ◽  
pp. 177-207 ◽  
Keyword(s):  
New Zealand ◽  
Lake Sediments ◽  
Pollen Analysis ◽  
Temperate Forest ◽  
Vegetation History ◽  
Late Glacial ◽  
Pollen Assemblage ◽  
Temperate Rainforest ◽  
Last Glaciation ◽  
Peat Swamp

Pollen analysis of 4 m of peat, swamp-soil and lake sediments dated from 0 to > 43800 years b.p. indicates the occurrence of three major pollen assemblage zones. During Zone 1 (11000-0 years b.p.) the area had temperate rainforest and the climate was warm, moist and interglacial. During Zone 2 ( ?25000-l 1000 years b.p.), correlated approximately with the last period of glaciation, the vegetation was mainly grassland and the climate was considerably colder than present. In late glacial times (14000-11000 years b.p.) pollen of shrub and tree taxa increased, especially during the later part of the period as the climate became warmer and moister. During Zone 3 (more than 4 3 0 0 0 -?25000 years b.p.) the vegetation was predominantly sub-alpine and alpine. This vegetation represents an interstadial assemblage for a lowland site. The climate was cool and moist. The results are compared with sites of similar age in Tasmania, and with sites from temperate forest environments in Chile and New Zealand.

Environmental and chemical factors regulating methane oxidation in a New Zealand forest soil

Soil Research ◽  
2004 ◽  
Vol 42 (7) ◽  
pp. 767 ◽  
Author(s):  
Sally J. Price ◽  
Francis M. Kelliher ◽  
Robert R. Sherlock ◽  
Kevin R. Tate ◽  
Leo M. Condron
Keyword(s):  
New Zealand ◽  
Water Content ◽  
Forest Soil ◽  
Oxidation Rate ◽  
Field Capacity ◽  
Soil Disturbance ◽  
Great Sensitivity ◽  
Ch4 Oxidation ◽  
Chemical Factors ◽  
Very High

Tropospheric methane (CH4) is oxidised by soil microbes called methanotrophs. We examined them in soil samples from a pristine Nothofagus forest located in New Zealand. Laboratory incubations indicated the presence of high-affinity methanotrophs that displayed Michaelis–Menton kinetics (Km = 8.4 µL/L where Km is the substrate concentration at half the maximal rate). When the soil was dried from its field capacity water content of 0.34 to 0.16 m3/m3, CH4 oxidation rate increased nearly 7-fold. The methanotrophs were thus metabolically poised for very high activity, but substrate availability was commonly limiting. When water content was held constant, CH4 oxidation rate nearly doubled as temperature increased from 5 to 12°C, a range found in the forest. By contrast, CH4 oxidation rate did not change much from 12 to 30°C, and it was zero at 35°C. When water content and temperature were held constant, the optimal soil pH for CH4 oxidation was 4.4, as found in the forest. Soil disturbance by nitrogen (N) and non-N salt amendment decreased CH4 oxidation rate, but this depended on the amendment species and concentration. The methanotrophs were adapted to native conditions and exhibited a great sensitivity to disturbance.

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