scholarly journals Effects of soil temperature on gas exchange and mor- phological structure of shoot and root in 1 yr old Scots pine (Pinus sylvestris L.) seedlings

1989 ◽  
Vol 46 (Supplement) ◽  
pp. 459s-463s ◽  
Author(s):  
J. Lippu ◽  
P. Puttonen
1999 ◽  
Vol 26 (3) ◽  
pp. 239 ◽  
Author(s):  
Pertti Hari ◽  
Annikki Mäkelä ◽  
Frank Berninger ◽  
Toivo Pohja

The ‘optimality hypothesis’ of gas exchange in plants has been studied since the 1970s, but testing it in the field has proven difficult. A recent reformulation of the hypothesis with detailing assumptions on leaf structure makes it possible to solve the optimisation problem explicitly, such that the predictions of gas exchange are readily testable against field data. This form of the model was tested against field measurements of photosynthesis, transpiration and stomatal conductance in Scots pine (Pinus sylvestris) shoots during three clear summer days. Model parameters were estimated independently from photosynthesis measurements on preceding days. The measurements were carried out at a new field measurement station with a very low level of noise. The predictions of photosynthesis, transpiration andstomatal conductance explained 84–98% of the variance in the data.


2017 ◽  
Vol 47 (4) ◽  
pp. 488-499 ◽  
Author(s):  
Minna Kivimäenpää ◽  
Sirkka Sutinen ◽  
Hanna Valolahti ◽  
Elina Häikiö ◽  
Johanna Riikonen ◽  
...  

Acclimation of conifer needle anatomy to climate change is poorly understood. We studied needle anatomy, shoot gas exchange, current-year shoot length, and stem diameter growth in Norway spruce (Picea abies (L.) Karst.) and Scots pine (Pinus sylvestris L.) seedlings exposed to elevated ozone (1.35× to 1.5× ambient concentration) and elevated temperature (0.9–1.3 °C + ambient temperature) alone and in combination for two exposure seasons in two separate open-field experiments in central Finland. Pines grew also at two soil nitrogen levels. In spruce, warming increased mesophyll intercellular space and reduced gas exchange and shoot growth and made needles narrower and the epidermis and hypodermis thinner. In pine, warming made needles bigger, increased shoot and stem growth, stomatal row number, and proportions of vascular cylinder, phloem, and xylem and reduced the proportion of mesophyll. These responses indicate that pine benefited and spruce suffered from moderate warming. Ozone caused a thickening of epi- and hypo-dermis and a lower stomatal conductance in both species, reduced stomatal density in spruce, and increased proportions of phloem, xylem, and sclerenchyma and reduced growth in pine. Ozone responses suggest increased oxidative stress defense. Stomatal responses were affected by interactions of elevated temperature and ozone in both species. Nitrogen availability modified ozone and temperature responses, particularly in the vascular tissues in pine.


1998 ◽  
Vol 28 (6) ◽  
pp. 946-950 ◽  
Author(s):  
Marja-Liisa Sutinen ◽  
Aulis Ritari ◽  
Teuvo Holappa ◽  
Kauko Kujala

The seasonal changes in soil temperature and in the frost hardiness of adult Scots pine (Pinus sylvestris L.) trees was studied between September 1991 and February 1993 in a pine forest located in Finnish Lapland. Air and soil (humus layer and 5 cm depth of mineral soil) temperatures were measured continuously every second hour. The frost hardiness of the roots in the humus layer and in the mineral soil (down to 10 cm) was measured by means of the electrolyte-leakage method. The temperature in the humus layer varied between 21.2°C and –3.2°C and in the mineral soil between 21.6°C and –2.4°C. The temperature in the humus layer was continuously slightly colder than in the mineral soil from late August until May. The frost hardiness of the pine roots was lowest (about –5°C) in May and during the first week of September. Frost hardiness stayed at its maximum of about –20°C during November and December and slightly decreased in January and February. During most of the sampling time, the frost hardiness of the roots in the humus layer was greater than in the mineral soil. There was a clear relationship between the soil temperature and the frost hardiness of roots.


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