Botany

Summary

Botany, also called plant science (or plant sciences), plant biology or phytology, is the science of plant life and a branch of biology. A botanist, plant scientist or phytologist is a scientist who specialises in this field. The term "botany" comes from the Ancient Greek word βοτάνη (botanē) meaning "pasture", "herbs" "grass", or "fodder"; βοτάνη is in turn derived from βόσκειν (), "to feed" or "to graze". Traditionally, botany has also included the study of fungi and algae by mycologists and phycologists respectively, with the study of these three groups of organisms remaining within the sphere of interest of the International Botanical Congress. Nowadays, botanists (in the strict sense) study approximately 410,000 species of land plants of which some 391,000 species are vascular plants (including approximately 369,000 species of flowering plants), and approximately 20,000 are bryophytes. Botany originated in prehistory as herbalism with the efforts of early humans to identify –

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Biogenic silica production in selected alpine plant species and plant communities

The biogenic silica extracted from samples of 28 alpine plant species belonging to 23 genera and nine families collected in the Swiss Alps (Valais) accounted for between 0.01 and 5.9% of the dry biomass of leaves and wood. Silica content, and plant contribution to the soil biogenic silica pool, varied widely among taxa. Plant net productivity and biogenic silica production From this study and from the literature have been used to predict the input made by different subalpine and alpine plant communities to soil-borne phytolith assemblages, and their contribution to the silicon biocycle. (C) 2001 Annals of Botany Company.

2001

Microworlds for Ecology Explorations: From DigitalSeed to Biosphera in fostering children's understanding of plant biology

Mauro Cherubini

2004

Cutover peatlands cover large surfaces of high potential value for biodiversity and carbon sequestration function if successfully restored but the evaluation of restoration success is not straighforward. We assessed the bioindicator value of organic matter (OM), testate amoebae (protozoa) and bacteria in peat from two regeneration stages and a reference site of a cutover bog. 2. Contrasting biochemical signatures of peat OM were observed along the regenerating profiles allowing clear differentiation between the newly regenerated peat and the old peat. Where peat macrofossils were absent sugar biomarkers allowed to infer peat botanical origin and OM alteration. 3. Over the succession, the OM composition of the new peat differed: peat from the recent stage was more dominated by Sphagnum-derived tissues and was characterised by lesser carbohydrate preservation and higher bacterial biomass than the advanced regeneration stage. 4. Surface testate amoeba communities also changed from the recent to the advanced stages of regeneration indicating a shift from wet and moderately acidic conditions to drier and more acidic conditions. Over this regeneration sequence (i) biomass and average size of species declined but were higher in the unexploited site (ii) species richness and diversity increased but density declined. 5. Synthesis and applications. Although the secondary succession in the cutover bog leads to an ecosystem similar to that of the reference site in terms of surface vegetation, OM and testate amoebae continue to reflect disturbances associated with peat harvesting. Nevertheless, the described dynamics of both microbial and biochemical variables over the succession showed similarities between the advanced stage and the reference: a higher testate amoeba diversity is associated with better carbohydrate preservation and a more heterogeneous botanical composition of the peat. The quantitative inference of water table depth and pH based on testate amoebae indicators represents an alternative to labour-intensive repeated measurements in the field. Botanical and biochemical composition of peat OM provides additional information on past anthropogenic perturbations of the bog and can be used for restoration monitoring. The combination of several indicators therefore provides a more complete assessment of ecological conditions which could be valuable for the management of cutover peatlands.

2008

Cutover peatlands cover large surfaces of high potential value for biodiversity and carbon sequestration function if successfully restored but the evaluation of restoration success is not straighforward. We assessed the bioindicator value of organic matter (OM), testate amoebae (protozoa) and bacteria in peat from two regeneration stages and a reference site of a cutover bog. 2. Contrasting biochemical signatures of peat OM were observed along the regenerating profiles allowing clear differentiation between the newly regenerated peat and the old peat. Where peat macrofossils were absent sugar biomarkers allowed to infer peat botanical origin and OM alteration. 3. Over the succession, the OM composition of the new peat differed: peat from the recent stage was more dominated by Sphagnum-derived tissues and was characterised by lesser carbohydrate preservation and higher bacterial biomass than the advanced regeneration stage. 4. Surface testate amoeba communities also changed from the recent to the advanced stages of regeneration indicating a shift from wet and moderately acidic conditions to drier and more acidic conditions. Over this regeneration sequence (i) biomass and average size of species declined but were higher in the unexploited site (ii) species richness and diversity increased but density declined. 5. Synthesis and applications. Although the secondary succession in the cutover bog leads to an ecosystem similar to that of the reference site in terms of surface vegetation, OM and testate amoebae continue to reflect disturbances associated with peat harvesting. Nevertheless, the described dynamics of both microbial and biochemical variables over the succession showed similarities between the advanced stage and the reference: a higher testate amoeba diversity is associated with better carbohydrate preservation and a more heterogeneous botanical composition of the peat. The quantitative inference of water table depth and pH based on testate amoebae indicators represents an alternative to labour-intensive repeated measurements in the field. Botanical and biochemical composition of peat OM provides additional information on past anthropogenic perturbations of the bog and can be used for restoration monitoring. The combination of several indicators therefore provides a more complete assessment of ecological conditions which could be valuable for the management of cutover peatlands.

2008