Genome sequence of dwarf birch (Betula nana) and cross-species RAD markers.

New sequencing technologies allow development of genome-wide markers for any genus of ecological interest, including plant genera such as Betula (birch) that have previously proved difficult to study due to widespread polyploidy and hybridization. We present a de novo reference genome sequence assembly, from 66× short read coverage, of Betula nana (dwarf birch) - a diploid that is the keystone woody species of subarctic scrub communities but of conservation concern in Britain. We also present 100 bp PstI RAD markers for B.

Metabolic adaptation to prolonged anoxia in leaves of American cranberry (Vaccinium macrocarpon).

The indigenous North American Cranberry (Vaccinium macrocarpon), when cultivated in specially constructed cranberry bogs, is normally flooded in winter to prevent frost injury. This protection under ice can give rise to prolonged periods of anoxia, which depending on the state of the vines and environmental conditions, can cause severe oxygen-deprivation injury. An experimental study of the tolerance of cranberry vines to controlled total anoxia reveals that mature dark-green perennating leaves with high carbohydrate levels are able to survive prolonged periods of total oxygen-deprivation while younger newly formed leaves are readily damaged.

The tundra-taiga interface and its dynamics: concepts and applications.

The tundra-taiga interface is a dominant vegetation boundary that is related to climate and has an importance at a global level for its contribution to land atmosphere interactions, biodiversity and land use. However, our understanding of the precise location, dynamics and characteristics of the boundary, and its environmental and biotic drivers at a circumpolar level is poor. Our understanding has been constrained for various reasons, perhaps including a quest by researchers to denote 2- or even 3-dimensional tree distribution limits to a single line on a map.

How will the tundra-taiga interface respond to climate change?

The intuitive and logical answer to the question of how the tundra-taiga interface will react to global warming is that it should move north and this is mirrored by many models of potential treeline migration. Northward movement may be the eventual outcome if climatic warming persists over centuries or millennia. However, closer examination of the tundra-taiga interface across its circumpolar extent reveals a more complex situation.

The dynamics of the tundra-taiga boundary: an overview and suggested coordinated and integrated approach to research.

The tundra-taiga boundary stretches for more than 13,400 km around the Northern Hemisphere and is probably the Earth's greatest vegetation transition. The trees that define the boundary have been sensitive to climate changes in the past and models of future vegetation distribution suggest a rapid and dramatic invasion of the tundra by the taiga. Such changes would generate both positive and negative feedbacks to the climate system and the balance could result in a net warming effect.