Carbon sink | EPFL Graph Search

A carbon sink is anything, natural or otherwise, that accumulates and stores some carbon-containing chemical compound for an indefinite period and thereby removes carbon dioxide () from the atmosphere. These sinks form an important part of the natural carbon cycle. An overarching term is carbon pool, which is all the places where carbon can be (the atmosphere, oceans, soil, plants, and so forth). A carbon sink is a type of carbon pool that has the capability to take up more carbon from the atmosphere than it releases. Globally, the two most important carbon sinks are vegetation and the ocean. Soil is an important carbon storage medium. Much of the organic carbon retained in the soil of agricultural areas has been depleted due to intensive farming. "Blue carbon" designates carbon that is fixed via the ocean ecosystems. Coastal blue carbon includes mangroves, salt marshes and seagrasses which make up a majority of ocean plant life and store large quantities of carbon. Deep blue carbo

Biogeochemical plant-soil microbe feedback in response to climate warming in peatlands

Richard David Bardgett, Luca Bragazza, Alexandre Buttler, Julien Parisod

Peatlands act as global sinks of atmospheric carbon (C) through the accumulation of organic matter(1), primarily made up of decay-resistant litter of peat mosses(2). However, climate warming has been shown to promote vascular plant growth in peatlands, especially ericaceous shrubs(3). A change in vegetation cover is in turn expected to modify above-ground/below-ground interactions(4), but the biogeochemical mechanisms involved remain unknown. Here, by selecting peatlands at different altitudes to simulate a natural gradient of soil temperature, we show that the expansion of ericaceous shrubs with warming is associated with an increase of polyphenol content in both plant litter and pore water. In turn, this retards the release of nitrogen (N) from decomposing litter, increases the amount of dissolved organic N and reduces N immobilization by soil microbes. A decrease of soil water content with increasing temperature promotes the growth of fungi, which feeds back positively on ericaceous shrubs by facilitating the symbiotic acquisition of dissolved organic N. We also observed a higher release of labile C from vascular plant roots at higher soil temperatures, which promotes the microbial investment in C-degrading enzymes. Our data suggest that climate-induced changes in plant cover can reduce the productivity of peat mosses and potentially prime the decomposition of organic matter by affecting the stoichiometry of soil enzymatic activity.

Nature Publishing Group2013

Phytoextraction of heavy metals by hyperaccumulating and non hyperaccumulating plants

Claudia Cosio

Although phytoextraction using hyperaccumulating plants is seen as a promising technique, a lack of understanding of the basic physiological, biochemical, and molecular mechanisms involved in heavy metal hyperaccumulation prevents the optimization of the phytoextraction technique and its further commercial application. The best-long term strategy for improving phytoextraction is therefore to understand and exploit the biological processes involved in metal acquisition, transport and shoot accumulation in plants. In order to compare Cd allocation in leaves and the role of the leaf cells in hyperaccumulating and non hyperaccumulating plants, we used a wide range of techniques and approaches on contrasting ecotypes of Thlaspi caerulescens, Arabidopsis halleri, Arabidopsis thaliana and one high biomass crop Salix viminalis. As a first step, the extent of hyperaccumulation and tolerance was studied in different plants. Five Swiss T. caerulescens populations were compared for their tolerance and Cd hyperaccumulation to two well studied populations: T. caerulescens Ganges (France) and T. caerulescens Prayon (Belgium). We showed that the behaviour of the populations in hydroponics was linked to the characteristics of their soil of origin. However, growing plants in hydroponics with 1 μM Cd seemed to be adequate to discriminate the various populations tested for hyperaccumulation. Cadmium effect on morphological parameters and Cd accumulation in S. viminalis leaves was also monitored. Salix viminalis was surprisingly tolerant to Cd and high Cd concentration in shoots. Because it may give an indication of the tolerance mechanisms employed by the different plants, we studied the general Cd allocation in leaves of hyperaccumulating (Ganges) and non-hyperaccumulating plants (Prayon, S. viminalis). Surprinsingly, when grown in hydroponics the only differences found between Prayon and Ganges at the leaf level was concentration of Cd found in the storage sinks. Results also showed similarities between T. caerulescens and S. viminalis in Cd storage, although the Cd concentrations found in leaves differed greatly. Both point-like accumulation and accumulation at the edges of the leaves were observed. A link could be established with visible symptoms (necrosis). At last differences in Cd localization between young and mature leaves were observed. These differences were attributed to physiological differences between leaves. Salix viminalis and T. caerulescens were both able to reduce Cd toxicity by allocating Cd in less sensitive tissues. Cadmium was found inside the cells and in the cell walls of the leaves of T. caerulescens, but mainly in cell walls and to a lesser extent in the symplasm in S. viminalis. Metal allocation in both plants indicated that the plant general growth strategy governed metal accumulation. We further investigated the role of the leaf cells in allocating Cd in leaves of Ganges, A. halleri and Prayon by characterizing Cd uptake in mesophyll protoplasts. Results indicated that differences in metal uptake could not be explained by different constitutive transport capacities at the leaf protoplast level. However, pre-exposure of the plants to Cd induced an increase in Cd accumulation in protoplasts of Ganges, whereas it decreased Cd accumulation in A. halleri protoplasts. The experiment with competitors eventually showed that probably more than one single transport system are carrying Cd in parallel into the cell. Metal allocation indicates that the principle of metal storage in metabolically less sensitive plant parts governs metal accumulation. Vacuolar compartmentalization and cell wall binding in leaves could therefore both play a role in accumulation of heavy metals. Based on these various results, we suggested that metal storage in plant demands the involvement of more than one compartment. Further work is however needed to assess many steps of the trafficking of metals that remain enigmatic.

EPFL2004

Linking soil microbial communities to vascular plant abundance along a climate gradient

Richard David Bardgett, Luca Bragazza, Alexandre Buttler, Edward Mitchell

The ongoing expansion of shrub cover in response to climate change represents a unique opportunity to explore the link between soil microbial communities and vegetation changes. This link is particularly important in peatlands where shrub expansion is expected to feed back negatively on the carbon sink capacity of these ecosystems. Microbial community structure and function were measured seasonally in four peatlands located along an altitude gradient representing a natural gradient of climate and associated vascular plant abundance. We show that increased soil temperature and reduced water content are associated with greater vascular plant biomass, in particular that of ericoids, and that this, in turn, is correlated with greater microbial biomass. More specifically, microbial community structure is characterized by an increasing dominance of fungi over bacteria with improved soil oxygenation. We also found that the carbon and nitrogen stoichiometry of microbial biomass differs in relation to soil microbial community structure and that this is ultimately associated with a different investment in extracellular enzymatic activity. Our findings highlight the fact that the determination of the structural identity of microbial communities can help to explain the biogeochemical dynamics of organic matter and provide a better understanding of ecosystem response to environmental changes.

Wiley-Blackwell2015

Phytoextraction of heavy metals by hyperaccumulating and non hyperaccumulating plants

Claudia Cosio

EPFL2004