Rhizome, Root/Sediment interactions, Aerenchyma and Internal Pressure Changes in Seagrasses

TY - CHAP

T1 - Rhizome, Root/Sediment interactions, Aerenchyma and Internal Pressure Changes in Seagrasses

AU - Brodersen, Kasper Elgetti

AU - Kühl, Michael

AU - Nielsen, Daniel Aagren

AU - Pedersen, Ole

AU - Larkum, Anthony W. D.

PY - 2018/7/27

Y1 - 2018/7/27

N2 - Life in seawater presents several challenges for seagrasses owing to low O 2 and CO 2 solubility and slow gas diffusion rates. Seagrasses have evolved numerous adaptations to these environmental conditions including porous tissue providing low-resistance internal gas channels (aerenchyma) and carbon concentration mechanisms involving the enzyme carbonic anhydrase. Moreover, seagrasses grow in reduced, anoxic sediments, and aerobic metabolism in roots and rhizomes therefore has to be sustained via rapid O 2 transport through the aerenchyma. Tissue aeration is driven by internal concentration gradients between leaves and belowground tissues, where the leaves are the source of O 2 and the rhizomes and roots function as O 2 sinks. Inadequate internal aeration e.g., due to low O 2 availability in the surrounding water during night time, can lead to sulphide intrusion into roots and rhizomes, which has been linked to enhanced seagrass mortality. Under favourable conditions, however, seagrasses leak O 2 and dissolved organic carbon into the rhizosphere, where it maintains oxic microzones protecting the plant against reduced phytotoxic compounds and generates dynamic chemical microgradients that modulate the rhizosphere microenvironment. Local radial O 2 loss from belowground tissues of seagrasses leads to sulphide oxidation in the rhizosphere, which generates protons and results in local acidification. Such low-pH microniches can lead to dissolution of carbonates and protolytic phosphorus solubilisation in carbonate-rich sediments. The seagrass rhizosphere is also characterised by numerous high-pH microniches indicative of local stimulation of proton consuming microbial processes such as sulphate reduction via root/rhizome exudates and/or release of alkaline substances. High sediment pH shifts the sulphide speciation away from H 2 S towards non-tissue-penetrating HS - ions, which can alleviate the belowground tissue exposure to phytotoxic H 2 S. High sulphide production can also lead to iron and phosphorus mobilization through sulphide-induced reduction of insoluble Fe(III)oxyhydroxides to dissolved Fe(II) with concomitant phosphorus release to the porewater. Adequate internal tissue aeration is thus of vital importance for seagrasses as it ensures aerobic metabolism in distal parts of the roots and provides protection against intrusion of phytotoxins from the surrounding sediment.

AB - Life in seawater presents several challenges for seagrasses owing to low O 2 and CO 2 solubility and slow gas diffusion rates. Seagrasses have evolved numerous adaptations to these environmental conditions including porous tissue providing low-resistance internal gas channels (aerenchyma) and carbon concentration mechanisms involving the enzyme carbonic anhydrase. Moreover, seagrasses grow in reduced, anoxic sediments, and aerobic metabolism in roots and rhizomes therefore has to be sustained via rapid O 2 transport through the aerenchyma. Tissue aeration is driven by internal concentration gradients between leaves and belowground tissues, where the leaves are the source of O 2 and the rhizomes and roots function as O 2 sinks. Inadequate internal aeration e.g., due to low O 2 availability in the surrounding water during night time, can lead to sulphide intrusion into roots and rhizomes, which has been linked to enhanced seagrass mortality. Under favourable conditions, however, seagrasses leak O 2 and dissolved organic carbon into the rhizosphere, where it maintains oxic microzones protecting the plant against reduced phytotoxic compounds and generates dynamic chemical microgradients that modulate the rhizosphere microenvironment. Local radial O 2 loss from belowground tissues of seagrasses leads to sulphide oxidation in the rhizosphere, which generates protons and results in local acidification. Such low-pH microniches can lead to dissolution of carbonates and protolytic phosphorus solubilisation in carbonate-rich sediments. The seagrass rhizosphere is also characterised by numerous high-pH microniches indicative of local stimulation of proton consuming microbial processes such as sulphate reduction via root/rhizome exudates and/or release of alkaline substances. High sediment pH shifts the sulphide speciation away from H 2 S towards non-tissue-penetrating HS - ions, which can alleviate the belowground tissue exposure to phytotoxic H 2 S. High sulphide production can also lead to iron and phosphorus mobilization through sulphide-induced reduction of insoluble Fe(III)oxyhydroxides to dissolved Fe(II) with concomitant phosphorus release to the porewater. Adequate internal tissue aeration is thus of vital importance for seagrasses as it ensures aerobic metabolism in distal parts of the roots and provides protection against intrusion of phytotoxins from the surrounding sediment.

UR - https://doi.org/10.1007/978-3-319-71354-0

U2 - 10.1007/978-3-319-71354-0_13

DO - 10.1007/978-3-319-71354-0_13

M3 - Book chapter

SN - 978-3-319-71352-6

SP - 393

EP - 418

BT - Seagrasses of Australia

A2 - Larkum, Anthony W. D.

A2 - Kendrick, Gary A.

A2 - Ralph, Peter J.

PB - Springer

ER -