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Kupper, H.

Publications and source records attributed to Kupper, H..

3 recordsLinked to original sources

Gain and loss of gene function shaped the nickel hyperaccumulation trait in Noccaea caerulescens

Nickel hyperaccumulation is an extreme adaptation to ultramafic soils observed in more than 500 plant species. However, our understanding of the molecular mechanisms underlying the evolution of this trait remains limited. To shed light on these mechanisms, we have generated a high-quality genome assembly of the metal hyperaccumulator Noccaea caerulescens. We then used this genome as reference to conduct comparative intraspecific and interspecific transcriptomic analyses using various accessions of N. caerulescens and the non-accumulating relative Microthlaspi perfoliatum, to identify genes associated with nickel hyperaccumulation. Our results suggest a correlation between nickel hyperaccumulation and a decrease in the expression of genes involved in defense responses and the regulation of membrane trafficking. Surprisingly, these analyses did not reveal a significant enrichment of genes involved in the regulation of metal homeostasis. However, we found that the expression levels of selected metal transporters, namely NcHMA3, NcHMA4 and NcIREG2, is consistently elevated in N. caerulescens accessions hyperaccumulating nickel. Furthermore, our analyses identified frameshift mutations in NcIRT1 associated with the loss of nickel hyperaccumulation in a few accessions. We further showed that the expression of a functional NcIRT1 in roots of the La Calamine accession increases nickel accumulation in shoots. Our results demonstrate that NcIRT1 participate in nickel hyperaccumulation in N. caerulescens. They also suggest that nickel hyperaccumulation is an ancient trait in N. caerulescens that has evolved from the high and constitutive expression of few metal transporters including NcIREG2 and that the trait was subsequently lost in a few accessions due to mutations in NcIRT1.

plant biology↗

Nodule-specific Cu+-chaperone NCC1 is required for symbiotic nitrogen fixation in Medicago truncatula root nodules

Cu+-chaperones are a diverse group of proteins that allocate Cu+ ions to specific copper-proteins, creating different copper pools targeted to specific physiological processes. Symbiotic nitrogen fixation carried out in legume root nodules indirectly requires relatively large amounts of copper e.g. for energy delivery via respiration, for which targeted copper deliver systems would be required. MtNCC1 is a nodule-specific Cu+-chaperone encoded in the Medicago truncatula genome, with a N-terminus Atx1-like domain that can bind Cu+ with picomolar affinities. This gene is expressed primarily from the late infection zone to the early fixation zone, and is located in the cytosol, associated to plasma and symbiosome membranes, and within nuclei. Consistent with its key role in nitrogen fixation, ncc1 mutants have a severe reduction of nitrogenase activity, and a 50% reduction in copper-dependent cytochrome c oxidase activity. A subset of the copper-proteome is also affected in the mutant nodules. Many of these proteins can be pulled-down when using a Cu+-loaded N-terminal MtNCC1 moiety as a bait, indicating a role in nodule copper homeostasis and in copper-dependent physiological processes. Overall, these data suggest a pleiotropic role of MtNCC1 in copper delivery for symbiotic nitrogen fixation.

plant biology↗

Massive accumulation of strontium and barium in diplonemid protists

Barium (Ba) and strontium (Sr) are often used as proxies for the reconstruction of past marine productivity and global climate. The ability to accumulate Ba2+ and Sr2+ in the form of crystals is rare among eukaryotes. Here we report that unicellular heterotrophs called diplonemids (Euglenozoa), one of the most abundant groups of marine planktonic protists, accumulate conspicuous amounts of these trace elements in the form of intracellular barite (BaSO4) and celestite (SrSO4) crystals, in concentrations greater than in other known Ba/Sr-accumulating organisms. Moreover, these flagellates can uptake Sr2+ exclusively or together with Ba2+ and form (Ba,Sr)SO4. One species, Namystinia karyoxenos, is naturally capable of intracellular accumulation of Ba2+ and Sr2+ 42,000 and 10,000 times relative to the surrounding medium. Altering the amounts of both elements in the medium resulted in corresponding changes in the quantity and composition of crystals. Planktonic copepods fed with diplonemids produce celestite-rich fecal pellets, which facilitate deposition of these minerals on the seafloor. We propose that diplonemids, which emerged during the Neoproterozoic era, qualify as impactful players of Ba2+/Sr2+ cycling in the ocean that possibly contributed to sedimentary rock formation over long geological periods.

microbiology↗