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@ARTICLE{Neues:140148,
      author       = {Neues, F. and Hild, S. and Epple, M. and Marti, O. and
                      Ziegler, A. and DESY},
      title        = {{A}morphous and crystalline calcium carbonate distribution
                      in the tergite cuticle of moulting {P}orcellio scaber
                      ({I}sopoda, {C}rustacea)},
      journal      = {Journal of structural biology},
      volume       = {175},
      issn         = {1047-8477},
      address      = {San Diego, Calif.},
      publisher    = {Elsevier},
      reportid     = {PHPPUBDB-24461},
      pages        = {10-20},
      year         = {2011},
      abstract     = {The main mineral components of the isopod cuticle consists
                      of crystalline magnesium calcite and amorphous calcium
                      carbonate. During moulting isopods moult first the posterior
                      and then the anterior half of the body. In terrestrial
                      species calcium carbonate is subject to resorption, storage
                      and recycling in order to retain significant fractions of
                      the mineral during the moulting cycle. We used synchrotron
                      X-ray powder diffraction, elemental analysis and Raman
                      spectroscopy to quantify the ACC/calcite ratio, the mineral
                      phase distribution and the composition within the anterior
                      and posterior tergite cuticle during eight different stages
                      of the moulting cycle of Porcellio scaber. The results show
                      that most of the amorphous calcium carbonate (ACC) is
                      resorbed from the cuticle, whereas calcite remains in the
                      old cuticle and is shed during moulting. During premoult
                      resorption of ACC from the posterior cuticle is accompanied
                      by an increase within the anterior tergites, and
                      mineralization of the new posterior cuticle by resorption of
                      mineral from the anterior cuticle. This suggests that one
                      reason for using ACC in cuticle mineralization is to
                      facilitate resorption and recycling of cuticular calcium
                      carbonate. Furthermore we show that ACC precedes the
                      formation of calcite in distal layers of the tergite
                      cuticle.},
      keywords     = {Animal Structures: chemistry / Animal Structures:
                      metabolism / Animal Structures: ultrastructure / Animals /
                      Calcification, Physiologic / Calcium Carbonate: chemistry /
                      Calcium Carbonate: metabolism / Isopoda: chemistry /
                      Isopoda: metabolism / Isopoda: ultrastructure / Microscopy,
                      Electron, Scanning / Molting / Powder Diffraction / Spectrum
                      Analysis, Raman / X-Ray Diffraction / Calcium Carbonate (NLM
                      Chemicals)},
      cin          = {EMBL},
      ddc          = {540},
      cid          = {$I:(DE-H253)EMBL_-2012_-20130307$},
      pnm          = {DORIS Beamline B2 (POF2-54G13)},
      pid          = {G:(DE-H253)POF2-B2-20130405},
      experiment   = {EXP:(DE-H253)D-B2-20150101},
      typ          = {PUB:(DE-HGF)16},
      pubmed       = {pmid:21458575},
      UT           = {WOS:000291371800002},
      doi          = {10.1016/j.jsb.2011.03.019},
      url          = {https://bib-pubdb1.desy.de/record/140148},
}