Tài liệu Báo cáo Y học: Soluble silk-like organic matrix in the nacreous layer of the bivalve Pinctada maxima A new insight in the biomineralization field pptx
Solublesilk-likeorganicmatrixinthenacreouslayerofthe bivalve
Pinctada maxima
A newinsightinthebiomineralization field
Lucilia Pereira-Mourie
`
s
1
, Maria-Jose
´
Almeida
1,3
, Cristina Ribeiro
3
, Jean Peduzzi
2
, Michel Barthe
´
lemy
2
,
Christian Milet
1
and Evelyne Lopez
1
1
Laboratoire de Physiologie Ge
´
ne
´
rale et Compare
´
e, UMR CNRS 8572, Muse
´
um National d’Histoire Naturelle, Paris, France;
2
Laboratoire de Chimie des Substances Naturelles, ESA CNRS 8041, Muse
´
um National d’Histoire Naturelle, Paris, France;
3
INEB – Instituto de Engenharia Biome
´
dica, Rua do Campo Alegre, Porto, Portugal
Nacre organicmatrix has been conventionally classified as
both Ôwater-solubleÕ and Ôwater-insolubleÕ,basedonits
solubility in aqueous solutions after decalcification with acid
or EDTA. Some characteristics (aspartic acid-rich, silk-
fibroin-like content) were specifically attributed to either one
or the other. The comparative study on the technique of
extraction (extraction with water alone vs. demineralization
with EDTA) presented here, seems to reveal that this gen-
erally accepted classification may need to be reconsidered.
Actually, the nondecalcified solubleorganic matrix, extrac-
ted in ultra-pure water, displays many ofthe characteristics
of what until now has been called Ôinsoluble matrixÕ.We
present the results obtained on this extract and on a
conventional EDTA-soluble matrix, with various charac-
terization methods: fractionation by size-exclusion and
anion-exchange HPLC, amino acid analysis, glycosami-
noglycan and calcium quantification, SDS/PAGE and
FTIR spectroscopy. We propose that the model for the
interlamellar matrix sheets of nacre given by Nakahara [In:
Biomineralization and Biological Metal Accumulation,
Westbroek, P. & deJong, E.W., eds, (1983) pp. 225–230.
Reidel, Dordrecht, Holland] and Weiner and Traub
[Phil.Trans.R.Soc.Lond.B(1984) 304, 425–434] may no
longer be valid. The most recent model, proposed by
Levi-Kalisman et al.[J. Struct. Biol. (2001) 135, 8–17],
seemed to be more in accordance with our findings.
Keywords: nacre; undecalcified soluble matrix; EDTA-
soluble matrix; hydrophobicity; silk-fibroin-like-proteins.
In thebiomineralization field, the mollusk shell is one of
the best studied of all calcium carbonate biominerals.
Particular attention has been given to theorganic matrix
[1–5]. The latter is thought to promote the nucleation of
the mineral component, to direct the crystal growth and to
act as glue, preventing fracture ofthe shell [6–9]. The main
biopolymers present intheorganicmatrix are essentially
proteins, either glycosylated or not, acidic polysaccharides
and chitin. In nacre, they represent 1–5% (w/w) of the
structure.
From the earliest experiments, it was believed that the
biochemical properties ofmatrix constituents depend of
the use ofa decalcification procedure for removing the
mineral component, which is strongly associated with the
organic matrix [1,3]. Therefore, all investigations up until
now used either EDTA, acetic acid or hydrochloric acid
for this demineralization step and, subsequently, two
fractions oftheorganicmatrix were separated, based on
their solubility in aqueous solutions. Accordingly, a
designation ofmatrix into two classes, thesoluble matrix
and the insoluble matrix, has evolved from this extraction
[10–14].
This paper presents for the first time the results of a
comparative study on theorganicmatrix extracted from
the nacreouslayerofthe shell from the pearl oyster
Pinctada maxima by two very different methods. The first
is a nondecalcifying technique obtained by an extraction in
ultra-pure water. This unconventional approach arises
from previous in vivo and in vitro experiments where we
showed that biochemical signals from nacre chips were able
to diffuse inthe surrounding media and to induce new
bone formation [15–22]. In an attempt to identify these
signal molecules, we have previously perfected this original
method of extraction oftheorganic matrix, without any
acid treatment or demineralization, in order to minimize
any possible alteration ofthe activity ofthe macromole-
cules [20,23]. The second method is one ofthe widely used
extraction techniques which involves a demineralization
with EDTA followed by intensive dialysis against distilled
water. The content ofthe respective solublematrix extracts
were very different and seemed to raise important
questions about the actual conventional classification of
the soluble (known as acidic and aspartic acid-rich) and
insoluble (said to be hydrophobic and glycine, alanine-rich)
matrices and on the current model of nacre organic matrix
organization.
Correspondence to E. Lopez, Laboratoire de Physiologie Ge
´
ne
´
rale
et Compare
´
e, UMR CNRS 8572, Muse
´
um National d’Histoire
Naturelle, 7 rue Cuvier, 75231, Paris Cedex 05, France.
Fax: +33 1 40795620, Tel: +33 1 40793622,
E-mail: lopez@mnhn.fr
Abbreviations:EDTA-IM,EDTA-insolublematrix;EDTA-SM,
EDTA-soluble matrix; GAG, glycosaminoglycan; PG, proteoglycan;
WIM, water-insoluble matrix; WSM, water-soluble matrix.
(Received 22 April 2002, revised 16 August 2002,
accepted 23 August 2002)
Eur. J. Biochem. 269, 4994–5003 (2002) Ó FEBS 2002 doi:10.1046/j.1432-1033.2002.03203.x
MATERIALS AND METHODS
Organic matrix extraction
The powdered nacre (particle size 50–150 lm), obtained
from the inner shell layerofthe pearl oyster P. maxima,was
extracted by either ultra-pure water or EDTA and then
fractionated into soluble and insoluble matrix by centrifu-
gation. Demineralization of powdered nacre with EDTA
was performed as described by Wheeler et al.[24].Fifty
grams of powdered nacre was dissolved in 100 mL 10%
EDTA disodium salt dihydrate, pH 8, with continuous
stirring for 24 h at room temperature. Then, the suspension
was transferred ina dialysis bag (Spectrapor 2, 12–14 kDa
molecular weight cut-off) and placed in 2 L ofthe same
EDTA solution (replaced by fresh solution every 12 h), with
stirring and at 4 °C, until the powdered shell was completely
demineralized (about 3 days). The extract was centrifuged at
27 000 g for 30 min to separate the EDTA-soluble matrix
(EDTA-SM) from the EDTA-insoluble matrix (EDTA-
IM).ToremoveEDTA,thetwosampleswereextensively
dialyzed against ultra-pure water (Milli-Q
TM
), at 4 °C, and
the EDTA-SM was freeze-dried. The water-soluble matrix
(WSM) was obtained as described in Almeida et al.[20].
Fractionation ofsoluble extracts by HPLC
The WSM and the EDTA-SM were separated by size-
exclusion high performance liquid chromatography
(SE-HPLC), and by anion-exchange HPLC (AE-HPLC),
as described elsewhere [20].
For the SE-HPLC, a solution of 30 mg (dry
weight)ÆmL
)1
was prepared for the two soluble extracts
and filtered through a 0.22 lm centrifuge tube filter (Spin-
XÒ, Costar) before injection. Aliquots of WSM (500 lL) or
EDTA-SM (250 lL) were injected onto the preparative
column. Proteins were eluted with ultra-pure water rather
than with a salt buffer in order to preserve the integrity of
the macromolecules [20,21].
Amino acid analysis
Samples of proteins were hydrolyzed at 110 °C under
vacuum with 6
M
HCl constant boiling (Sigma) for 24 h.
Phosphoserine was determined from hydrolysis in 4
M
HCl
for 6 h [25]. The resulting amino acids were separated on a
cation exchange PC6A resin (Pierce) and the o-phthaldial-
dehyde derivatives of amino acids were detected with a
Waters 420 fluorimeter. Proline, hydroxyproline and
hydroxylysine were examined at 254 nm by reverse-phase
HPLC of their phenylisothiocarbamate derivatives [26], as
reported previously [20]. The serine, threonine and tyrosine
contents ofthe hydrolysates were corrected for destruction
during the hydrolysis by extrapolation to zero time hydro-
lysis. The amino acid compositions, expressed as a mole
percent, represent the average of at least three independent
determinations. The amount of protein in each extract was
calculated from the amino acids’ molar yields.
Glycosaminoglycan analysis
Organic matrix samples were dissolved in 5 mL of 0.1
M
NaOH [27] at room temperature for 24 h with periodic
mixing and maceration, followed by centrifugation at
1000 g for 10 min. Sulfated and nonsulfated glycosamino-
glycans (GAGs) from the supernatant were estimated by the
Whiteman Alcian blue binding technique [28,29], using
chondroitin sulfate as standard. The assay was adapted to
the estimation of GAG in more dilute samples by increasing
the aliquot size, as proposed by Gold [30].
Calcium analysis
Calcium analyses were performed after nitric acid hydrolysis
of samples, by atomic absorption spectrophotometry, using
a GBC 904AA spectrophotometer.
Fourier transform infrared (FTIR) spectroscopy
Organic compounds binding groups from soluble matrix
samples were detected by FTIR spectrometry. The FTIR
spectra were obtained using a Perkin Elmer 200FTIR
spectrometer. All the samples were prepared as KBr discs
and were run at a spectral resolution of 4 cm
)1
.One
hundred scans were acquired for each sample.
Polyacrylamide gel electrophoresis
The proteins from thesoluble samples were separated under
denaturating conditions (30 lg total protein per well) by
SDS/PAGE [31] using 12% polyacrylamide mini-gels (Mini
Protean III apparatus, Bio-Rad) of 0.75 mm thickness.
After electrophoresis, proteins were visualized by silver-
staining, as described by Morrissey [32], without the
glutaraldehyde step. The molecular masses were estimated
using the Amersham Pharmacia Biotech LMW-SDS
marker kit for electrophoresis.
RESULTS
Extraction ofsoluble matrix
After extraction and lyophilization, the two soluble extracts
(WSM and EDTA-SM) were re-suspended in ultra-pure
water for protein analysis. The protein recovery was similar
in the two cases, with about 0.05% by weight of powdered
nacre.
Fractionation ofsoluble extracts by HPLC
The size-exclusion chromatographic profiles for WSM and
EDTA-SM were very different (Fig. 1). As described in
Almeida et al. [20], thesolublematrix recovered by an
aqueous extraction (WSM) was separated in four distinct
fractions (Fig. 1A). On the contrary, under the same
conditions, thesolublematrix obtained after nacre demin-
eralization by EDTA (EDTA-SM) consisted of only two
different fractions (Fig. 1B). Absorbance values were very
high for EDTA-SM, in comparison with those obtained for
WSM, whereas the volume of EDTA-SM injected was half
the WSM volume. The low molecular weight peak due to
the use of EDTA, often mentioned inthe literature [24,33],
was not observed inthe size-exclusion profiles of the
EDTA-SM extract (Fig. 1B).
The fractionation by anion-exchange HPLC was also
different for WSM and EDTA-SM. Separation was better
Ó FEBS 2002 Solublesilk-likeorganicmatrixin nacre (Eur. J. Biochem. 269) 4995
resolved for EDTA-SM than for WSM (Fig. 2). The main
peak from each separation, indicated by an asterisk in
Fig. 2, was collected and submitted to amino acid analysis.
Amino acid compositions
In accordance with previous studies on nacre EDTA-SM on
other mollusk shells [34,35], this extract was aspartate-rich
(nearly 40 mole percent) (Table 1) and exhibited a charge to
hydrophobic ratio (C/HP; Asx, Glx, His, Arg, Lys/Ala, Pro,
Val, Met, Ile, Leu, Phe) of 2.86. The main amino acids
found in EDTA-SM were aspartate and glycine (69.2% of
total amino acids). Previous studies with regard to soluble
organic matrixof mollusk shells indicated that more than
80% ofthe aspartate and glutamate is inthe form of
aspartic and glutamic acid, respectively [34]. In order to
compare our results with published data [4,33,36], we also
determined the global amino acid composition of the
EDTA-IM. Here again, the composition was as expected,
i.e. very hydrophobic (C/HP ¼ 0.42) and glycine, alanine-
rich. Unexpectedly, thesolublematrix obtained by aqueous
extraction, WSM, likewise exhibited more than 60% of
glycine and alanine residues and a large proportion of
hydrophobic amino acids, resulting ina very low C/HP
value (0.29). Its content in Asx was moderate. These
features are exactly the opposite of that found in EDTA-SM
which exhibits a high Asx content (39.6%) and a low
content for alanine (6.5%). Thus, the alanine and glycine
content of WSM was rather similar to that of EDTA-IM. In
spite ofthe presence of mineral, it was possible to analyze
the amino acid composition ofthe water insoluble matrix
(WIM). Again we found a high content in Gly-Ala, and the
global composition was very similar to the WSM, and
consequently the EDTA-IM. Hydroxyproline, hydroxy-
lysine and phosphoserine were not detected in WSM, WIM,
EDTA-SM and EDTA-IM.
The comparison ofthe amino acid composition of the
main peak obtained from AE-HPLC of WSM and EDTA-
SM is given in Table 2. These two peaks were characterized
by a high content in glycine-alanine (31–30.6%) and serine.
As expected from an anion-exchange separation, the two
peaks contained acidic proteins. Nevertheless, they were
aspartic-rich in EDTA-SM whilst being quite glutamic acid-
rich in WSM.
Glycosaminoglycan analysis
Glycosaminoglycans are highly negatively charged because
of the presence of sulfate ester and/or carboxyl groups.
Therefore, they interact with cations and are precipitated by
cationic dyes like Alcian blue [37].
GAGs were found in WSM and EDTA-SM (Table 3).
Nevertheless, their amount in EDTA-SM was about 15
times as much as that of WSM, suggesting that they are
firmly tightened to the mineral or the aspartic acid-rich
Fig. 2. Anion exchange-HPLC elution profiles ofthe water-soluble
matrix (A) and the EDTA-soluble matrix (B) ofPinctadamaxima nacre.
Samples (55 lL) containing 400 lg (WSM) or 200 lg(EDTA-SM)
protein mixture in 20 m
M
Tris/HCl pH 7.8 were loaded on a Mono Q
HR 5/5 column equilibrated with the same buffer. Proteins were eluted
at a flow rate of 1 mLÆmin
)1
with a 25-min linear gradient from 0 to
100% solvent (500 m
M
NaCl, 20 m
M
Tris/HClbuffer,pH7.8).
Absorbance was monitored at 226 nm. The main peak from each
separation is indicated by an asterisk.
Fig. 1. Size exclusion-HPLC elution profiles ofthe water-soluble matrix
(A) and the EDTA-soluble matrix (B) ofPinctadamaxima nacre.
Samples of protein in ultra-pure water (500 lL and 250 lL, respect-
ively), were injected onto the preparative column (TSKGel G 3000
SW, 600 · 21.5 mm) and proteins were eluted with ultra-pure water at
2.5 mLÆmin
)1
flow rate. Absorbance was monitored at 280 nm. The
column was calibrated with alcohol dehydrogenase (150 kDa), bovine
serum albumin (66 kDa) and lysozyme (17 kDa).
4996 L. Pereira-Mourie
`
s et al. (Eur. J. Biochem. 269) Ó FEBS 2002
matrix. Very few GAGs were found inthe pellet (EDTA-
IM) obtained after demineralization.
Calcium analysis
In the EDTA-SM, the amount of nondialyzable calcium
after decalcification was 51.2 lgÆmg
)1
dry weight (Table 3),
and one may suppose that some EDTA remained in the
soluble extract, associated with calcium, as suggested by
Wheeler et al. [24,35]. The presence of residual EDTA after
intensive dialysis of EDTA-SM was also observed in amino
acid composition determination as EDTA eluted near to the
histidine, precluding from detecting this amino acid. The
calcium content ofthe EDTA-IM was, as expected, much
higher; about 310 lgÆmg
)1
dry weight. This high value may
in part be related to the incomplete demineralization of
powdered nacre, during extraction. In contrast, WSM
contained only 1.1 lg calcium per mg dry weight, confirm-
ing that very small amounts of calcium were dissolved in
water and/or linked to thematrix components.
Fourier transform infrared (FTIR) spectroscopy
Infrared spectroscopy provides means for a characterization
at the molecular level ofthe structure and bonding of
surface functional groups and adsorbed species. In this
study, we used infrared spectroscopy to identify possible
differences in composition between the decalcified nacre
soluble matrix (EDTA-SM) and the aqueous, nondecalci-
fied, nacre organicmatrix (WSM).
The FTIR spectrum ofthe EDTA-SM (Fig. 3A) was
characterized by two intense bands, one at 3432 cm
)1
(OH
and/or NH stretching modes oftheorganicmatrix compo-
nents) and another, the most intense, at 1593 cm
)1
, possibly
corresponding to the COO coordinated asymmetric stretch-
ing band. The presence of this band resulted from the
EDTA, a potent metal chelator that was used to extract the
soluble matrix from the crystalline structure. The EDTA
molecule has six potential sites for bonding with a metal ion:
four carboxyl groups and the two amino groups. When
EDTA is dissolved in water, it behaves like an amino acid
such as glycine. From the infrared spectrum ofa metal
chelated compound of EDTA, it is possible to distinguish
the coordinate and free COO stretching band. The union-
ized and uncoordinated COO stretching band occurs at
Table 2. Amino acid compositions (mole percent) ofthe main peak from
anion-exchange (AE) HPLC of water-soluble matrix (WSM) and
EDTA-soluble matrix (EDTA-SM). Cysteine, hydroxylysine, hydroxy-
proline, phosphoserine, proline and tryptophan were not determined.
Amino acid AE-WSM AE-EDTA-SM
Asx 9.7 21.0
Thr 3.3 3.7
Ser 27.6 18.3
Glx 13.4 9.5
Gly 22.4 22.9
Ala 8.6 7.7
Val 2.6 2.7
Met 0 0.5
Ile 1.7 2.1
Leu 3.9 2.9
Tyr 1.5 1.5
Phe 1.9 1.4
His 1.7 2.3
Lys 1.3 2.6
Arg 0.8 0.9
C/HP
a
1.44 2.10
a
Ratio charged to hydrophobic residues (see Results, section
Amino acid composition, for details).
Table 1. Amino acid compositions (mole percent) ofthe water-soluble matrix, water-insoluble matrix, the EDTA-soluble matrix and the EDTA-
insoluble matrixofPinctadamaxima nacre. Results are expressed as a mole percent and represent the mean of at least three independent
determinations. Cysteine and tryptophan were not determined. Hydroxyproline, hydroxylysine and phosphoserine were not detected in all samples.
Amino acid
Water-soluble
matrix
Water-insoluble
matrix
EDTA-soluble
matrix
EDTA-insoluble
matrix
Asx 7.3 10.8 39.6 10.8
Thr 0.9 1.1 1.4 1.1
Ser 3.9 4.0 3.6 4.4
Glx 2.2 2.2 4.3 2.2
Gly 37.6 28.7 29.6 31.5
Ala 30.0 31.8 6.5 30.5
Pro 1.5 1.1 1.2 1.3
Val 2.2 2.1 1.4 1.9
Met 1.2 1.1 1.3 1.0
Ile 1.2 1.3 1.5 1.2
Leu 6.7 6.3 3.4 5.9
Tyr 0.8 1.9 1 1.7
Phe 1.3 1.7 1.4 1.4
His 0.1 0.2 ND
a
0
Lys 1.2 1.7 1.7 1.2
Arg 1.9 4.1 2.1 3.9
C/HP
b
0.29 0.42 2.86 0.42
a
ND, not determined. After intensive dialysis the sample still contained residual EDTA.
b
Ratio charged to hydrophobic residues (see
Results, section Amino acid composition, for details).
Ó FEBS 2002 Solublesilk-likeorganicmatrixin nacre (Eur. J. Biochem. 269) 4997
1750–1700 cm
)1
whereas the ionized and coordinated COO
stretching band appears at 1650–1590 cm
)1
[38]. The latter
frequency depends on the nature ofthe metal. Although the
EDTA-SM was subjected to intensive dialysis against ultra-
pure water to remove EDTA, the fractions isolated from the
oyster matrix seem to be, for the most part, EDTA protein
complexes. This finding recommends that caution must be
taken in interpreting binding data of EDTA-extracted
matrix. Another strong band appeared at 1409 cm
)1
and
corresponds to the COO symmetric stretching band. We
could also identify the presence of sulfate groups absorbing
at 1284, 1260, 927 and 855 cm
)1
. Absorption bands that can
be attributed to the amide vibrations, namely 1328 cm
)1
(C–N stretching vibration, amide III), 808 cm
)1
(amide
VII), 708 cm
)1
(amide V or VII), 639 and 621 cm
)1
(amide
IV), were also observed. Several bands were present in the
1000–1150 cm
)1
zone, which is the major polysaccharide
absorption region. A band at 1180 cm
)1
was probably due
to in-plane NH
2
rocking. It is also possible that the small
bands located at 963, 985 and 1032 cm
)1
in the EDTA-SM
and the bands 997, 1032 and 1047 cm
)1
in the WSM
correspond to PO
4
3–
vibrations. Phosphate as well as sulfate
groups are potential calcium-binding moieties and are
reported to be present in mollusk shell soluble fractions
[1,39].
The FTIR spectrum ofthe WSM (Fig. 3B) was very
different from that ofthe EDTA-SM, although some of
the bands are common to both samples. These corres-
pond to the band at 3431 cm
)1
(OH and/or NH
stretching modes oftheorganicmatrix components)
and those inthe 2800–3000 cm
)1
region (C–H stretching
modes). Inthe WSM spectrum, a strong band at
1656 cm
)1
, also assigned as a shoulder inthe EDTA-
IM and powdered nacre spectra (data not shown), was
present and corresponds to the amide I groups (C¼O
stretching vibration inthe associated state). The absorp-
tion occurred inthe high-frequency wing ofthe amide II
band and was sometimes partly merged with it [40]. A
band at 1542 cm
)1
was also visible and is characteristic of
the amide II groups. Inthe WSM spectrum, other bands
were clearly assigned, namely at 1455 cm
)1
(CH
2
scissor-
ing) and 1384 cm
)1
(C–N stretching vibration, amide III).
Most ofthe absorption ofthe later band came within the
region 1390 ± 40 cm
)1
, in which the methyl or methy-
lene deformations are also active. The WSM sample
absorbed less inthe region between 1000 and 1150 cm
)1
compared to the EDTA-SM sample and therefore
appeared to contain a smaller proportion of polysaccha-
rides in its composition. That confirms the GAGs analysis
results.
Polyacrylamide gel electrophoresis
Proteins from shell soluble matrices are generally not easy to
visualize after SDS/PAGE separation [41]. Inthe present
study, most ofthe proteins from both EDTA-SM and
WSMmigratedinthegelwithnodistinctpattern,leavinga
dark continuous smear after silver staining (Fig. 4). No
discrete individual bands were observed inthe WSM
sample. However, the EDTA-SM revealed two distinct
proteins around 14 and 20 kDa, still presenting with the
dark smear background.
Table 3. Glycosaminoglycan analysis and calcium measurements ofthe water-soluble matrix, the EDTA-soluble matrix and the EDTA-insoluble
matrix ofPinctadamaxima nacre. Sulfated and nonsulfated glycosaminoglycans from the supernatant were estimated by the Whiteman Alcian
blue binding technique [28,29], using chondroitin sulfate as standard. Calcium analyses were performed on samples digested with nitric acid,
by atomic absorption spectrophotometry. Results are expressed as lgÆmg
)1
organic matrix dry weight (mean value ± standard deviation of three
determinations).
Water-soluble
matrix
EDTA-soluble
matrix
EDTA-insoluble
matrix
Glycosaminoglycans 1.59 ± 0.41 24.38 ± 1.10 0.18 ± 0.02
Calcium 1.1 ± 0.5 51.2 ± 1.7 312.1 ± 155.7
Fig. 3. FTIR spectra ofthe EDTA-soluble
matrix (A) and the water-soluble matrix (B) of
Pinctada maxima nacre. Samples were pre-
pared as KBr discs and were run at a spectral
resolution of 4 cm
)1
.
4998 L. Pereira-Mourie
`
s et al. (Eur. J. Biochem. 269) Ó FEBS 2002
DISCUSSION
For several years, mollusk shell biomineralization has been
studied with demineralized structures, in order to obtain the
organic material. In this way, thematrix molecules have
been classified conventionally into two types based on their
solubility in aqueous solutions after demineralization, the
insoluble matrix being characterized by the presence of
highly hydrophobic molecules and by a rich content in
glycine and alanine residues. It is thought to be largely
intercrystalline [42] and to provide a framework where
mineralization occurs. Thesolublematrix is characterized
by the predominance of acidic glycoproteins. It is known as
intracrystalline and is considered to play an important role
in induction of oriented nucleation, inhibition of crystal
growth and control of aragonite-calcite polymorphism [43].
At present, only a few constituents of these organic
matrices have been identified. One ofthe reasons for this is
that shell proteins are very difficult to isolate by means of
traditional biochemical methods (chromatography, electro-
phoresis, enzymatic cleavage) due to self-aggregation of the
molecules or an unusual resistance to temperature, chem-
icals and enzymes. Essentially, the recent advances in
isolation and characterization ofmatrix molecules have
been possible due to the genetic approach and cDNA
cloning. Ina recent paper, Marin et al.[44]describeda
combined technique of preparative electrophoresis and
Western blot on individual proteins which enables the
purification of different proteins in relative large amounts.
In this work, we compare the nacre organic matrix
obtained by the traditional demineralizing extraction
method, to an original method of studying matrix mole-
cules, without previous decalcification. We showed that it is
possible to extract and study organic compounds of the
biomineral nacre, by bypassing the demineralization step.
We think that it may present anew perception of how the
different fractions oftheorganicmatrix are organized in the
biomineral structure.
First, the aqueous method affected neither the yield of
organic material extraction in general nor the extraction of
proteins. Also, the WSM has a low calcium content,
confirming that the molecules extracted are not associated
with minute particles of CaCO
3
that had not been removed
by centrifugation. What changed significantly was the
content oftheorganic material and, presumably, its original
location inthe biomineral itself. In fact, the FTIR spectra,
the amino acid compositions, the chromatographic and
electrophoretic fractionations of EDTA-SM and WSM
showed a first sign of this dissimilarity. For the FTIR
spectra, the main differences were as follows: first, the
presence of sulfate groups and several bands corresponding
to polysaccharides inthe EDTA-SM, which may be
assigned to the high content of GAGs, observed in the
quantification assay. Second, theorganicmatrix extracted
solely in water, i.e. WSM, exhibited fewer polysaccharide
bands, but showed strong protein peaks (amide I and amide
II bands) that were previously observed inthe insoluble
matrix from decalcified nacre [45] or shell material [46]. The
position ofthe amide I band, the major protein absorption
band, depends on the conformation ofthe polypeptide
chain [47]. The presence of this amide I absorption band at
1656 cm
)1
suggests that the proteins in WSM are in the
a-helix or randomly coiled form, two conformations not
distinguishable by IR spectrometry [48]. Until very recently,
it was thought that the aspartic acid-rich proteins from the
decalcified solublematrix were in part inthe b-sheet
conformation [6,43], as well as the decalcified, silk-fibroin-
like insoluble matrices [49]. Recently Levi-Kalisman et al.
[5] modified these assumptions in suggesting that the ÔsilkÕ
would coat the chitin core ina homogeneous and
completely disorganized phase. Does the random coiled
form of WSM correspond to that disorganized phase? If so,
the WSM would be related to the ÔsilkÕ matrix and not to the
soluble aspartic acid-rich matrix.
The electrophoretic pattern of WSM did not give
significant information on its protein composition. The
continuous smear suggests the presence of GAGs or other
sugars bound to the proteins, despite a low GAG content in
this extract. Western blot analysis with a WSM fraction-
specific antibody revealed the complexity of this kind of
matrix, with several closely separated bands [50]. The
EDTA-SM showed a 14-kDa band, probably the N14
protein found by Kono et al. [14], and another one around
20 kDa. Attempts to purify and characterize these proteins
are presently in progress.
Above all these distinctions, the global amino acid
composition showed clearly that the proteins extracted by
the two methods are not the same. On the one hand, the
soluble (aspartic acid-rich proteins) and insoluble (glycine,
alanine-rich, hydrophobic proteins) matrices extracted after
demineralization with EDTA are in accordance with similar
results in corresponding literature [7,51,52]. On the other
hand, the amino acid composition of WSM, obtained by an
aqueous extraction, was completely different to that of the
EDTA-SM and the so-called soluble matrices in general.
This extract was highly hydrophobic with a C/HP value of
0.29 and exhibited more than 65% glycine and alanine
residues. To begin with, such a characteristic is strange for a
Fig. 4. SDS/PAGE ofPinctadamaxima nacre soluble matrices. (1)
LMW calibration kit; (2) EDTA-SM (30 lg protein); (3) WSM (50 lg
protein). Samples in Laemmli buffer were loaded on a 12% poly-
acrylamide mini-gel 0.75-mm thick, and silver stained.
Ó FEBS 2002 Solublesilk-likeorganicmatrixin nacre (Eur. J. Biochem. 269) 4999
soluble extract. Again, these are predominantly features of
what has been called up until now Ôinsoluble matrixÕ,andof
the known silk-fibroin-like molecules. When we looked to
the WIM, we found that it was similar in amino acid
composition to the WSM and the EDTA-IM extractions.
This result means that thesilk-likematrix is not completely
extracted with WSM, being present inthe two phases. The
acidic matrix would be still enclosed inthe mineral phase of
the WIM and would not be accessible for quantification.
However, when we placed the extracted particles (the pellet)
in pure water once again, no more matrix was released (data
not shown). This confirms the hypothesis that the silk is
indeed present in two states, soluble and insoluble, the latter
being in some way protected from dissolution in water. The
peculiarity ofthe WSM led to the question: how can such a
hydrophobic pool of molecules be dissolved in pure water?
Recently we hypothesized [50] that sugars might be
associated with the apolar proteins of WSM and would
be responsible for their solubilization in water. Here we
showed that GAGs are present in WSM, but in minor
amounts compared with the EDTA-SM.
GAGs and, more specifically, proteoglycans (PGs) are
supposed to be present in mollusk shell organic matrix.
Their presence was indicated by IR spectrometry and Alcian
blue staining [48,53], though without direct quantification.
Our results confirmed their presence in P. maxima nacre
organic matrix and showed that GAGs are mainly released
with EDTA and less with water. This is in accordance with
the observations of Golberg and Takagi [54] who have also
detected a loss of PGs in dentine during EDTA deminer-
alization. They concluded that it is necessary to study PGs
distribution on material fixed either with cryotechniques,
where PGs appear as an amorphous substance in dental
organic matrix, or with cationic dyes. The role of GAGs is
not really understood, but their presence inthe organic
matrices of bones, teeth, avian eggshell, otoconia and
kidney stones shows their importance in biomineralizing
systems. Acidic mucopolysaccharides have been considered
as possible candidates for the initiation ofthe crystal
formation [55]. Sulfate, as well as carboxylate groups, may
cooperate inthe induction of oriented crystal nucleation
[56]. These molecules may be responsible for fixation of
calcium inthe shell [57]. Also, PGs which are GAGs
associated to a core protein, may act in cell signaling and
metabolic activity [58,59].
To proceed with our argument on the nacre organic
matrix organization, we may understand why the WSM
obtained by an aqueous extraction does not contain acidic
proteins, like the other soluble matrices obtained after
demineralization. The acidic proteins are thought to be
firmly linked to the mineral, and without decalcification it
seems difficult to dissociate them from the whole structure.
Thus, in WSM, we theoretically extracted the molecules that
were directly accessible to water around the sides of the
small mineral particles. Inthe five-layered model of nacre
organic matrix organization [7,60] the surface layers, also
called the ÔenvelopeÕ by the authors, are the aspartic acid-
rich proteins. However, the surface molecules extracted in
WSM correspond to the core oftheorganicmatrixlayer of
the previous model, the silk-fibroin-like molecules. Thus, we
may think ofa different structure for nacre organic matrix,
where the silk (maybe WSM or at least part of it) would not
be so deeply located. From the cryo-transmission electron
microscopy studies ofthematrixofthebivalve Atrina,anew
model for thenacreouslayerorganicmatrix was recently
proposed by Levi-Kalisman et al. [5]. In this model, which
would be in accordance with our findings, a hydrated silk-
gel phase would be located between the mainly composed
b-chitin interlamellar sheets (Fig. 5). The aspartic acid-rich
glycoproteins would be present both within the silk gel prior
to mineralization and also as electron-dense patches at the
surface of b-chitin. The presence of chitin combined with the
silk-fibroin-like molecules was unfortunately not investi-
gated in P. maxima WSM. Still, its presence was demon-
strated in P. maxima as a chitin–protein complex, which
precipitated after demineralization ofthenacreous layer
with hydrochloric acid [61]. The characterization of the
proteins associated to this complex by amino acid analysis
of the precipitate after two deacetylation steps revealed the
predominance of two amino acids: alanine (39.2%) and
glycine (30%). Interestingly, the proportions are very similar
to those found in WSM for alanine and glycine.
Curiously, the presence ofa gel phase in shells was rarely
mentioned inthe literature until now, although the forma-
tion ofa jelly like substance within the shells of cultured
Crassostrea gigas is frequently reported by farmers. This
phenomenon is usually accompanied by a thickening of the
shell, with spaces filled by a nonmineralizing organic matrix
(a jelly-like substance) and is due to exogenous factors such
as exposure to the tributyltin contained in anti-fouling
paints. The few data available on the composition of this
kind of gel showed that it can not be compared to a silk-
fibroin-like substance [62–66]. Though this jelly-like sub-
stance is produced in abnormal situations, it shows that
bivalve organisms do possess the biochemical machinery
needed to produce gel inthe calcification process.
In our opinion, the importance ofthe silk-fibroin-like
matrix has been neglected until now, in part because of its
inaccessibility. The first insoluble molecules, after decalcifi-
cation, to be purified from mollusk shell were MSI 60 and
MSI 31, both from Pinctada fucata nacreous and prismatic
Fig. 5. Schematic representation ofthenew model for thenacreous layer
organic matrix structure, as proposed by Levi-Kalisman et al.[5].The
putative silk gel phase is located between the interlamellar sheets
of b-chitin. See details in Discussion (courtesy of Professor Steve
Weiner and coworkers). Reprinted from Journal of Structural Biology
135, Levi-Kalisman et al., Structure ofthenacreousorganic matrix,
pp 8–17, 2001, with permission from Elsevier Science.
5000 L. Pereira-Mourie
`
s et al. (Eur. J. Biochem. 269) Ó FEBS 2002
layers, respectively [67]. At about the same time, Shen et al.
[68] isolated lustrin A, a modular and multifunctional
protein from Haliotis rufescens nacre. Lastly, N16 [69] and
its homologous soluble protein N14 [14] have been charac-
terized inthenacreouslayerof P. fucata and P. maxima,
respectively, and would constitute anew protein family.
Many more ofthe studies on theorganicmatrix of
biominerals were focused on the attempt to characterize
and purify the aspartic acid-rich molecules [70–72]. One of
the obvious reasons is the solubility ofthe aspartic acid-rich
matrix under the conditions imposed by the decalcification
step. Another reason, related to the first one, may be the
accessibility ofthe acidic molecules. Being easily solubilized,
it was possible to use these molecules to perform tests in vitro
for their control inthebiomineralization process. Some
important roles were ascribed to them as the control of
nucleation, the growth and the inhibition of crystal forma-
tion [8,73]. The other compounds ofthe nacre organic
matrix, present in WSM, also possess important biological
activities on cellular mechanisms involved in biominerali-
zation. Indeed, we have shown that the WSM is able to
induce in vitro the differentiation pathway of osteoblasts
from precursor cells like fibroblasts, bone marrow cells and
preosteoblasts [20,21,74,75]. As silk-fibroin is insoluble after
demineralization, it is difficult to isolate these molecules.
The significance ofthe findings presented here is that, in
practice, the silk fraction can now be analyzed for primary
and secondary conformations, as well as for other biological
and physical properties.
With our comparative study on P. maxima nacre, it
seems that a classification oftheorganicmatrix into soluble
and insoluble, to distinguish the acidic proteins from the
hydrophobic glycine-alanine-rich molecules, is no longer
valid and may even lead to misunderstandings. Some results
support the idea that the amino acid sequence of proteins
extracted from soluble and insoluble matrices share com-
mon features [4]. Such a characteristic indicates that some of
these proteins may in fact belong to the same family.
ACKNOWLEDGMENTS
We would like to express our thank to Professor Steve Weiner and
Dr Lia Addadi for providing the illustration in Fig. 5. We are grateful
to Dr Sophie Berland and Sandrine Borzeix (Laboratoire de
Physiologie, MNHN, Paris, France) for all their useful comments
and iconography, respectively. This study was partly funded by a Siera
SA/CNRS Research and Development contract and by grants
(PRAXIS XXI/BPD/11811 and PRAXIS XXI/BD/20023) from the
Science and Technology Foundation of Portugal.
REFERENCES
1. Crenshaw, M.A. (1972) Thesolublematrix from Mercenaria
mercenaria shell. Biomineralization 6, 6–11.
2. Krampitz, G., Engels, J. & Cazaux, C. (1976) Biochemical studies
on water-soluble proteins and related components of gastropod
shells. InThe Mechanisms of Mineralization inthe Invertebrates
and Plants (Watabe, N. & Wilbur, K.M., eds), pp. 175–190. The
Barush B.W. Library in Marine Science no. 5, The University of
South Carolina Press, Columbia.
3. Weiner, S., Traub, W. & Lowenstam, H.A. (1983) Organic matrix
in calcified exoskeletons. InBiomineralization and Biological Metal
Accumulation (Westbroek, P. & deJong, E.W., eds), pp. 205–224.
Reidel, Dordrecht, Holland.
4. Keith, J., Stockwell, D., Ball, D., Remillard, K., Kaplan, D.,
Thannhauser, T. & Sherwood, R. (1993) Comparative analysis of
macromolecules in mollusc shells. Comp. Biochem. Physiol. 105B,
487–496.
5. Levi-Kalisman, Y., Falini, G., Addadi, L. & Weiner, S. (2001)
Structure ofthenacreousorganicmatrixofabivalve mollusk shell
examined inthe hydrated state using cryo-TEM. J. Struct. Biol.
135, 8–17.
6. Weiner, S. & Hood, L. (1975) Soluble protein ofthe organic
matrix of mollusk shells: a potential template for shell formation.
Science 190, 987–989.
7. Weiner, S. & Traub, W. (1984) Macromolecules in mollusc shells
and their functions in biomineralization. Phil. Trans. R. Soc. Lond.
B 304, 425–434.
8. Belcher, A.M., Wu, X.H., Christensen, R.J., Hansma, P.K.,
Stucky,G.D.&Morse,D.E.(1996)Controlofcrystalphase
switching and orientation by soluble mollusc-shell proteins.
Nature 381, 56–58.
9. Kamat, S., Su, X., Ballarini, R. & Heuer, A.H. (2000) Structural
basis for the fracture toughness ofthe shell ofthe conch Strombus
gigas. Nature 405, 1036–1040.
10. Hare, P.E. (1963) Amino acids inthe proteins from aragonite and
calcite inthe shells of Mytilus californianus. Science 139, 216–217.
11. Hare, P.E. & Abelson, P.H. (1965) Amino acid composition of
some calcified proteins. Carnegie Inst Washington Year Book 64,
223.
12. Watabe, N. (1984) Shell. In Biology ofthe Integument,Vol.1
Invertebrates (Bereiterhahn, J., Matolsty, A.G. & Richards, K.S.,
eds), pp. 448–485. Springer-Verlag, Berlin.
13. Mann, S. (1988) Molecular recognition in biomineralization.
Nature 332, 119–124.
14. Kono, M., Hayashi, N. & Samata, T. (2000) Molecular mechan-
ism ofthenacreouslayer formation inPinctada maxima. Biochem.
Biophys. Res. Commun. 269, 213–218.
15. Lopez, E., Berland, S. & Le Faou, A. (1994) Nacre, osteogenic and
osteoinductive properties. Bull. Inst Oce
´
an. Monaco 14, 49–57.
16. Lopez, E., Vidal, B., Berland, S., Camprasse, C., Camprasse, G. &
Silve, C. (1992) Demonstration ofthe capacity of nacre to induce
bone formation by human osteoblasts maintained in vitro. Tissue
Cell 24, 667–679.
17. Atlan, G., Balmain, N., Berland, S., Vidal, B. & Lopez, E. (1997)
Reconstruction of human maxillary defects with nacre powder:
histological evidence for bone regeneration. C. R. Acad. Sci. Paris,
Life Sci. 320, 253–258.
18. Atlan, G., Delattre, O., Berland, S., Le Faou, A., Nabias, G., Cot,
D. & Lopez, E. (1999) Interface between bone and nacre implants
in sheep. Biomaterials 20, 1017–1022.
19. Lamghari, M., Almeida, M.J., Berland, S., Huet, H., Laurent, A.,
Milet, C. & Lopez, E. (1999) Stimulation of bone marrow cells and
bone formation by nacre: in vivo and in vitro studies. Bone 25S,
91S–94S.
20. Almeida, M.J., Milet, C., Peduzzi, J., Pereira, L., Haigle, J.,
Barthe
´
lemy, M. & Lopez, E. (2000) The effect of water-soluble
matrix fraction extracted from the nacre ofPinctadamaxima on
the alkaline phosphatase activity of cultured fibroblasts. J. Exp.
Zool. (Mol. Dev. Evol.) 288, 327–334.
21. Almeida, M.J., Pereira, L., Milet, C., Haigle, J., Barbosa, M. &
Lopez, E. (2001) Comparative effects of nacre water-soluble
matrix and dexamethasone on the alkaline phosphatase activity of
MRC-5 fibroblasts. J. Biomed. Mater. Res. 57, 306–312.
22. Lamghari,M.,Berland,S.,Laurent,A.,Huet,H.&Lopez,E.
(2001) Bone reactions to nacre injected percutaneously into the
vertebrae of sheep. Biomaterials 22, 555–562.
23. Lopez,E.,Giraud,M.,LeFaou,A.,Berland,S.&Gutierrez,J.
(1995) Proce
´
de
´
de pre
´
paration de substances actives a
`
partir de la
nacre, produits obtenus, utiles comme me
´
dicaments.PatentCNRS
no. FR. 9515650, 28/12/1995, WO 97/24133–10/07/97.
Ó FEBS 2002 Solublesilk-likeorganicmatrixin nacre (Eur. J. Biochem. 269) 5001
24. Wheeler, A.P., Rusenko, K.W., George, J.W. & Sikes, S. (1987)
Evaluation of calcium binding by molluscan shell organic matrix
and its relevance to biomineralization. Comp. Biochem. Physiol.
87B, 953–960.
25. Cohen-Solal, L., Lian, J.B., Kossiva, D. & Glimcher, M.J. (1978)
The identification of O-phosphothreonine with soluble non-
collagenous phosphoproteins of bone matrix. FEBS Lett. 89,
107–110.
26. Cohen, S.A. & Strydom, D.J. (1988) Amino acid analyses utilizing
phenylisothiocyanate derivatives. Anal. Biochem. 174, 1–16.
27. Hewitt, B.R. (1958) Spectrophotometric determination of protein
in alkaline solution. Nature 187,246.
28. Whiteman, P. (1973) The quantitative determination of glycos-
aminoglycans in urine with Alcian blue 8GX. Biochem. J. 131,
351–357.
29. Whiteman, P. (1973) The quantitative measurement of Alcian
blue-glycosaminoglycan complexes. Biochem. J. 131, 343–350.
30. Gold, E.W. (1979) A simple spectrophotometric method for esti-
mating glycosaminoglycan concentrations. Anal. Biochem. 99,
183–188.
31. Laemmli, U.K. (1970) Cleavage of structural proteins during the
assembly ofthe head of bacteriophage T4. Nature 227, 680–685.
32. Morrissey, J.H. (1981) Silver stain for proteins in polyacrylamide
gels: a modified procedure with enhanced uniform sensitivity.
Anal. Biochem. 117, 307–310.
33. Wheeler, A.P., Rusenko, K.W. & Sikes, S. (1988) Organic matrix
from carbonate biomineral as a regulator of mineralization. In
Chemical Aspects of Regulation of Mineralization (Sikes,C.S.&
Wheeler, A.P., eds). University of South Alabama Publication
Services, Mobile, Alabama.
34. Weiner, S. (1979) Aspartic acid-rich proteins: major components
of thesolubleorganicmatrixof mollusk shells. Calcif. Tissue Int.
29, 163–167.
35. Wheeler, A.P., Rusenko, K.W., Swift, D.M. & Sikes, S. (1988)
Regulation ofin vitro and in vivo CaCO
3
crystallization by frac-
tions of oyster shell organic matrix. Mar. Biol. 98, 71–80.
36. Halloran, B.A. & Donachy, J.E. (1995) Characterization of
organic matrix macromolecules from the shells ofthe antarctic
scallop Adamussium colbecki. Comp. Biochem. Physiol. 111B,
221–231.
37. Scott, J.E., Quintarelli, G. & Dellovo, M.C. (1964) The chemical
and histochemical properties of Alcian blue staining. Histochemie
4, 73–85.
38. Nakamoto, K. (1986) IR and Raman Spectra of Inorganic and
Coordination Compounds.J.Wiley&Sons,NewYork.
39. Samata,T.&Krampitz,G.P.(1982)Calciumbindingpolypep-
tides in oyster shells. Malacologia 22, 225–233.
40. Roeges, N.P.G. (1998) A Guide to the Complete Interpretation of
Infrared Spectra ofOrganic Structures.J.Wiley&Sons,New
York.
41. Cariolou, M. & Morse, D. (1988) Purification and characteriza-
tion of calcium binding conchiolin shell peptides from the mollusc,
Haliotis rufescens, as a function of development. J. Comp. Physiol.
157B, 717–729.
42. Krampitz, G.P. (1982) Structure oftheorganicmatrixin mollusc
shells and avian eggshells. In Biological Mineralization and
Demineralization (Nancollas, G.H., ed.), pp. 219–232. Springer-
Verlag, Berlin, Heidelberg, New York.
43. Weiner, S. & Addadi, L. (1991) Acidic macromolecules of
mineralized tissues: the controllers of crystal formation. Trends
Biochem. Sci. 16, 252–256.
44. Marin, F., Pereira, L. & Westbroek, P. (2001) Large-scale frac-
tionation of molluscan shell matrix. Protein Expr. Purif. 23,
175–179.
45. Balmain, J., Hannoyer, B. & Lopez, E. (1999) Fourier transform
infrared spectroscopy (FTIR) and X-ray diffraction analyses of
mineral and organicmatrix during heating of mother of pearl
(nacre) from the shell ofthe mollusc Pinctada maxima. J. Biomed.
Mater. Res. Appl. Mat. 48, 754.
46.Marxen,J.C.,Hammer,M.,Gehrke,T.&Becker,W.(1998)
Carbohydrates oftheorganic shell matrix and the shell forming
tissue ofthe snail Biomphalaria glabrata (Say). Biol. Bull. 194,
231–240.
47. Miyazawa, T. & Blout, E.R. (1961) The infrared spectra of poly-
peptides in various conformations – amide I and II bands. J. Am.
Chem. Soc. 83, 712–719.
48. Worms, D. & Weiner, S. (1986) Mollusk shell organic matrix:
fourier transform infrared study ofthe acidic macromolecules.
J. Exp. Zool. 237, 11–20.
49. Weiner, S. & Traub, W. (1980) X-ray diffraction study of the
insoluble organicmatrixof mollusk shells. FEBS Lett. 111,311–
316.
50. Pereira-Mourie
`
s, L., Almeida, M.J., Marin, F., Gay, M., Milet, C.
& Lopez, E. (2002) Soluble proteins ofthe nacre from the giant
oyster Pinctadamaxima with highly hydrophobic amino acids.
Biomineralization: Formation, Diversity, Evol. Appl, in press.
51. Nakahara, H., Kakei, M. & Bevelander, G. (1980) Fine structure
and amino acid composition oftheorganic ÔenvelopeÕ in the
prismatic layerof some bivalve shells. Venus Jpn. J. Malacol. 39,
167–177.
52. Falini, G., Albeck, S., Weiner, S. & Addadi, L. (1996) Control of
aragonite or calcite polymorphism by mollusk shell macro-
molecules. Science 271, 67–69.
53. Simkiss, K. (1965) Theorganicmatrixofthe oyster shell. Comp.
Biochem. Physiol. 16, 427–435.
54. Golberg, M. & Takagi, M. (1993) Dentine proteoglycans: com-
position, ultrastructure, and functions. Histochem. J. 25, 781–806.
55. Wilbur, K.M. (1976) Recent studies of invertebrate mineraliza-
tion. InThe Mechanisms of Mineralization in Invertebrates and
Plants (Watabe, N. & Wilbur, K.M., eds), pp. 79–108. The Uni-
versity of. South Carolina Press, The Belle W. Baruch Library in
Marine Science no. 5, Columbia.
56. Addadi, L., Moradian, J., Shay, E., Maroudas, N.G. & Weiner, S.
(1987) A chemical model for the cooperation of sulfates and car-
boxylates in calcite crystal nucleation: Revelance to biominer-
alization. Proc. Natl Acad. Sci. USA 84, 2732–2736.
57. Marxen,J.C.&Becker,W.(2000)Calciumbindingconstituentsof
the organic shell matrix from the freshwater snail Biomphalaria
glabrata. Comp. Biochem. Physiol. 127B, 235–242.
58. Tanaka, Y., Adams, D.H. & Shaw, S. (1993) Proteoglycans on
endothelial cells present adhesion-inducing cytokines to leuko-
cytes. Immunol. Today 14, 111–115.
59. Jackson, R.L., Bush, S.J. & Cardin, A.D. (1991) Glycosami-
noglycans: molecular properties, protein interactions, and role in
physiological processes. Physiol. Rev. 71, 481–539.
60. Nakahara, H. (1983) Calcification of gastropod nacre. In Bio-
mineralization and Biological Metal Accumulation (Westbroek, P.
& deJong, E.W., eds), pp. 225–230. Reidel, Dordrecht, Holland.
61. Zentz, F., Be
´
douet,L.,Almeida,M.J.,Milet,C.,Lopez,E.&
Giraud, M. (2001) Characterization and quantification of chitosan
extracted from nacre ofthe abalone Haliotis tuberculata and the
oyster Pinctada maxima. Mar. Biotechnol. 3, 36–44.
62. Alzieu, C., Thibaud, Y., Heral, M. & Boutier, B. (1980) Evaluation
des risques dus a l’emploi des peintures anti-sallissures dans les
zones conchyoliques. Rev. Trav. Inst. Pe
ˆ
ches Marit. 44, 301–348.
63. Alzieu, C., Heral, M., Thibaud, Y., Dardignac, M.J. & Feuillet,
M. (1982) Influence des peintures anti-sallissures a
`
base
d’organostanniques sur la calcification de la coquille de l’huıˆtre
Crassostrea gigas. Rev. Trav. Inst. Pe
ˆ
ches Marit. 45, 101–116.
64. Krampitz, G., Drolshagen, H. & Deltreil, J.P. (1983) Soluble
matrix components in malformed oyster shells. Experientia 39,
1105–1106.
65. Alzieu, C. & Heral, M. (1984) Ecotoxicological effects of orga-
notin coumpounds on oyster culture. In Ecotoxicological Testing
5002 L. Pereira-Mourie
`
s et al. (Eur. J. Biochem. 269) Ó FEBS 2002
for the Marine Environment, 2 (Persoone, G., Jaspers, E. & Claus,
C., eds), pp. 187–196. State University Ghent and Inst. Mar. Sci.
Res., Bredene, Belgium.
66. Almeida, M.J. (1996) Crescimento em ostras: factores que
afectam a formac¸a
˜
o e estrutura da concha. PhD Thesis, Instituto
de Cieˆ ncias Biome
´
dicas Abel Salazar, University of Porto,
Portugal.
67. Sudo, S., Fujikawa, T., Nagakura, T., Ohkubo, T., Sakaguchi, K.,
Tanaka, M., Nakashina, K. & Takahashi, T. (1997) Structures of
mollusc shell framework proteins. Nature 387, 563–564.
68. Shen, X., Belcher, A.M., Hansma, P.K., Stucky, G.D. & Morse,
D.E. (1997) Molecular cloning and characterization of Lustrin A,
a matrix protein from shell and pearl nacre of Haliotis rufescens.
J. Biol. Chem. 272, 32472–32481.
69. Samata, T., Hayashi, N., Kono, M., Hasegawa, K., Horita, C. &
Akera, S. (1999) Anewmatrix protein family related to the
nacreous layer formation ofPinctada fucata. FEBS Lett. 462,
225–229.
70. Mann, S., Webb, J. & Williams, R.J.P. (1989) Biomineralization:
Chemical and Biochemical Perspectives, pp. 35–62. VCH,
Weinheim.
71. Simkiss, K. & Wilbur, K.M. (1989) Biomineralization – Cell
Biology and Mineral Deposition. Academic Press, San Diego.
72. Sarashina, I. & Endo, K. (1998) Primary structure ofa soluble
matrix protein of scallop shell: implications for calcium carbonate
biomineralization. Am. Mineral. 83, 1510–1515.
73. Weiss, I., Kaufmann, S., Mann, K. & Fritz, M. (2000) Purification
and characterization of perlucin and perlustrin, two new proteins
from the shell ofthe mollusc Haliotis laevigata. Biochem. Biophys.
Res. Commun. 267, 17–21.
74. Pereira-Mourie
`
s,L.,Milet,C.,Almeida,M.J.,Rousseau,M.,
Borzeix, S. & Lopez, E. (2001) Biological effect ofthe water-
soluble matrix extract ofthe nacre shell layerofPinctada maxima
on vertebrate cell proliferation and differentiation. In Proceedings
of the 3rd International Satellite Symposium on the Comparative
Endocrinology of Calcium Regulation (Gay, C.V., Dacke, C.G.,
Dancks, J.A. & Cox, P.A., eds). http://www.sci.port.ac.uk/-cecr
75. Pereira-Mourie
`
s, L., Almeida, M.J., Milet, C., Berland, S. &
Lopez, E. (2002) Bioactivity of nacre water-soluble organic matrix
from thebivalve mollusk Pinctadamaximain three mammalian
cell types: fibroblasts, bone marrow stromal cells and osteoblasts.
Comp. Biochem. Physiol. 132, 215–217.
Ó FEBS 2002 Solublesilk-likeorganicmatrixin nacre (Eur. J. Biochem. 269) 5003
. Soluble silk-like organic matrix in the nacreous layer of the bivalve
Pinctada maxima
A new insight in the biomineralization field
Lucilia Pereira-Mourie
`
s
1
,. water -soluble matrix, water-insoluble matrix, the EDTA -soluble matrix and the EDTA-
insoluble matrix of Pinctada maxima nacre. Results are expressed as a mole