From hemoglobin to urchin spicules.

A retrospective of an academic career. The article poses the question about the values involved in a life in the academy, starting with the role of hemoglobin in the chick embryo and ending with the role of calcium in the sea urchin spine.

Endocytosis in primary mesenchyme cells during sea urchin larval skeletogenesis.

The sea urchin larval embryo elaborates two calcitic endoskeletal elements called spicules. Spicules are synthesized by the primary mesenchyme cells (PMCs) and begin to form at early gastrula stage. It is known that the calcium comprising the spicules comes from the seawater and we wish to further consider the mode of calcium transport from the extracellular seawater to the PMCs and then onto the forming spicules.

Investigating protein function in biomineralized tissues using molecular biology techniques.

We describe modern molecular biology methods currently used in the study of biomineralization. We focus our descriptions on two areas of biomineralization research in which these methods have been particularly powerful. The first area is the use of modern molecular methods to identify and characterize the so-called occluded matrix proteins present in mineralized tissues.

SM30 protein function during sea urchin larval spicule formation.

A central issue in better understanding the process of biomineralization is to elucidate the function of occluded matrix proteins present in mineralized tissues. A potent approach to addressing this issue utilizes specific inhibitors of expression of known genes. Application of antisense oligonucleotides that specifically suppress translation of a given mRNA are capable of causing aberrant biomineralization, thereby revealing, at least in part, a likely function of the protein and gene under investigation.

Phase transitions in biogenic amorphous calcium carbonate.

Crystalline biominerals do not resemble faceted crystals. Current explanations for this property involve formation via amorphous phases. Using X-ray absorption near-edge structure (XANES) spectroscopy and photoelectron emission microscopy (PEEM), here we examine forming spicules in embryos of Strongylocentrotus purpuratus sea urchins, and observe a sequence of three mineral phases: hydrated amorphous calcium carbonate (ACC · H(2)O) → dehydrated amorphous calcium carbonate (ACC) → calcite.

Molecular aspects of biomineralization of the echinoderm endoskeleton.

Echinoderms possess a rigid endoskeleton composed of calcite and small amounts of occluded organic matrix proteins. The test (i.e.

Proteomic analysis of sea urchin (Strongylocentrotus purpuratus) spicule matrix.

Background: The sea urchin embryo has been an important model organism in developmental biology for more than a century. This is due to its relatively simple construction, translucent appearance, and the possibility to follow the fate of individual cells as development to the pluteus larva proceeds. Because the larvae contain tiny calcitic skeletal elements, the spicules, they are also important model organisms for biomineralization research.

SpSM30 gene family expression patterns in embryonic and adult biomineralized tissues of the sea urchin, Strongylocentrotus purpuratus.

The SpSM30 gene family of the sea urchin, Strongylocentrotus purpuratus, is comprised of six members, designated SpSM30A through SpSM30F (Livingston et al., 2006). The SpSM30 proteins are found uniquely in embryonic and adult mineralized tissues of the sea urchin.

Mechanism of calcite co-orientation in the sea urchin tooth.

Sea urchin teeth are remarkable and complex calcite structures, continuously growing at the forming end and self-sharpening at the mature grinding tip. The calcite (CaCO(3)) crystals of tooth components, plates, fibers, and a high-Mg polycrystalline matrix, have highly co-oriented crystallographic axes. This ability to co-orient calcite in a mineralized structure is shared by all echinoderms.

Transformation mechanism of amorphous calcium carbonate into calcite in the sea urchin larval spicule.

Sea urchin larval spicules transform amorphous calcium carbonate (ACC) into calcite single crystals. The mechanism of transformation is enigmatic: the transforming spicule displays both amorphous and crystalline properties, with no defined crystallization front. Here, we use X-ray photoelectron emission spectromicroscopy with probing size of 40-200 nm.

The dynamics of secretion during sea urchin embryonic skeleton formation.

Skeleton formation involves secretion of massive amounts of mineral precursor, usually a calcium salt, and matrix proteins, many of which are deposited on, or even occluded within, the mineral. The cell biological underpinnings of this secretion and subsequent assembly of the biomineralized skeletal element is not well understood. We ask here what is the relationship of the trafficking and secretion of the mineral and matrix within the primary mesenchyme cells of the sea urchin embryo, cells that deposit the endoskeletal spicule.

Probing the organic-mineral interface at the molecular level in model biominerals.

It is widely known that macromolecules, such as proteins, can control the nucleation and growth of inorganic solids in biomineralizing organisms. However, what is not known are the complementary molecular interactions, organization, and rearrangements that occur when proteins interact with inorganic solids during the formation of biominerals. The organic-mineral interface (OMI) is expected to be the site for these phenomena, and is therefore extraordinarily interesting to investigate.

The genome of the sea urchin Strongylocentrotus purpuratus.

We report the sequence and analysis of the 814-megabase genome of the sea urchin Strongylocentrotus purpuratus, a model for developmental and systems biology. The sequencing strategy combined whole-genome shotgun and bacterial artificial chromosome (BAC) sequences. This use of BAC clones, aided by a pooling strategy, overcame difficulties associated with high heterozygosity of the genome.

A functional genomic and proteomic perspective of sea urchin calcium signaling and egg activation.

The sea urchin egg has a rich history of contributions to our understanding of fundamental questions of egg activation at fertilization. Within seconds of sperm-egg interaction, calcium is released from the egg endoplasmic reticulum, launching the zygote into the mitotic cell cycle and the developmental program. The sequence of the Strongylocentrotus purpuratus genome offers unique opportunities to apply functional genomic and proteomic approaches to investigate the repertoire and regulation of Ca(2+) signaling and homeostasis modules present in the egg and zygote.

Developmental biology meets materials science: Morphogenesis of biomineralized structures.

Biomineralization is the process by which metazoa form hard minerals for support, defense, and feeding. The minerals so formed, e.g.

The localization of occluded matrix proteins in calcareous spicules of sea urchin larvae.

The sea urchin embryo forms calcareous endoskeletal spicules composed of calcite and an occluded protein matrix. Though the latter is approximately 0.1% of of the mass, the composite has substantially altered material properties, e.

Ultrastructural localization of spicule matrix proteins in normal and metalloproteinase inhibitor-treated sea urchin primary mesenchyme cells.

Studies of the sea urchin larval skeleton have contributed greatly to our understanding of the process of biomineralization. In this study we have undertaken an investigation of the morphology of skeleton formation and the localization of proteins involved in the process of spicule formation at the electron microscope level. Sea urchin primary mesenchyme cells undergo a number of morphological changes as they synthesize the larval skeleton.

Development of calcareous skeletal elements in invertebrates.

Most metazoans require skeletal support systems. While the formation of bones and teeth in vertebrates has been well studied, endo- and exoskeleton development of non-vertebrates, especially calcification during terminal differentiation, has been neglected. Biomineralization of skeletons in invertebrates presents interesting research opportunities.

Biomineralization of the spicules of sea urchin embryos.

The formation of calcareous skeletal elements by various echinoderms, especially sea urchins, offers a splendid opportunity to learn more about some processes involved in the formation of biominerals. The spicules of larvae of euechinoids have been the focus of considerable work, including their developmental origins. The spicules are composed of a single optical crystal of high magnesium calcite and variable amounts of amorphous calcium carbonate.

Spicule matrix protein LSM34 is essential for biomineralization of the sea urchin spicule.

Biomineralized skeletal structures are composite materials containing mineral and matrix protein(s). The cell biological mechanisms that underlie the formation, secretion, and organization of the biomineralized materials are not well understood. Although the matrix proteins influence physical properties of the structures, little is known of the role of these matrix proteins in the actual formation of the biomineralized structure.

Injection of myo-inositol reverses the effects of lithium on sea urchin blastomeres.

Lithium is known to cause sea urchin blastomeres destined to give rise to epithelium rather than to differentiate into gut or skeleton. While it has been proposed that lithium alters development by interfering with the inositol-tris phosphate-protein kinase C (IP -PKC) signaling pathway, the mechanism of action of lithium in sea urchins has remained elusive. Here we describe experiments that examine the hypothesis that lithium exerts its effect on sea urchin embryos via the IP -PKC pathway.

Gene Expression, DNA Synthesis and Protein Synthesis in Cells from Dissociated Sea Urchin Embryos: (gene expression/sea urchins/cell interactions).

DNA synthesis, protein synthesis, and the accumulation of two tissue-specific transcripts were examined in cultures of sea urchin embryos that were completely dissociated during early cleavage stages and raised in Ca -free sea water for 24 hr. In Strongylocentrotus purpuratus, both DNA and protein synthesis were severely reduced by dissociation treatment. Previous studies using this species indicated that aboral ectoderm-specific transcript accumulation is severely reduced while mesenchyme-specific transcripts generally accumulate more normally (11, 17).