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Parietal bone

The parietal bones are a pair of large, flat, cranial bones that form the superior and lateral walls of the cranium, contributing significantly to the protection of the . These bones are essential components of the , overlaying the parietal lobes of the and covered externally by the . Each parietal bone is slightly curved, with a external surface that is smooth and features the parietal eminence—a rounded elevation marking the site of —and temporal lines for muscle attachments. The internal surface is concave and irregular, accommodating grooves for the and branches of the . Positioned symmetrically on either side of the , the two parietal bones meet along the midline at the , while anteriorly they articulate with the at the and posteriorly with the at the . Laterally, each bone connects with the greater wing of the sphenoid and the squamous part of the at the sphenoparietal and squamosal sutures, respectively, forming key junctions such as the (sphenoidal angle) and asterion (mastoid angle). These articulations via fibrous cranial sutures provide structural integrity to the calvaria, the upper portion of the . A notable feature is the parietal foramen, a small opening near the sagittal border that transmits an emissary vein connecting the extracranial veins to the , though its presence and size can vary. In terms of development, the parietal bones ossify intramembranously from a single center in the parietal eminence during the eighth week of fetal life, growing to form much of the by adulthood. Their robust yet thin structure—typically 5–7 mm thick—balances protection with minimal weight, making them vital for enclosing the while allowing for skull growth in infancy through suture patency.

Anatomy

Location and structure

The parietal bones are a pair of flat, irregular, bones that form the superior and lateral aspects of the cranium, contributing significantly to the or calvaria. They are positioned symmetrically on either side of the , overlying the parietal lobes of the , and are covered externally by the and . Together with the frontal and occipital bones, they enclose and protect the upper portion of the . Structurally, each parietal bone exhibits a slightly curved, shape with a external surface and a internal surface, adapting to the contours of the underlying . The external surface is generally smooth and , featuring the parietal eminence—a rounded elevation in its central region that marks the site of maximum breadth—and two temporal lines: the superior temporal line for attachment of the and the inferior temporal line for the . A small parietal foramen is often present near the superior border, transmitting an emissary vein to the . The internal surface is irregular and concave, accommodating cerebral structures; it includes the sagittal sulcus along the superior border for the and grooves for branches of the . The bone is bounded by four borders: the anterior frontal border, which is serrated and articulates with the at the ; the posterior occipital border, irregular and meeting the at the ; the superior sagittal border, the thickest, joining the contralateral parietal bone at the ; and the inferior squamosal border, which articulates with the greater wing of the sphenoid and squamous part of the via the sphenoparietal and squamous sutures, respectively. At the corners where these borders meet, four angles form key landmarks: the anterior frontal angle at the , the anteroinferior sphenoidal angle at the , the posterosuperior occipital angle at the , and the posteroinferior mastoid angle at the asterion. These articulations connect the parietal bone to five other cranial bones, ensuring structural integrity through immovable fibrous joints.

External surface

The external surface of the parietal bone is convex and smooth, contributing to the superior and lateral aspects of the . This surface is gently curved to accommodate the overlying and provides attachment points for muscular and fascial structures involved in mastication and scalp tension. A prominent feature is the parietal eminence (or ), a rounded elevation located near the center of the bone, which represents the site of primary during embryonic . Arching across the anterosuperior portion of this surface are the superior and inferior temporal lines. The superior temporal line, a curved ridge, marks the attachment of the , separating the above from the below. The inferior temporal line, positioned parallel and slightly below, serves as the origin for the fibers. Near the posterior border, along the superior sagittal margin, the parietal foramen may be present as a small opening. This foramen transmits the parietal emissary vein, which connects the extracranial veins to the , facilitating venous drainage and potential communication between intracranial and extracranial venous systems. The overall convexity of the external surface also supports the insertion of galea aponeurotica fibers indirectly through its relation to the layers.

Internal surface

The internal surface of the parietal bone is concave and irregular, featuring impressions that correspond to the convolutions of the underlying cerebral hemispheres. These gyral impressions provide a molded fit against the brain's surface, accommodating the gyri and sulci for protection and stability within the . Prominent vascular grooves mark this surface, including the sagittal sulcus along the superior border, which articulates with the corresponding sulcus on the opposite parietal bone to form a channel for the . This broad groove runs anterosuperiorly and is often surrounded by small pits known as granular foveolae, which house arachnoid granulations that facilitate the drainage of into the venous system. Additionally, branching grooves for the and its vessels extend posterosuperiorly from the sphenoidal angle, originating near the foramen spinosum and supplying the . In some individuals, a parietal may pierce the posterosuperior region near the sagittal border, transmitting an emissary vein connecting to the and branches of the occipital artery. Near the mastoid angle, a small groove may overlie a portion of the , though this is more prominently associated with the adjacent . These features collectively support the bone's role in housing and arterial structures essential for intracranial circulation.

Borders

The parietal bone, one of the paired flat bones forming the superior and lateral aspects of the cranium, features four distinct borders that facilitate its articulations with adjacent cranial bones via fibrous sutures, contributing to the structural integrity of the skull vault. These borders are irregular and serrated to interlock securely, minimizing movement and providing robust protection for the . The superior border, also known as the sagittal border, is the longest and thickest of the four, extending along the superomedial margin of the bone. It articulates with the corresponding superior border of the contralateral parietal bone, forming the interparietal (sagittal) suture that runs along the midline of the from the coronal to the lambdoid sutures. This border meets the anteriorly at the and the posteriorly at the , key sites in the fetal that ossify postnatally. The anterior border, or frontal border, is highly serrated and lies along the anterosuperior edge, articulating with the lateral aspect of the to form the superolateral portion of the . This suture extends transversely across the , separating the from the parietals and serving as a critical landmark for surgical approaches to the anterior cranium. The posterior border, termed the occipital border, is irregular and jagged, articulating with the superior aspect of the to constitute the inferolateral half of the . This suture converges with the at the and with the parietomastoid suture at the asterion, a clinically significant point for identifying underlying venous structures and mastoid air cells. The inferior border, known as the squamosal or temporal border, is the most variable in thickness, being thin anteriorly and thickening as it arches posteriorly. Its anterior portion articulates with the greater wing of the via the sphenoparietal suture, while the posterior segment connects with the squamous and mastoid parts of the through the squamous (squamosal) and parietomastoid sutures, respectively. This border forms the lateral wall of the and is adjacent to the anteriorly, a weak region prone to fractures due to its thin bony structure overlying the .

Angles

The parietal bone is an irregularly quadrilateral structure featuring four distinct angles, each formed by the convergence of two borders and serving as key anatomical landmarks for suture intersections. These angles are the frontal (anterosuperior), sphenoidal (anteroinferior), occipital (posterosuperior), and mastoid (posteroinferior). The frontal angle, located at the —the of the coronal and sagittal sutures—is formed by the meeting of the frontal and sagittal borders and marks the anterior superior corner of the bone. This angle articulates with the superiorly and the opposite parietal bone medially, contributing to the stability of the . The sphenoidal angle, situated at the pterion, arises from the intersection of the frontal and squamosal (inferior) borders and is positioned at the confluence of the coronal, sphenoparietal, and sphenofrontal sutures. This anteroinferior angle is clinically significant due to its proximity to the , where fractures can lead to epidural hematomas; the internal surface here features prominent grooves for the artery's anterior and posterior branches. Posteriorly, the occipital angle, more rounded in contour, forms at the —the of the lambdoid and sagittal sutures—and results from the sagittal and occipital borders' convergence. It connects with the , reinforcing the posterior cranial architecture. Completing the quadrilateral, the mastoid angle lies posteroinferiorly at the asterion, where the parietomastoid, lambdoid, and occipitomastoid sutures meet, defined by the squamosal and occipital borders. This angle articulates with the mastoid portion of the , providing attachment for muscles like the sternocleidomastoid and facilitating the transmission of auditory structures. Collectively, these angles not only delineate the parietal bone's boundaries but also serve as reference points in and for identifying cranial trauma or developmental variations.

Development

Ossification process

The parietal bone develops through , a in which forms directly from mesenchymal without a preceding cartilaginous template. This mode of ossification is characteristic of the flat bones of the , including the parietal bones, which originate from paraxial mesoderm-derived . Unlike seen in long bones, intramembranous ossification allows for rapid expansion of the to accommodate the growing during fetal development. The process begins with the aggregation of mesenchymal cells into condensations near the parietal eminence, a prominent on the lateral aspect of the developing . These cells differentiate into osteoprogenitor cells and then osteoblasts under the influence of signaling factors such as bone morphogenetic proteins (BMPs) and fibroblast growth factors (FGFs). Each parietal typically arises from two primary centers that appear simultaneously at the parietal eminence during the eighth week post-conception. These centers lie in the same plane or slightly superimposed, initiating formation through the secretion of osteoid matrix by osteoblasts, which subsequently mineralizes to form woven . Ossification progresses radially outward from these central foci, with osteoblasts depositing layers of bone matrix in an appositional manner, expanding the bone peripherally toward the sutures. By the fourteenth week of gestation, extensive ossification has occurred in both parietal bones, though the process continues along the margins throughout fetal life. The two primary centers fuse by the fourth month of gestation, resulting in a single cohesive bone plate per side. As the bone matures, the initial woven bone is remodeled into lamellar bone, with compact cortical layers forming on the outer and inner surfaces and trabecular spongy bone in the diploë (the space between). Postnatally, further growth of the parietal bone occurs primarily through at the sutural edges, driven by mechanical forces from and coordinated with adjacent cranial bones. This sutural growth persists until early adulthood, when the sutures begin to fuse, typically completing between ages 20 and 30. ossification centers may occasionally appear near the sutures, contributing to minor variations, but the primary process remains intramembranous throughout.

Variations in ossification

The parietal bone typically undergoes from primary centers (formed by the early of two centers) per side, initiating at approximately 7–8 weeks of embryonic life and expanding radially to meet and articulate along the midline at the by late fetal development. However, variations arise from disruptions in this process, such as the presence of multiple centers, delayed , or genetic defects, leading to segmented or incomplete bone formation. One notable variation is os parietale partitum, a segmentation of the parietal bone into two or more parts due to failure of fusion between ossification centers, often manifesting as an additional suture in the anteroposterior or superoinferior direction. This trait is linked to embryological disturbances during the 7–8th prenatal week and is typically unilateral, with reported around 1.9% in specific populations such as . It may associate with skull asymmetry but is generally . Enlarged parietal foramina represent another ossification defect, characterized by symmetric, paired lucencies in the posterior parietal bones near the sagittal and lambdoid sutures, resulting from insufficient around the embryonic parietal notch. These foramina, with diameters from millimeters to centimeters, occur due to heterozygous in the MSX2 or ALX4 genes and follow an autosomal dominant with incomplete . is estimated at 1:15,000 to 1:50,000, and while often resolving into smaller openings by adulthood, persistent cases may require surgical intervention if associated with risks like leakage. Interparietal bone variations, though primarily involving the occipital squama, can influence parietal at the through shared developmental pathways, including non-fusion of 2–3 pairs of ossification centers leading to bipartite, , or pre-interparietal segments. Such anomalies, observed in adult skulls as symmetrical midline pieces, highlight the of posterior cranial ossification and are documented in classifications encompassing unipartite to multipartite forms. Additional variations include parietal fissures and obelic (or os incae) bones, stemming from delayed or incomplete that leaves persistent gaps or sutural at the obelion, often closing the third fontanel irregularly. These are less common and may relate to broader congenital defects like , underscoring the parietal bone's sensitivity to gestational factors.

Function

Protective role

The parietal bones, forming the superior and lateral aspects of the , play a critical role in safeguarding the from external by enclosing and supporting the underlying neural structures. As paired, elements, they contribute to the neurocranium's dome-like , which shields the , particularly the parietal lobes responsible for and spatial awareness. This protective enclosure prevents direct injury to the fragile during impacts, falls, or blunt force. The bone's trilayered composition enhances its biomechanical resilience: an outer table of dense compact bone, a central diploë of trabecular bone, and an inner table of compact bone. The outer table, typically thicker and denser than the inner, provides initial resistance to compressive forces, while the diploë acts as an energy-absorbing core, dissipating impact through its porous, lightweight structure that offers cushioning and . This sandwich-like design functions akin to an engineering composite, distributing and attenuating forces to minimize transmission to the brain's and . Additionally, the parietal bone's slight convexity on the external surface and concavity internally, combined with its articulations via interlocking cranial sutures, further optimize force deflection and . The curved helps redirect lateral and superior impacts, reducing localized stress concentrations and promoting even load distribution across the vault. These features collectively ensure the bone's durability, with variations in thickness (up to 7-8 mm in adults) correlating with enhanced protection in high-risk areas like the parietal eminence.

Attachment sites

The parietal bone serves as an attachment site for several key structures, primarily on its external and internal surfaces, facilitating muscular support, dural reflections, and vascular passages. On the external surface, the superior temporal line provides attachment for the , which envelops the and spans from the to the parietal and temporal bones. Inferior to this, the inferior temporal line marks the origin of the fibers, contributing to the muscle's broad attachment area that extends onto the frontal and temporal bones for mandibular elevation during mastication. These temporal lines arch across the convex external surface, with the inferior line serving as the primary muscular anchorage point on the parietal bone. The internal surface, which is concave and molded to the cerebral contours, features grooves and borders that accommodate dural and vascular structures. Along the superior border, the sagittal sulcus houses the and provides attachment for the , a dural fold that separates the cerebral hemispheres and runs from the to the internal occipital protuberance. Arachnoid granulations project into this groove, facilitating drainage into the venous system. Near the posterior angle, a shallow groove for the appears, while the tentorium cerebelli, another dural reflection that divides the from the , attaches at the posteroinferior angles of the parietal bone. Additionally, branching grooves for the traverse the anteroinferior region, supplying the and calvaria. The parietal foramen, typically located near the posterosuperior aspect of the internal surface (often corresponding to the external surface's midpoint), transmits connecting the to extracranial veins, as well as branches of the occipital artery. These attachments collectively anchor the parietal bone within the cranial framework, supporting both mechanical stability and neurovascular integrity.

Clinical significance

Fractures and trauma

The parietal bone is the most frequently fractured bone in the skull, accounting for a significant portion of cranial injuries in both adults and children due to its exposed lateral position. Linear fractures, which are non-displaced cracks without bone fragmentation, represent the majority of parietal bone injuries and often result from low- to moderate-energy impacts. These fractures typically heal without intervention but serve as markers for potential underlying brain trauma, necessitating thorough neurological evaluation. In adults, parietal fractures commonly arise from high-impact events such as collisions (20-25% of cases), falls from height (28-35%), and assaults, with the parietal region involved in up to 48% of depressed fractures. Depressed fractures, where fragments are driven inward by more than the thickness of the inner table (typically >5 mm), occur in severe and carry higher risks, particularly if compound (open to ) or associated with dural . In pediatric populations, the thinner, more pliable predisposes infants and young children to parietal fractures from falls, sports, or non-accidental , with simple linear parietal fractures being the most prevalent type in both accidental and inflicted injuries. Bilateral parietal fractures in infants raise suspicion for , though they can result from accidental mechanisms like compression or double impacts. Diagnosis relies on non-contrast computed tomography (CT) as the gold standard, which detects linear fractures with high sensitivity and identifies associated intracranial injuries; skull radiographs are less reliable and reserved for resource-limited settings. Clinical assessment includes Glasgow Coma Scale (GCS) scoring, with scores of 13-15 predicting good outcomes in 97% of depressed fracture cases, while GCS ≤8 correlates with poorer recovery. Management of linear parietal fractures is conservative, involving hospital observation, pain control, and serial neurological exams, with most patients discharged within days if no complications arise. Depressed or compound fractures require surgical intervention, such as elevation, , and dural repair, especially if contaminated, causing neurological deficits, or involving (CSF) leaks; early surgery (within 24-48 hours) improves outcomes in 81% of cases for patients aged 20-40 years. Antibiotics and prophylaxis are standard for open wounds, and anticonvulsants may be used prophylactically in high-risk scenarios. Complications include (e.g., epidural or in 30-55% of associated cases), (up to 10% in open fractures), posttraumatic seizures (5-10% risk), and rare growing fractures in children where leptomeningeal cysts form at the site. Dural involvement worsens , leading to poor outcomes in 35% of cases, while contusions or multiple fractures further elevate mortality and morbidity. In skull base-associated parietal fractures, seen in 11% of pediatric cases, or bleeding occurs in up to 55%, with succeeding in 75% but surgical needs in 25%. Overall, isolated parietal fractures have a favorable , with >90% good recovery in uncomplicated linear cases, but associated brain injury drives , emphasizing multidisciplinary care to mitigate long-term neurological deficits.

Surgical and pathological aspects

The parietal bone is susceptible to various pathological s, ranging from congenital defects to acquired lesions. Enlarged parietal foramina, also known as persistent parietal foramina, represent a rare inherited disorder characterized by symmetrical, circular openings in the parietal bones that fail to close during fetal development, typically measuring from a few millimeters to several centimeters in diameter. This arises from mutations in the MSX2 or ALX4 genes, which encode transcription factors essential for cranial , affecting approximately 1 in 15,000 to 50,000 individuals in an autosomal dominant pattern with variable . Most cases are asymptomatic, but complications may include scalp defects, increased susceptibility to skull fractures or brain injury from due to weakened bone integrity, and occasional neurological issues such as seizures or headaches from pressure on the openings. Acquired pathological conditions of the parietal include fractures, tumors, and rare osteolytic disorders. Depressed fractures involving the parietal often result from high-impact and can lead to underlying dural tears, contusions, or hematomas if the depression exceeds the inner table by more than 5 mm. Benign tumors such as cavernous hemangiomas, which constitute less than 1% of tumors and preferentially affect the parietal in the fourth decade of life, present as expansile lytic lesions causing localized , headaches, or cosmetic deformities, sometimes precipitated by prior . , an even rarer entity involving progressive osteolysis due to intraosseous vascular proliferation, can manifest as a painless, enlarging calvarial defect in the parietal region, with fewer than 150 reported cases worldwide. Isolated parietal defects, potentially from defective or neural tube separation issues, may associate with encephalomalacia or , necessitating thorough to rule out intracranial abnormalities. Surgical interventions for parietal bone pathologies prioritize restoration of cranial integrity, prevention of complications, and access to underlying structures. For depressed parietal fractures, especially in children or cases with contamination, dural laceration, or , elevation via craniectomy is indicated to debride, irrigate, and repair the dura, followed by potential using autologous bone or synthetic materials like . In infants, minimally invasive techniques such as burr hole elevation may suffice for non-compound depressions, while open reduction is reserved for significant displacements or associated hematomas. of the parietal bone, often performed through a horseshoe incision and burr holes along the superior temporal line, provides access to supratentorial lesions like parafalcine tumors or the atrium of the lateral ventricle via a transulcal approach, guided by landmarks such as the intraparietal point (5 cm lateral to the and 6 cm anterior to ). This procedure spares eloquent motor and sensory cortices using neuronavigation or intraoperative mapping to minimize risks like injury to the or vein of Labbé. Tumor resection in the parietal bone, as seen in cavernous hemangiomas or , typically involves en bloc excision with tumor-free margins to alleviate symptoms and achieve , confirmed histopathologically post-surgery. For congenital defects like enlarged foramina, surgery is rarely required unless complicated by or neurological deficits, in which case reinforces the weakened area. Overall, perioperative outcomes, including transfusion needs and hospital length of stay, correlate with parietal bone thickness; in pediatric spring-mediated for sagittal , thicker bones are associated with higher risks of blood loss and transfusion. Postoperative monitoring focuses on prevention through antibiotics and care, with most uncomplicated cases allowing discharge within a week.

Comparative anatomy

In mammals and other vertebrates

In mammals, the parietal bones consist of a pair of flat, curved membrane bones that form the majority of the cranial vault's roof and lateral walls, articulating anteriorly with the frontal bones, posteriorly with the , inferiorly with the temporal and sphenoid bones, and meeting each other along the . These bones develop through from mesodermal , with contributions from cells in the rostral portion in some species like mice, and they expand to accommodate the enlarged braincase characteristic of mammalian evolution. In derived mammals, such as humans and rabbits, the parietals remain distinct throughout life, providing structural support and attachment for temporalis muscles, though they may fuse with adjacent bones in certain taxa like monotremes. In reptiles, the parietal bones are prominent dermal elements of the roof, typically paired and meeting along the midline, but they are often larger relative to the braincase compared to mammals, bordering the temporal fenestrae in diapsids such as and snakes. These bones articulate with frontals anteriorly, squamosals laterally, and occipitals posteriorly, contributing to the kinetic or akinetic skull configurations; for instance, in and crocodilians, they form a robust, fused . Homologically, reptilian parietals derive from the same dermal armor precursors as in early tetrapods, with mesodermal origins predominant, and they lack the extensive involvement seen variably in mammals. Birds exhibit parietal bones that are reduced and fuse early in development with the frontal and other cranial elements, resulting in an obliterated and a single, solid frontoparietal complex in adults, which supports the lightweight, akinetic adapted for flight. This pattern, observed in like chickens and pigeons, contrasts with the distinct parietals of mammals and reflects evolutionary modifications for reduced weight while maintaining protection, with the parietals forming part of the expanded orbital and temporal regions. In amphibians, the parietal bones are present as paired dermal roof elements but frequently fuse with the frontals to form a frontoparietal bone, particularly in anurans like frogs, creating a simplified, anapsid-like skull without temporal fenestrae. In urodele amphibians such as salamanders, they remain more distinct, articulating with surrounding bones via sutures that persist into adulthood, developing through intramembranous ossification similar to that in amniotes. Evolutionarily, amphibian parietals represent a transitional form, homologous to those in reptiles but adapted to a more flexible, aquatic-terrestrial lifestyle with variable neural crest contributions. Among fish, true parietal bones are absent, as the skull roof is instead composed of other dermal bones like the supraoccipital or extrascapulars in actinopterygians, reflecting the divergent evolution of the chondrocranium and dermatocranium without the expanded vault seen in tetrapods. In basal vertebrates like placoderms, elements homologous to parietals may appear as part of the lateral line-associated dermal armor, but these do not persist in modern teleosts, underscoring the parietal's emergence as a tetrapod innovation.

In reptiles and dinosaurs

In reptiles, the parietal bones are paired dermal elements that form the posterior portion of the skull roof, positioned dorsal to the case and immediately posterior to the frontal bones, where they typically meet along a midline suture. These bones contribute to enclosing the and supporting surrounding dermal roofing elements, with their shape and size varying by group to accommodate differences in cranial architecture. In many lineages, the parietals fuse medially, enhancing structural integrity, and often bear a parietal (pineal) in the midline, which transmits the parietal associated with the pineal organ or "" for photoreception and . Variations in parietal reflect diversity. In crocodilians and basal amniotes, the parietals frequently fuse with the frontals to form a composite frontoparietal , creating a solid . Squamates, such as and , retain distinct paired parietals that remain unfused with adjacent elements, allowing for greater cranial flexibility in kinetic skulls. In (Testudines), the parietals form part of the primary roof but may integrate with postfrontals and squamosals to produce a secondary roofing layer in more primitive species, adapting to the encased cranial design. These differences underscore evolutionary adaptations in skull rigidity and sensory function across reptilian clades. Dinosaurs, as archosauromorph reptiles, exhibit parietal bones that align with this general reptilian pattern but show clade-specific elaborations. The parietals are paired, flat to slightly convex bones forming the posterior midline of the skull roof, posterior to the frontals and contributing to the overall enclosure of the braincase. A pineal foramen is commonly present on the fused parietals, suggesting retention of parietal eye functionality similar to other reptiles. In ceratopsian dinosaurs, such as Triceratops, the parietals are dramatically expanded posteriorly to form the central midline of the iconic frill—a broad, bony shelf that likely served in display and defense—while remaining paired but tightly sutured. In contrast, sauropod and theropod dinosaurs typically feature more modest parietals integrated into the supratemporal fenestrae borders, supporting jaw musculature attachments without extensive expansions. These features highlight how parietal morphology in dinosaurs balanced neuroprotection with biomechanical and behavioral demands.

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