The craniovertebral junction develops from somites that differentiate into sclerotomes around the notochord. The central pivot includes the dens, C2 vertebral body, and basiocciput. It is surrounded by the foramen magnum and atlantal rings. The proatlas, from the 4th occipital sclerotome, is important in development. Ossification of C2 occurs in three phases, with fusion completing by age 16-18. Abnormalities can result in instability or neural compression and include segmentation errors, assimilation, or developmental disorders affecting metabolism or inflammation.
2. Craniovertebral Junction
Divided into 2 portions:
● Central pivot
o Dens, C2 vertebral body, basiocciput
● 2 ringed structures surrounding central pivot
o Foramen magnum ring
clivus, exocciput, occipital condyles, opisthion
o Atlantal ring
3. Embryology
● Notochord forms early axial skeleton
● During 4th week gestation, 42 somites
formed
o 4 occipital, 8 cervical, 12 thoracic, 5 lumbar, 5
sacral, 8-10 coccygeal
● Each somite differentiates
o outer dermatome
o inner myotome
o medial sclerotome - form vertebrae around notocord
4 occipital sclerotomes
● 4th Occipital Sclerotome - Proatlas - important for CVJ
development
8. Posterior Fossa
● Expansion occurs by endochondral
reabsorption, sutural growth, & boney
accretion until 16-18 years of age
● Growth of basion elongated basiocciput &
lowers frontal margins of foramen magnum
● Downward displacement of cerebellum &
rotation of occipital and temporal lobes
causes resorptive drift down and backward
of opisthion
9. Development of C2
● Apical dens from proatlas
● Dens from 1st cervical sclerotome
● VB of C2 from 2nd cervical sclerotome
● Odotoid separate from VB at birth by
cartilaginous bands - 2 synchondroses
● 3 phases of synchondrosis & ossification
o 1st - 4mo fetus at VB/neural arches
o 2nd - 6mo fetus basal dental segment
ossification of lower syndrondrosis at birth
o 3rd - 3-5 yrs at apical dental segment
not completely fused to basal dens until 6-9 yrs
o Fully completed by age 16-18
11. Developmental Abnormalities
● In general abnormalities result in:
o Central pivot
instability
however, basilar impression & retroflexed
odontoid can cause neural compression
o 2 rings (atlas & axis)
deformity & crowding
however, hypoplasia/aplasia can cause
weakening/loss of ligamentous structures -
instability
12. Congenital Anomalies & Malformations
● Occipital bone
o Manifestations of occipital vertebra
clivus segmentations
remnants around foramen magnum
atlas variants
dens segmentations anomalies
o Basilar invagination
o Condylar hypoplasia
o Assimilation of atlas
13. Congenital Anomalies & Malformations
● Atlas
o Assimilation of atlas
o Atlantoaxial fusion
o Aplasia of atlas arches
● Axis
o Irregular atlantoaxial segmentation
o Dens dysplasias
Ossiculum terminale persistens
Os odontoideum
Hypoplasia-aplasia
o Segmentation failure of C2/3
14. Developmental & Acquired Abnormalities
● Foramen Magnum
o Secondar basilar invagination (Paget’s dz,
osteomalacia, rheumatoid cranial settling, Rickets)
o Foraminal stenosis (achondroplasia)
● Atlantoaxial Instability
o Errors in metabolism (Morquio’s syndrome)
o Down syndrome
o Infection (Grisel’s syndrome)
o Inflammatory (rheumatoid arthritis)
o Traumatic OA & AA dislocation, os odontoideum
o Tumors (NF)
Notes de l'éditeur
Congenital and developmental osseous anomalies and abnormalities that affect the craniovertebral complex can result in neural compression, vascular compromise, and can manifest with abnormal cerebrospinal fluid dynamics.
Resegmentation of somites to form sclerotomes and changes
of sclerotomal primordia to mature vertebral parts. The somitic and
primordial origins of vertebral parts and phenotypic parts are colour-
matched, and the locations of the somites, resegmented sclerotomes,
and vertebrae along the embryonic axis are approximately counter-
registered. During resegmentation, the sclerotome is formed from the
caudal and rostral halves of two adjacent somites, such that the middle
of the resegmented sclerotome lines up with the intersomitic cleft (IC).
Both the axial sclerotome (Scl-A) and lateral sclerotome (Scl-L)
develop dense and loose zones. The dense zone of the lateral
sclerotome (Ld) becomes the neural arch (NA) and pedicle (P), which
is attached to the rostral part of the vertebral body (VB) formed from
chondrification of the loose (Al) and part of the dense zones (Ad) of
the axial sclerotome. The rostral layer of the dense zone of the axial
sclerotome soon forms the intervertebral boundary zone (IBZ)
containing intervertebral boundary mesenchyme (IBM), which ulti-
mately forms the annulus (A) and, together with notochord remnants
(NC), the nucleus pulposus (NP) of the intervertebral disc (ID). The
loose zone of the lateral sclerotome (Ll) does not form bone but
promotes emergence of the nerve roots (NR). Thus, the neural arch is
derived from a single somite but the vertebral body receives
contributions from two adjacent somites. IV intersomitic vessel.
Arrows indicate developmental fates of the sclerotomes.
Formation of the human craniovertebral junction. Sclerotomal
primordia and their vertebral phenotypes are colour-matched. During
resegmentation, the caudal half of the fourth somite (fourth occipital
somite) and rostral half of the fifth somite combine to form the
proatlas sclerotome (PA). Derived from the proatlas are: the axial
zones (Ad and Al) which become the basion (B) of the basioccipital or
clivus (CL) and the apical segment of the dens (AD); the lateral dense
zone (Ld) becomes the exoccipital comprising the occipital condyle
(OC), and lateral rim and opisthion (OT) of the foramen magnum; the
proatlas’ hypochordal bow (HBp) forms the ventral clival tubercle
(CT). The C1 resegmented sclerotome (C1) comes from adjacent
halves of the fifth and sixth somites. Derived from the C1 sclerotome
are: the axial zones form the basal segment of the dens (BD); the
lateral zone forms the posterior atlantal arch (C1P); the hypochordal
bow (HBc) forms the anterior atlantal arch (C1A). The C2 resegmented
sclerotome (C2) comes from the sixth and seventh somites. From the
C2 sclerotome: the axial zone forms the C2 vertebral body (AB); the
lateral zone forms the neural arch of C2 vertebra. The intervertebral
boundary zone (IBZ) between the proatlas and C1 sclerotome forms
the upper dental synchondrosis (US) and the IBZ between the C1 and
C2 sclerotomes forms the lower dental synchondrosis (LS)
The three developmental phases of the axis (C2) and the three
waves of ossification. The primordia for the dens components are
assembled during the membranous phase. Upper and lower dental
synchondroses are shown as dense lines. First wave of ossification at
fourth foetal month consists of bilateral centres for the neural arches
and a single centre for the centrum. Second wave at sixth foetal month
At birth, the basal dental centres should have integrated in the midline
and begun to be fused to the centrum. Third wave of C2 ossification
occurs from 3 to 5 years post-natal life at the apical dental segment,
which does not become fused to the basal dens till the 6–9th year, and
fully formed during adolescence.