Chapter 7 Physiological and anatomical changes in childbirth
For labour to commence two things have to occur: the onset of coordinated uterine contractions and the softening of the uterine cervix. The critical factor for the increase in uterine activity is the rise in intracellular calcium, which activates phosphorylation of myosin and the creation of cross-bridges with actin, which results in the contraction of the myometrial cell. The cervical changes are due to a breakdown in collagen owing to the release of metalloproteinases and an increase in the water content. Prostaglandins and leukotrienes are involved in these physiological changes.
The fetus then has to negotiate the birth canal, propelled by contractions of the uterus. Factors that can delay or prevent this are:
THE PASSAGES
Bony pelvis
The bony pelvis is made up of four bones, the two innominate bones, the sacrum and the coccyx, united at three joints. When a woman stands erect, the pelvis is tilted forward. The pelvic inlet makes an angle of about 55 ° with the horizontal. The angle varies between individuals and between races; for example, black Africans have a lesser angle. An angle of more than 55 ° may make the descent of the fetal head into the pelvis difficult (Fig. 7.1).
The ‘true’ pelvis is bounded by the pubic crest, the iliopectineal line and the sacral promontory. An ‘ideal obstetric’ pelvis is described in Box 7.1 and the brim is shown in Figure 7.2. The true pelvis is cylindrical in shape, with a bluntly curved lower end, and is slightly curved anteriorly. Anteriorly the pubic bones form its boundary, measuring 4.5 cm. Posteriorly, the curve of the sacrum forms its boundary, measuring 12 cm. Laterally its walls narrow slightly distally (Fig. 7.3). The walls are penetrated by the obturator foramen anteriorly and the sciatic foramen laterally, which is divided into two parts by the sacrospinous and sacrotuberous ligaments.
Box 7.1 The ideal obstetric pelvis
Brim | Round or oval transversely |
No undue projection of the sacral promontory | |
Anterior–posterior diameter 12 cm | |
Transverse diameter 13 cm | |
The plane of the pelvic inlet not less than 55 ° | |
Cavity | Shallow with straight side-walls |
No great projection of the ischial spines | |
Smooth sacral curve | |
Sacrospinous ligament at least 3.5 cm | |
Outlet | Pubic arch rounded |
Subpubic angle > 80 ° | |
Intertuberous diameter at least 10 cm |

Fig. 7.3 The pelvic cavity. The right innominate bone has been removed in order to show the extent of the cavity.
For descriptive purposes the true pelvis can be divided into four zones. These are shown in Figure 7.4. The measurements of the zone of the inlet are shown in Figure 7.2. The zone of the cavity is wedge-shaped in profile and almost round in section. It is the most roomy part of the true pelvis, the anterior–posterior diameter measuring 13.5 cm and the transverse diameter 12.5 cm.
The zone of the midpelvis passes through the apex of the pubic arch, the spines of the ischia, the sacrospinous ligament and the tip of the sacrum. It is the smallest zone and its most important diameter is the ischial–bispinous diameter, which measures 10.5 cm. If this zone is contracted the fetal presenting part may not be able to rotate and may become arrested.
The zone of the outlet (Fig. 7.5) does not usually interfere with the birth unless the pubic rami are narrow, which reduces the intertuberous diameter. In these cases delay may occur and the soft tissues of the perineum may be torn and damaged.
The axis of the birth canal corresponds to the direction the fetal presenting part – usually the head – takes during its passage through the birth canal (Fig. 7.6).

Fig. 7.6 Inclination of the pelvic brim and the axis of the birth canal. The plane of the pelvic brim makes an angle of about 55 ° with the horizontal in the erect patient, and the plane of the outlet about 10 ° with the horizontal. The axis of the birth canal is angled, the alteration in direction occurring at the pelvic floor.
Factors influencing pelvic shape and size
Minor alterations in pelvic shape have been found in many women receiving routine radiological pelvimetry, but only in a few instances has the abnormality been found to delay the birth. Smaller women tend to have a smaller bony pelvis, but also tend to have smaller babies. More severe alterations occur in populations where rickets or osteomalacia are found, but are uncommon in the developed countries today.
Soft tissues of the female pelvis
These include the uterus, the muscular pelvic floor and the perineum. The anatomical details are described in Chapter 43.
Uterus
The uterus in pregnancy can be divided into three parts:
Upper uterine segment
This portion of the uterus consists of the fundus and that part of the uterus lying above the reflection of the vesico-uterine fold of peritoneum. During pregnancy it undergoes the greatest degree of myometrial hyperplasia and hypertrophy. In labour it provides the strong contractions that push the fetus along the birth canal.
Lower uterine segment
This portion of the uterus lies between the vesico-uterine fold of the peritoneum superiorly and the cervix inferiorly. During pregnancy the upper part of the cervix is incorporated into the lower uterine segment, which stretches to accommodate the fetal presenting part (Fig. 7.7). In late pregnancy, as the upper segment muscle contractions increase in frequency and strength, the lower uterine segment develops more rapidly and is stretched radially to permit the fetal presenting part to descend (Fig. 7.8). In labour the entire cervix becomes incorporated into the stretched lower uterine segment.

Fig. 7.7 Formation of the lower uterine segment based on the observations of CP Wendell-Smith. Cone, the condensation of muscle at the junction of the body of the uterus and the cervix; AIO, anatomical internal os; HIO, histological internal os.

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