A. Schlemmer et al., MORNING OR EVENING ADMINISTRATION OF NASAL CALCITONIN - EFFECTS ON BIOCHEMICAL MARKERS OF BONE TURNOVER, Bone, 20(1), 1997, pp. 63-67
The purpose of this study was to examine the effect of intranasal salm
on calcitonin (sCT) administration (200 IE), given either in the morni
ng (8:00) or evening (21:00), on the known circadian variation in bioc
hemical markers of bone turnover. An open, placebo-controlled, randomi
zed, crossover study, with three 24 h studies of blood samples drawn e
very third hour and urine collected in 3 h aliquots was undertaken. Su
bjects consisted of nine healthy postmenopausal women, aged 58 +/- 7 y
ears. Urinary CrossLaps (a measure of bone resorption) was measured by
ELISA and corrected for creatinine (Cr), Serum osteocalcin (sOC) was
measured by radioimmunoassay (RIA). The first 24 h study was performed
without intervention. Prior to this control study the participants we
re randomized to either morning (8:00) or evening (21:00) sCT (200 LE)
, sCT administrations were given 4-5 days prior to and during the seco
nd study, After a washing-out period of 2 weeks the participants were
given 200 IE of sCT at the reverse time of the day 5 days prior to and
during the third study. At all timepoints, urinary CrossLaps/Cr exhib
ited a significant (p < 0.001) circadian rhythm with its zenith in ear
ly morning and nadir in late afternoon. Both morning and evening admin
istration of sCT significantly decreased the urinary excretion of Cros
sLaps/Cr approximately 3-6 h after administration with a subsequent re
bound effect, sOC did not exhibit a significant circadian variation an
d was not affected by the calcitonin. The 24 h mean urinary CrossLaps/
Cr and sOC remained unchanged. Both morning and evening sCT significan
tly decreased the urinary excretion of CrossLaps/Cr 3-6 h after admini
stration, with a rebound effect approximately 12 h later. However, the
present study does not indicate that neither evening nor twice-daily
administration is superior to morning administration. (C) 1997 by Else
vier Science Inc.