Auris Nasus Larynx 39 (2012) 544–548
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Auris Nasus Larynx
journal homepage: www.elsevier.com/locate/anl
Benign paroxysmal positional vertigo showing sequential translations of four
types of nystagmus
Takao Imai a,*, Noriaki Takeda b, Atsuhiko Uno a, Arata Horii c, Tadashi Kitahara d,
Suetaka Nishiike a, Kayoko Higashi-Shingai e, Hidenori Inohara a
a
Department of Otorhinolaryngology - Head and Neck Surgery, Osaka University Graduate School of Medicine, 2-2 Yamadaoka, Suita-shi, Osaka 565-0871, Japan
Department of Otolaryngology, Tokushima University Graduate School of Medicine, Tokushima, Japan
Department of Otolaryngology, Suita Municipal Hospital, Osaka, Japan
d
Department of Otolaryngology, Osaka Rosai Hospital, Osaka, Japan
e
Department of Otolaryngology, Sumitomo Hospital, Osaka, Japan
b
c
A R T I C L E I N F O
A B S T R A C T
Article history:
Received 16 June 2011
Accepted 21 October 2011
Available online 15 November 2011
Objective: We report a case of benign paroxysmal positional vertigo (BPPV) showing sequential
translation of four types of nystagmus and discuss its pathophysiology.
Methods: The case was 65-year-old female. We analyzed her nystagmus three-dimensionally.
Results: At the first visit, she showed vertical-torsio nystagmus of the posterior canal type of BPPV (PBPPV) and subsequently showed recently reported geotropic nystagmus with a long time constant. Two
weeks later, she showed apogeotropic nystagmus of the horizontal canal type of BPPV (AH-BPPV) and
subsequently a geotropic nystagmus with a short time constant of the horizontal canal type of BPPV (GHBPPV).
Conclusions: Three kind of nystagmus, namely P-BPPV, AH-BPPV and GH-BPPV can be explained by the
otoconial debris hypothesis of the same ear. Finally, the recently reported geotropic nystagmus with a
long time constant may be explained by a reversible lesion such as the denatured cupula or utricular
imbalance of the same ear.
ß 2011 Elsevier Ireland Ltd. All rights reserved.
Keywords:
Benign paroxysmal positional vertigo
Apogeotropic
Geotropic
Three dimensional
Rotation vector
1. Introduction
Benign paroxysmal positional vertigo (BPPV) is caused by either
canalolithiasis or cupulolithiasis [1] and can theoretically affect
each of the three semicircular canals [1]. Torsio-vertical nystagmus
in patients with the posterior semicircular canal (PSCC) type of
BPPV (P-BPPV) is caused by canalolithiasis in PSCC [1]. Among the
horizontal semicircular canal (HSCC) type of BPPV (H-BPPV),
apogeotropic nystagmus in patients with H-BPPV (AH-BPPP) is
caused by cupulolithiasis on the cupula of HSCC [1]. Geotropic
nystagmus that is of limited duration with short time constant in
patients with H-BPPV (GH-BPPV) is caused by canalolithiasis in
HSCC [1]. Recently, another geotropic nystagmus that is persistent
with long time constant was reported, suggesting that it is caused
by the denatured cupula of less specific weight than the
surrounding endolymph in HSCC [2].
Translation from P-BPPV to H-BPPV occurs when canalolithiasis
moves from PSCC into HSCC [1]. Translation from AH-BPPV to
* Corresponding author. Tel.: +81 6 6879 3951; fax: +81 6 6879 3959.
E-mail address: imaitakao@hotmail.com (T. Imai).
0385-8146/$ – see front matter ß 2011 Elsevier Ireland Ltd. All rights reserved.
doi:10.1016/j.anl.2011.10.007
GH-BPPV also occurs during the transition from cupulolithiasis to
canalolithiasis in HSCC [3]. In this study, we report a case of BPPV
that showed sequential translations of four types of nystagmus:
torsio-vertical nystagmus of P-BPPV, the recently reported
geotropic nystagmus with long time constant, apogeotropic
nystagmus of AH-BPPV and geotropic nystagmus with short time
constant of GH-BPPV. We analyzed each nystagmus threedimensionally and discussed its pathophysiology.
2. Methods and subject
The case is 65-year-old female complaining of positioning
vertigo. We recorded positional and positioning nystagmus at her
first visit to our hospital and at her second visit two weeks later.
She had no canal paresis in the caloric test with no other
neurological signs. We did not perform canalith repositioning
maneuver at any of her visit.
Positional and positioning nystagmus of her left eye was
recorded on digital video (DV) with an infrared CCD camera
(RealEyes, Micromedical Technologies). In the present study, eye
movements were three-dimensionally described by rotation
vectors [4]. The analysis method of the eye rotation vector and
T. Imai et al. / Auris Nasus Larynx 39 (2012) 544–548
its accuracy has already been described elsewhere [3,5,6]. For the
space coordinates, the X axis parallel to the naso-occipital axis
(positive forward), Y axis parallel to the inter-aural axis (positive
left), and Z axis normal to the X–Y plane (positive upwards) were
defined. X, Y, and Z components mainly reflect roll, pitch, and yaw
components, respectively. We used the unit degree that is given as
2 tan 1(magnitude of rotation vector) to represent the eye position
as axis-angle representations [3]. Using r that is the rotation vector
of eye position and with the following formula: v = 2(dr/
dt + r dr/dt)/(1 + r2), we calculated the eye velocity v around
X, Y, and Z axes [4]. We then extracted the slow phase eye velocity
(SPEV) of nystagmus by the method based on a fuzzy set approach
[3]. Using the least squares method, SPEV against time was
approximated exponentially. Finally, the time constant was
calculated as the reciprocal of the coefficient of time [3].
3. Results
At the patient’s first visit, she showed torsio-vertical nystagmus
with clockwise and upward direction of its fast phase seen in
patients with right P-BPPV [1], when she tilted her head backward
in the sitting position (Fig. 1A). The maximum SPEV and time
constant of the torsio-vertical nystagmus was 36.58/s in X
component and 2.4 s in X component, respectively (Fig. 3A ).
The axis angles of SPEV of the nystagmus were plotted along the
axis perpendicular to the plane of right PSCC (Rp) [7] on XY, XZ and
YZ planes (Fig. 4A). She then showed the similar, but fatigued
nystagmus with slower maximum SPEV (18.48/s in X component)
with the same short time constant (2.7 s) in right Dix-Hallpike
maneuver (from sitting to right head hanging position) [1]
(Fig. 3A ). Therefore, canalolithiasis was suggested in right PSCC.
But, in left Dix-Hallpike maneuver, she showed leftward
horizontal nystagmus (Fig. 3A ). Thereafter, she showed the
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recently reported geotropic nystagmus with long time constant in
supine position [2]. When her head was turned to right lateral
position in supine, she showed rightward horizontal nystagmus
with much longer time constant (183.3 s) (Figs. 1B and 3A ).
When her head was turned to left lateral position in supine, she
showed leftward horizontal nystagmus again with the same long
time constant (1642.0 s) (Figs. 1C and 3A ).
Two weeks later, she visited our clinic again and showed
leftward and rightward horizontal nystagmus, when she tilted her
head forward and backward in the sitting position, respectively
(Fig. 2A and B). Such nystagmus was seen in patients with AH-BPPV
where cupulolithiasis induced apogeotropic nystagmus with long
time constant in the supine position [8]. The time constant of the
leftward and rightward horizontal nystagmus was as long as 20.1
and 25.9 s, respectively (Fig. 3B and ). Actually, she showed
leftward horizontal nystagmus with time constant of 13.9 s, when
her head turned to right lateral position in supine (Figs. 2C and 3B
first ). The axis angles of SPEV of the nystagmus were plotted
along the axis perpendicular to the plane of left HSCC (Lh) [7] on XY,
XZ and YZ planes (Fig. 4B). Because nystagmus induced by the
ampullofugal inhibition of right HSCC rotates around the plane of
left HSCC [9], cupulolithiasis was suggested in right HSCC.
Thereafter, she showed geotropic nystagmus seen in patients
with GH-BPPV where canalolithiasis in HSCC induced geotropic
nystagmus with short time constant in the supine position. When
her head turned to left lateral position in supine, she showed
leftward horizontal nystagmus with short time constant of 8.7 s
(Figs. 2D and 3B ). When her head turned to right lateral position
in supine, she showed rightward horizontal nystagmus with short
time constant of 5.2 s (Figs. 2E and 3 second ). The maximum
SPEV of the rightward horizontal nystagmus was 191.88/s in Z
component (Fig. 3B second ), which was greater than that of the
leftward horizontal nystagmus (34.78/s) (Fig. 3B ). Because
Fig. 1. Axis angles of the eye position in the patient at her first visit to our hospital. (A) When she tilted the head backward, she showed torsio-vertical nystagmus with
clockwise and upward fast phase direction. (B) When she turned the head to right lateral position in supine, she showed horizontal nystagmu with a rightward fast phase
direction. (C) When she turned to left lateral position in supine, she showed horizontal nystagmus with a leftward fast phase direction. Inserted figures show her head position
and her right PSCC or HSCC with otocanial debris (). The direction of the arrow near the eye of the inserted head figures shows the direction of her nystagmus.
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T. Imai et al. / Auris Nasus Larynx 39 (2012) 544–548
Fig. 2. Axis angles of the eye position of her nystagmus at her second visit to our hospital. (A) When she bowed the head, she showed horizontal nystagmus with a leftward fast
phase direction. (B) When she tilted the head backward, she showed horizontal nystagmus with a rightward fast phase direction. (C) When she turned to right lateral position
in supine at first time, she showed horizontal nystagmus with a leftward fast phase direction. (D) When she turned the head to left lateral position in supine, she showed
horizontal nystagmus with a leftward fast phase direction. (E) When she turned the head to right lateral position in supine at second time, she showed horizontal nystagmus
with a rightward fast phase direction.
geotropic nystagmus is stronger when the head turned to the side
of the affected ear [8], canalolithiasis was suggested in right HSCC.
Three weeks after the first visit, her positional and positioning
nystagmus had disappeared and she did not complain of any
dizziness and/or vertigo, as this condition was generally realized as
self limiting.
4. Discussion
At the first visit of the patient, she showed torsio-vertical
positioning nystagmus and axis angles of its SPEV were plotted
along the axis perpendicular to the plane of right PSCC. As
demonstrated by Suzuki and Cohen the electrical stimulation of
Fig. 3. Axis angles of SPEV of her nystagmus. (A) At her first visit to our hospital. (B) At her second visit to our hospital. After the point of second
, the scale of eye velocity in Z
Head backward in the sitting position,
component was different from other part. The number enclosed by square represents the time constant. The unit was second.
head to the upright sitting position,
from sitting to right head hanging position,
left head hanging position,
head in right lateral position in supine,
head in left
head bowed in the sitting position, and
head in centered position in supine.
lateral position in supine,
T. Imai et al. / Auris Nasus Larynx 39 (2012) 544–548
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Fig. 4. The axis angles of SPEV are plotted in XY, XZ, and YZ planes. (A) Head backward at her first visit to our hospital. The axis angles of SPEV were plotted around the axis
perpendicular to the plane of right PSCC (Rp). (B) Head in right lateral position in supine at her second visit to our hospital. The axis angles of SPEV were plotted around the axis
perpendicular to the plane of left HSCC (Lh). Dotted line, the averaged rotation axis of SPEV. Ra, axis perpendicular to the plane of the right anterior semicircular canal; Rh, axis
perpendicular to the plane of the right HSCC; Rp, axis perpendicular to the plane of the right PSCC; La, axis perpendicular to the plane of the left anterior semicircular canal; Lh,
axis perpendicular to the plane of the left HSCC; Lp, axis perpendicular to the plane of the left PSCC [7].
single semicircular canal afferents induced eye movements around
the plane of the canal in cats and monkeys [10,11], it is suggested
that the torsio-vertical nystagmus originated from right PSCC.
Taken together with the observations that the time constant of
SPEV declination of the nystagmus was short (2.4 s) with SPEV
fatigability after repeated positioning maneuver, these findings led
to the diagnosis of right P-BPPV, suggesting canalolithiasis in PSCC
of the right ear.
At her second visit, she showed apogeotropic positional
nystagmus. Axis angles of SPEV of leftward horizontal nystagmus at right-side-down head position in supine were plotted
along the axis perpendicular to the plane of left HSCC. Because
nystagmus induced by the ampullofugal inhibition of right HSCC
rotates around the plane of left HSCC [9], the leftward horizontal
nystagmus was suggested to originate from right HSCC. Taken
together with its time constant (13.9 s), these findings led to the
diagnosis of right AH-BPPV, suggesting cupulolithiasis on the
cupula of right HSCC. Translation from torsio-vertical nystagmus
to apogeotropic nystagmus in the patient suggested that
otoconial debris in the right PSCC as canalolithiasis moved into
HSCC were attached on the cupula of the same ear. Translation
from P-BPPV to H-BPPV in the same ear was reported previously
[1].
Thereafter, she showed geotropic nystagmus in the supine
position with short time constant and rightward horizontal
nystagmus stronger than left one. These findings led to the
diagnosis of right GH-BPPV, suggesting canalolithiasis in right
HSCC. It is suggested that translation from apogeotropic
nystagmus to geotropic nystagmus was due to displacement of
otoconial debris from the cupula into the canal of the right HSCC.
Such translation from AH-BPPV to GH-BPPV was reported
previously [3].
In the present study, we analyzed patient’s nystagmus threedimensionally and found that she sequentially suffered from PBPPV, AH-BPPV and GH-BPPV within 2 weeks. The pathophysiology was suggested as follows: otoconial debris dislodged from the
otolith organ of the right ear dropped firstly into PSCC to be
canalolithiasis of P-BPPV. Then, the otoconial debris moved into
HSCC and was attached on its cupula to be cupulolithiasis of AHBPPV. Thereafter, they were displaced from the cupula to the canal
of HSCC of the right ear to be GH-BPPV.
The patient showed the recently reported geotropic nystagmus
with long time constant after disappearance of torsio-vertical
nystagmus of P-BPPV at her first visit [2]. The nystagmus may be
explained by the denatured cupula of less specific weight than the
surrounding endolymph in HSCC [2]. Geotropic nystagmus with
long time constant might be explained by the otolith imbalance
hypothesis. Accordingly, since otoconial debris is considered to be
dislodged from the utricle [1,12], imbalance of utricular function
reported in patients with BPPV [12] may induce geotropic
nystagmus with long time constant [13]. The imbalance of
utricular fuciton causes asymmetry of horizontal eye movement
during otolith vestibulo-ocular reflex [14]. The suggested lesion
such as the denatured cupula or utricular imbalance might have
been of benign nature [15] because of disappearance of the
nystagmus after three weeks at her first visit.
In conclusion, we showed a case of BPPV that showed
sequential translations of four types of nystagmus: torsio-vertical
nystagmus of P-BPPV, the recently reported geotropic nystagmus
with long time constant, apogeotropic nystagmus of AH-BPPV and
geotropic nystagmus with short time constant of GH-BPPV. Three
kind of nystagmus except the recently reported geotropic
nystagmus with long time constant can be explained by the
otoconial debris hypothesis of the right ear. The recently reported
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T. Imai et al. / Auris Nasus Larynx 39 (2012) 544–548
geotropic nystagmus with long time constant may be explained by
reversible lesion such as the denatured cupula or utricular
imbalance of the same ear.
Conflict of interest
None.
Acknowledgement
This study was supported by a Grant-in-Aid for Scientific
Research from the Ministry of Education, Culture, Sports, Science,
and Technology of Japan.
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