D. Alais et al., THE CONTRIBUTION OF ONE-DIMENSIONAL MOTION MECHANISMS TO THE PERCEIVED DIRECTION OF DRIFTING PLAIDS AND THEIR AFTEREFFECTS, Vision research, 34(14), 1994, pp. 1823-1834
When motion aftereffects (MAEs) are measured by adapting to a drifting
plaid (simultaneous adaptation) or by adapting to the plaid's compone
nt gratings in alternation (alternating adaptation), it has been shown
that the velocity and duration of the MAE are smaller in the latter c
ase [Wenderoth, P., Bray, R. and Johnstone, S. (1988) Perception, 17,
81-91; Burke, D. and Wenderoth, P. (1993) Vision Research, 33,351-359]
. However, Burke and Wenderoth additionally reported that the directio
ns of MAEs induced by simultaneous and alternating adaptation were ide
ntical, an apparent inconsistency if the differences in duration and v
elocity were due to the presence of ''blobs'' at the component grating
intersects in the simultaneous case. Presumably, the direction of the
''blobs'' should also affect perceived plaid direction during adaptat
ion and, hence, the MAE direction. In five experiments, we have measur
ed both perceived adapting plaid and MAE direction, tested with both a
lternating and simultaneous adaptation, measured interocular transfer
of plaid-induced MAEs and obtained MAE and plaid direction judgments u
nder monocular and binocular viewing conditions. All of the data indic
ate that there is a blob tracking mechanism which is preferentially st
imulated by plaids whose component gratings have high spatial frequenc
y, low temporal frequency and high contrast. Differences between simul
taneous and alternating adaptation emerge only when more optimal blobs
are used, thus accounting for Burke and Wenderoth's failure to find a
difference. The data also support Burke and Wenderoth's claim that th
e blob tracking mechanism is monocular: alternating and simultaneous a
daptation produce identical MAEs under interocular transfer conditions
, even using plaids with more optimal blobs, We also report the unexpe
cted finding that plaids with more- and less-optimal blobs appear to d
rift in directions 20 degrees apart yet their aftereffects differ in d
irection by only 3-5 degrees. That is, more optimal blob plaids-compar
ed with less optimal blob plaids-change both perceived plaid direction
during adaptation and subsequent perceived MAE direction but the latt
er change is much more modest. Possible explanations of this dissociat
ion are considered.