Lin Chen1, Congbo Cai2, Tianhe Yang3, Jianzhong Lin3, Shuhui Cai1, Jiaxing Zhang4, and Zhong Chen1
1Department of Electronic Science, Xiamen University, Xiamen, People's Republic of China, 2Department of Communication Engineering, Xiamen University, Xiamen, People's Republic of China, 3Zhongshan Hospital, Xiamen, People's Republic of China, 4Department of Physiology and Neurobiology, Xiamen University, Xiamen, People's Republic of China
Synopsis
Environmental
factors may influence brain iron concentration. We investigated the changes of magnetic
susceptibility and R2* values of cerebral regions
especially in six deep gray matter nuclei of twenty-nine participants after high altitude
exposure for four weeks. The results show that the susceptibility values of gray
matter, especially in caudate nucleus, putamen, globus pallidus, substantia
nigra, red nucleus, increased significantly. Traditional R2*
maps verify the results of QSM evaluation except in red nucleus. Therefore, high
altitude hypoxia can lead to significant increase of cerebral iron
concentration.
Purpose
While iron plays important
roles in physiological functions and development of human brain, aberrant
deposition of iron is often associated with toxic free radical and pathological
damage.1 The pathologic mechanisms of iron deposition have been
actively investigated, but possible environmental factors, which may influence
brain iron concentration, has rarely been mentioned. Recent study discover that
acute exposure to high altitude (HA) hypoxia can cause disruption of the
blood-brain barrier (BBB) and thus iron deposition in cerebral regions.2
However, it has not been reported that whether prolonged acclimatization to HA
can cause iron deposition in brain. In present work, we aimed to investigate
the effects of HA acclimatization on iron concentration in cerebral tissue by quantitative
susceptibility mapping (QSM) and traditional R2*
measurement.Methods
Twenty-nine healthy participants (13 female, mean age = 20±0.8) were imaged on a 3T Siemens Tim Trio MRI scanner (Siemens, Erlangen,
Germany) at
sea level before their ascent to Qinghai-Tibet Plateau
(4200 m) and immediately after they returned from an expedition for 4 weeks. All
images were acquired with three-dimensional multi-echo gradient-recalled
sequence. The experimental parameters were: TR = 55 ms, TE1 = 3.6 ms,
8 echoes at ΔTE = 5.9 ms, flip
angle = 15°, slice thickness = 2
mm and acquisition matrix size = 256×256. The field map was estimated from the
multi-echo datasets using a nonlinear fitting algorithm followed by spatial
phase unwrapping and projection onto the dipole field was used for background
field removal. Finally, QSM was obtained by using morphology
enabled dipole inversion (MEDI) method.3 R2*
maps were reconstructed by mono-exponential fitting with all echoes of the GRE
magnitude images. To generate binary segmentation masks of cerebrospinal fluid
(CSF), white matter (WM), gray matter (GM) (Fig. 1A), we utilized FMRIB’s
automated segmentation tool (FAST) to process magnitude images of the first
echo. We obtained the regions of interest (ROIs) including caudate nucleus (CN), putamen (PT),
globus pallidus (GP), substantia nigra (SN), red nucleus (RN), and dentate nucleus (DN) by converting a
customized common atlas created in the Montreal Neurological Institute (MNI)
space to each individual participant space using FMRIB Software Library (FSL,
University of Oxford) (Fig. 1B). Paired t-tests were
performed to examine the differences of iron concentration in cerebral regions.Result
This work shows that no significant
variation can be observed in the susceptibility value of CSF after HA exposure.
Similarly, the susceptibility value of WM shows no significant difference after
altitude, no matter with or without referencing the susceptibility value of CSF
to zero. However, the susceptibility value of GM increases significantly after
HA exposure with (p < 0.05) and without (p < 0.001) referencing the
susceptibility value of CSF to zero (Fig. 2A). All susceptibility values in the
six GM nuclei relative to CSF (0.00 ppb) were examined. The susceptibility
values in CN, SN, RN (p < 0.01), PT and GP (p < 0.001) regions of 29
participants increase significantly after HA exposure in comparison with
counterpart in before-altitude group. Changes of the R2*
values within CN, PT, GP and SN regions verify the results of QSM evaluation.
However, the R2* value within the RN region fails to
demonstrate statistical difference between before- and after-altitude groups (Table 1).Discussion
Tissue iron serves as
the dominant source of magnetic susceptibility in GM.4 The recovery of oxygen
saturation (SaO2) after HA exposure in our clinical examination
eliminates the interference from SaO2 in brain iron investigation.
Therefore, the results indicate that iron levels increase in GM, especially in
CN, PT, GP, SN and RN nuclei with potential causes of increased degradation of
hemoglobin, minor increment in the permeability of BBB and increased oxidative
stress.5 The missed R2* value difference
in RN indicate the lower sensitivity of R2* map to iron
content distribution in comparison with QSM. This may be because R2*
map possesses poor resistance to magnetic field inhomogeneity and reflects the
summation of magnetic properties from local and surrounding tissues.6Conclusion
HA hypoxia can lead to
increase of brain iron concentration, especially in deep GM regions after HA
acclimatization, which should raise concern over cerebral impairment due
to activities in HA.Acknowledgements
This
work was supported by the National Natural Science Foundation of China under
Grants 11474236, U12322121, 81171331 and 81471630, the Specialized Research
Fund for the Doctoral Program of Higher Education of China under Grant
20130121110014, and Science and Technology Project of Fujian Province of China under
Grant 2016Y0078.References
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