MSI dipole variability mean unreliability?

MSI dipole variability mean unreliability?

Clinical Neurophysiology xxx (2014) xxx–xxx Contents lists available at ScienceDirect Clinical Neurophysiology journal homepage: www.elsevier.com/lo...

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Clinical Neurophysiology xxx (2014) xxx–xxx

Contents lists available at ScienceDirect

Clinical Neurophysiology journal homepage: www.elsevier.com/locate/clinph

Letter to the Editor Does MEG/MSI unreliability?

dipole

variability

mean

The field of a magnetoencephalography (MEG)/magnetic source imaging (MSI) (Cohen, 1968) has grown considerably over the last 45 years. As clinicians worldwide know, thousands of patients with epilepsy have benefited directly from the insight about their epileptic foci provided by MEG/MSI (Bagic et al., 2009). Taken together, one gets the impression that MSI should be considered a mature clinical field by now (Bagic, 2011). Thus, it remains perplexing why MEG/MSI has, in some minds, not earned the status of a ‘‘routine’’ clinical test. Have there not been a number of clinical studies (Knowlton et al., 2008a,b, 2009; Sutherling et al., 2008; etc.) proving its additive value to non-invasive presurgical evaluations of patients with medically-resistant epilepsy? Or is it simply because epilepsy clinicians are traditionally conservative and leery of new technology? Alternatively, could a negative bias be continuing to play a role? Wennberg and Cheyne (2013a) have attempted to examine the ‘‘reliability’’ of MEG source localization using a single, supposedly ‘‘well-characterized’’, temporal neocortical spike focus. Their hypothesis is that the scatter of dipoles of individual spikes reflects a localization imprecision of MEG methodology. In the process of this investigation, the authors did corroborate the usefulness of several procedures that are known to improve source modeling accuracy, such as bandpass filtering and spike averaging to enhance the signal to noise (S/N) of an MEG or EEG spike. However, their welcomed recommendations for the routine use of these protocols are in contrast to several areas of concern, namely their insistence on the ‘‘identical’’ nature of their recorded spikes, their somewhat misleading use of the term ‘‘reliability’’, and their conclusion that the source of dipole location variability from spike to spike is due to ‘‘the limitation in spatial accuracy of the source localization technique’’. The authors’ stated objective was ‘‘to assess the reliability of magnetic source imaging (MSI) of anterior temporal spikes through detailed analysis of the localization and orientation of source solutions obtained for a large number of spikes that were separately confirmed by intracranial EEG (ICEEG) to be focally generated within a single, well-characterized spike focus’’. Unfortunately, ‘‘reliability’’ can be an emotionally charged word, when used in a clinical setting. It infers that one is attempting to determine whether the results of a test, or indeed the procedure itself, are trustworthy. Perhaps, ‘‘consistency’’ or ‘‘variability’’ would be a more neutral term? Inferences aside, the term, reliability, might have been justified had they really been able to do repeated source localizations on identical spikes, but that is a physiological impossibility (Ebersole, 2003; Spencer et al., 2008; Haider and McCormick, 2009; Sabolek et al., 2012). Even in idealized cases of nearly identical spikes, it is the background MEG or EEG activity, unrelated to the spikes

themselves, that is always variable and represents ‘‘noise’’ in this situation (Bast et al., 2004, 2006; de Jongh et al., 2005; Ramantani et al., 2006). Background noise is a key determinant of dipole scattering. Clearly, that is why spike averaging, just like evoked potential averaging, works to improve the S/N (Scherg et al., 1999; Ebersole, 2003; Ramantani et al., 2006). Furthermore, spike foci that produce scalp-recordable spikes are quite large in area (Cooper et al., 1965; Ebersole, 2003; Tao et al., 2005) and have within them complex neural networks (van Diessen et al., 2013). All these elements are unlikely to be involved to the same extent and with identical synchrony from spike to spike. Thus, there is also some intrinsic variability in the signal, that would also contribute to dipole scattering (Scherg and Ebersole, 1993, 1994; Murro et al., 1995; Braun et al., 1997; Ebersole, 2000, 2003). Accordingly, the authors’ persistent use of the expression, ‘‘identical spikes’’, is clearly inaccurate. It would appear that the authors’ claim of identical spikes was based principally on intracranial EEG recordings. Unfortunately their intracranial spatial sampling, using only a total of 16 contacts (three 4-contact subdural strips and one 4-contact depth electrode), is hardly optimal and cannot justify their claim of ‘‘complete characterization’’ of this anterior temporal focus. The four-contact strip on the lateral surface of the temporal tip, that recorded nearly all the spike activity, provided only an impression of the AP dimension of the focus. There was no coverage of the basal, superior, or mesial aspect of the temporal tip. This is not sufficient to claim that ‘‘all the spikes have an identical source’’. Similarly, only using 19 10–20 electrodes (without subtemporal coverage) to compare and equate scalp EEG spikes recorded with simultaneous ICEEG to those recorded with simultaneous MEG is also inadequate. Note that the EEG field maps in their Fig. 1 do not resolve either the negative or the positive field maxima, let alone any other variability in the subtemporal fields. Accordingly, it is very unlikely that by ‘‘careful visual inspection’’ they could be certain that the spikes recorded with ICEEG were identical to those recorded with MEG. Finally, the authors themselves provide us with a glimpse of the variability in their studied spike population. The tracings of raw EEG in Fig. 1 show a number example spikes that are far from identical. Regardless of what the authors stated, the spike population chosen for study was not ‘‘the classical anterior temporal spike’’ that originates in the infero-lateral and lateral aspect of the anterior temporal lobe (Ebersole and Wade, 1991; Ebersole, 2003), but rather it was a temporal tip spike, the field of which had principally a tangential, not radial, orientation. This was good for a study of MEG, given its sensitivity to tangential field orientations (Ebersole,1991; Fuchs et al., 1998; Murro et al., 1995; Nakasato et al., 1994; Scheler et al., 2007; Haueisen et al., 2012; Agirre-Arrizubieta et al., 2014). However, the EEG dipole solution for this interictal population was also not typical for classic anterior

http://dx.doi.org/10.1016/j.clinph.2014.01.037 1388-2457/Ó 2014 International Federation of Clinical Neurophysiology. Published by Elsevier Ireland Ltd. All rights reserved.

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Letter to the Editor / Clinical Neurophysiology xxx (2014) xxx–xxx

temporal spikes. These typically have a more radial orientation, are modeled by EEG dipoles that are usually two to three cm deep to the generating cortex (Ebersole and Wade, 1991; Ebersole, 2003). Accordingly, the authors should temper their claim that the results reflect the classic anterior temporal spike. Furthermore, it is curious that dipole scattering with EEG source imaging (ESI) was not included in the discussion, given that comparisons between MEG and EEG source imaging was one thrust of the paper. A number of studies using simultaneous MEG and EEG have shown that EEG dipole scatter is greater than that of MEG (Nakasato et al., 1994; Mikuni et al., 1997; Oishi et al., 2002; Zijlmans, 2002; Scheler et al., 2004, 2007; Ossenblok et al., 2007). MEG spike dipole clusters are nearly always smaller than EEG clusters of the same spikes and often smaller than that shown in this study. In fact, the authors themselves also show, in an accompanying study of ESI (Wennberg and Cheyne, 2013b), that dipole models of single EEG spikes vary widely in location with up to a third being ‘‘physiologically invalid’’. Given the known physiological variability in any spike focus (Cohen et al., 2002; Sabolek et al., 2012) and given the effect of variable background MEG (or EEG) activity on a resultant spike field (Ramantani et al., 2006), one cannot hypothesize, as did the authors, that ‘‘in this particular well characterized case of a focal spike generator, a reliable source localization technique should return an identical solution for each spike analyzed’’. Although some may believe that the extent of an MEG dipole cluster is related to the actual size of the epileptic focus, this is not the case with most experienced clinical MEG practitioners. However, a small dipole cluster does mean a stable interictal source (Ebersole, 1991, 2003), and this has been shown to be a good predictor of epilepsy surgery success (Otsubo et al., 2001; Chitoku et al., 2003; Assaf et al., 2004; Ebersole, 2003; Fischer et al., 2005; Oishi et al., 2006; Ramachandran-Nair et al., 2007; Agirre-Arrizubieta et al., 2014). Thus, this feature of an MSI result is useful clinically without having to believe that dipole cluster size infers knowledge about focus size. Perhaps what is most unfortunate about the authors’ conclusions is their insistence that MEG dipole scatter is a function of the ‘‘limitations in the spatial accuracy of the source localization technique’’. This might be justified if repeating a dipole localization of the same MEG spike leads to different results, but it does not. This conclusion also might have been given support had they shown that minor variations in spike parameters lead to inconsistent and unusually large variations in dipole location, but this was not shown. Such an investigation is worthy of future consideration. However, given the known relationship that signal and noise have with dipole variability and given the intrinsic physiological variability of individual spikes, we simply cannot accept the authors’ conclusion that the source modeling technique is to blame for dipole scatter. MEG/MSI is a proven, useful clinical tool. It may not be ‘‘the’’ answer; but it is ‘‘an’’ answer, along with other available functional methods for the question of where is the epileptogenic focus (Bagic et al., 2009). MEG/MSI does not replace EEG; rather it is complementary and additive to EEG (Ebersole et al., 1993; Fuchs et al., 1998; Ebersole and Ebersole, 2010). All clinicians want to utilize the best and most complete relevant information available before making important clinical decisions (Burgess et al., 2011a, 2011b). A balanced presentation of the related research findings has the critical role in helping them achieve this goal. It is unfortunate that the authors did not temper their negative position toward MEG source modeling, lest physicians seeking understanding be lead to believe falsely that MEG/MSI is clinically ‘‘unreliable’’.

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Anto Bagic´ University of Pittsburgh Comprehensive Epilepsy Center (UPCEC), UPMC MEG Epilepsy Program, Department of Neurology, University of Pittsburgh Medical School, Suite 811, Kaufmann Medical Building, 3471 Fifth Avenue, Pittsburgh, PA 15213, USA ⇑ Tel.: +1 412 692 4603; fax: +1 412 692 4636. E-mail address: [email protected] John S. Ebersole MEG and Functional Mapping Program, Atlantic Neuroscience Institute Epilepsy Center, 99 Beauvoir Avenue, Summit, NJ 07902, USA E-mail addresses: [email protected] Available online xxxx