g , Brandt and Stark, 1997, Johansson et al , 2012 and Spivey and

g., Brandt and Stark, 1997, Johansson et al., 2012 and Spivey and Geng, 2001). Further support comes from neuropsychological studies that have demonstrated links between the Frontal Eye Field (FEF) and spatial working memory performance (e.g., Cabeza and Nyberg, 2000, Campana et al., 2007 and Gaymard et al., 1999), while experiments in non-human

primates suggest activation in oculomotor regions such as FEF signals the location of memorized targets even after they have disappeared (Bruce and AZD5363 molecular weight Goldberg, 1985 and Sommer and Wurtz, 2001). However, an alternative to the eye-movement theory is that VSWM relies on shifts in covert spatial attention (i.e., the see more ability to shift attention to locations without executing any overt eye movement). For example, Awh and Jonides, 2001 and Awh et al., 1998 found reaction times were faster when targets

appeared at locations held in working memory, and that participants’ spatial working memory was disrupted when they were prevented from attending to memorized locations during a retention interval. Furthermore, Godijn and Theeuwes (2012) report that memory for a sequence of locations indicated by numbered peripheral items is unaffected by requiring participants to maintain fixation, in comparison to a condition in which they are free to execute overt eye movements during a retention interval. Conversely, however, Belopolsky and Theeuwes

have reported being unable to find evidence that spatial attention interacts with spatial working memory during performance of a match to sample task (2009a). We argue that there are several reasons why previous studies in the literature may have struggled to differentiate between Rho eye-movement and attention-based mechanisms in VSWM. One major problem has been the apparent lack of any experimental paradigm that can reliably decouple attentional processes from oculomotor control processes in VSWM. This arises because executing an eye-movement necessarily involves a participant also producing a comparable shift of covert attention (Shepherd, Findlay, & Hockey, 1986). Equally, we argue it is insufficient to investigate oculomotor involvement in VSWM by comparing conditions in which participants move their eyes to conditions where their gaze remains fixated (e.g., Godijn & Theeuwes, 2012), as participants may still engage in saccade preparation even without subsequent execution. An additional limitation of previous studies is that many studies have adopted a selective interference paradigm in which participants are required to produce eye-movements during the rehearsal period of a spatial working memory task (e.g., Guerard et al., 2009, Pearson and Sahraie, 2003 and Postle et al., 2006).

All of the post-1952 sedimentation rates were divided by the back

All of the post-1952 sedimentation rates were divided by the background rate for conversion to a dimensionless index of sedimentation relative to the early 20th century. We standardized the spatial datasets of catchment topography and land use into a consistent GIS database structure, organized by individual catchment, in terms of layer and attribute definitions. The Spicer (1999) and Schiefer et al. (2001a) data were converted from an older ARC/INFO format to a more recent Shapefile layer format that matched the Schiefer and Immell (2012) data. Layers that were available selleck inhibitor for all catchments included: catchment boundary, rivers, lakes, coring location,

a DEM, roads (temporal, i.e. containing an attribute for known or estimated year of construction), and cuts (temporal). The Foothills-Alberta Plateau catchments also included seismic cutline and hydrocarbon well (primarily for natural gas) layers of land use (temporal). We developed

Selleck Y27632 GIS scripts to extract a suite of consistent variables for representing catchment morphometry and land use history, including: region (categorical), catchment area (km2), mean catchment slope (%), road density (km/km2), cut density (km2/km2), cutline density (km/km2), and well density (number of wells/km2). All of the land use density variables were extracted for the full catchment areas, as well as for four different buffer distances from rivers and lakes (10 m, 50 m, 250 m, and 500 m) to quantify land use densities at different proximities to water

courses. To assess potential relations between sedimentation trends and climate change, we generated temperature and precipitation data for each study catchment. Wang et al. (2012) combined regression and spatial smoothing techniques to produce interpolated climate data for western North America from the Parameter-elevation Regressions on Independent Slopes Model (PRISM) gridded data (Daly et al., 2002). An associated application (ClimateWNA, version 4.70) produces down-scaled, annual climate data from 1901 to 2009, including mean monthly temperature and precipitation, suitable for the variable terrain Morin Hydrate of the Canadian cordillera. The climate data generated for our analyses included mean monthly temperature (°C) and total precipitation (mm) for times of the year that represent open-water conditions (i.e. generally lacking ice cover) (Apr–Oct) and closed-water conditions (Nov–Mar). This climate data was added to our longitudinal dataset by using the centroid coordinate for each catchment polygon as a PRISM interpolation point. Given the degree of spatial interpolation of the climate data, we do not attempt to resolve climatic gradients within individual catchments. The land use and climate variables were both resampled to the same 5-year interval used for the sedimentation data (Table 1).

Our results demonstrate that chronic alcohol feeding results in a

Our results demonstrate that chronic alcohol feeding results in a decrease in AMPK activity, which is recovered by RGE treatment. Previously, we reported that feeding mice with a Lieber–DeCarli diet containing 5% EtOH for 10 days, followed by a single dose of EtOH gavage (5 g/kg body weight) (chronic–binge EtOH model) induces significant fatty liver and liver injury

with oxidative stress (Fig. 6A) [25]. To investigate the effect of RGE for the treatment of BKM120 cost ALD using the chronic–binge EtOH model, EtOH-fed mice were treated with RGE. Treatment with RGE decreased EtOH-induced serum ALT and AST levels (Fig. 6B). The protective effect of RGE on alcoholic steatosis was further confirmed by liver histology as shown by H&E staining. It was noted that treatment of alcohol-fed mice with RGE completely inhibited fat infiltration (Fig. 6C), confirming Dactolisib manufacturer the ability of RGE to inhibit fat accumulation in liver. Moreover, the chronic–binge EtOH model significantly increased 4-HNE positive cells, which is consistent with our previous report [25]. However, similar to the chronic EtOH model, the amount of 4-HNE positive cells was dose-dependently and significantly reduced by treatment with RGE (Fig. 7A). RGE also markedly attenuated nitrotyrosine positive cells, confirming that RGE is capable of inhibiting alcohol-induced oxidative stress in the chronic–binge EtOH animal model (Fig. 7B). We next examined the effect of RGE on

fat accumulation in a mouse hepatocyte cell line, AML12. EtOH treatment for 3 days increased fat accumulation in hepatocytes as Carbohydrate shown by Oil red O staining. However, RGE (500 μg/mL or 1000 μg/mL) treatment reduced fat accumulation in a dose-dependent manner (Fig. 8A). To determine whether changes of fat accumulation in the hepatocyte were consistent with lipogenesis- or lipolytic-associated gene expression, the expression of SREBP-1, Sirt1, and PPARα was observed by Western blot analysis following concomitant treatment with 10–1000 μg/mL of RGE and EtOH for 3 days. In agreement with the in vivo data, RGE inhibited the ability of EtOH to induce SREBP-1 and repress Sirt1

and PPARα expression in AML12 cells ( Fig. 8B). The pharmacological properties of ginseng are primarily attributed to a group of active ingredients, the ginsenosides, which are a diverse group of steroidal saponins. Gum and Cho recently reported that total ginsenoside amount of RGE was 19.66 mg/g containing the major ginsenosides Rb1 (4.62 mg/g), Rb2 (1.83 mg/g), Rc (2.41 mg/g), Rd (0.89 mg/g), Re (0.93 mg/g), Rf (1.21 mg/g), Rg1 (0.71 mg/g), Rg2 (3.21 mg/g), Rg3 (3.05 mg/g), Rh1 (0.78 mg/g), and other minor ginsenosides [21]. Therefore, we next identified the major component of red ginseng required for the inhibition of hepatic steatosis. We determined the effects of the major ginsenosides Rb1, Rb2, and Rd on the EtOH-induced fat accumulation in AML12 cells.

We welcome contributions that elucidate deep history and those th

We welcome contributions that elucidate deep history and those that address contemporary processes; we especially invite manuscripts with potential to guide and inform humanity into the future. While Anthropocene emphasizes publication of research and review articles detailing human interactions

with Earth systems, the Journal also provides a forum for engaging global discourse on topics of relevance and interest to the interdisciplinary communities. We therefore seek short essays on topics that include policy and management issues, as well as cultural aspects of bio-physical phenomena. We also welcome communications that debate the merits and timing of the Anthropocene as a proposed geologic epoch. While we encourage these discussions, the Journal will remain neutral in its position with regards to the proposal to name a new epoch within the Geological Time Scale. The title of the journal, Anthropocene, is intended as a

AG-014699 mw broad metaphor to denote human interactions with Earth systems and does not imply endorsement for a new geologic epoch. We are pleased to highlight the first issue of Anthropocene comprising contributed and invited articles reporting studies from different parts of the world and different components of Earth’s systems. The editorial team is committed to producing a quality journal; we look forward to Selleck Ku-0059436 working together with the research communities to facilitate advancement of the science of the Anthropocene. “
“The nature, scale and chronology of alluvial sedimentation is one of the most obvious geological elements in the identification and demarcation of the Anthropocene (sensu Zalasiewicz et al. (2010)) – the proposed geological period during which humans have overwhelmed the ‘forces of nature’ ( Steffen et al., 2007). The geological record is largely composed of sedimentary rocks which reflect both global and regional Earth surface conditions. Although the geological record is dominated by marine Vasopressin Receptor sediments there are substantial intervals of the record where fluvial sediments are common (such as the Permo-Trias and much of the Carboniferous). The constitution of the rock record fundamentally reflects plate tectonics and global climate with the

two being inter-related through spatiotemporal changes in the distribution of land and oceans, astronomical forcing (Croll-Milankovitch cycles) and oceanic feedback loops. However, even marine sediments are the result of a combination of solutional and clastic input both of which are related to climate and Earth surface processes such as chemical weathering and erosion. Geomorphology is therefore an integral part of the rock-cycle and so fundamentally embedded within the Geological record both in the past and today ( Brown, 2008 and Brown et al., 2013). It is in this context that we must consider the role of humans both in the past and under the present increasingly human-driven global climate. Since pioneering work in North America after the dust-bowl of the 1930s by Happ et al.

LoVo, SNU-407, DLD-1, SNU-638, AGS, KPL-4, and SK-BR-3 cells were

LoVo, SNU-407, DLD-1, SNU-638, AGS, KPL-4, and SK-BR-3 cells were obtained from the Korean Cell Line

Bank (Seoul, Korea). LoVo, SNU-407, DLD-1, SNU-638, AGS, KPL-4, and SK-BR-3 cells were maintained in RPMI 1640 medium supplemented with 10% fetal bovine serum (Gibco, Grand Island, NY, USA) and an antibiotic cocktail (100 U/mL penicillin and 100 μg/mL streptomycin), and were subcultured by trypsinization every 3–4 days. Cells were grown at 37°C and 5% CO2 in humidified air. Two-dimensional gel electrophoresis (2-DE) analysis was performed as described previously [10]. A 0.15-mg protein sample was applied to 13-cm immobilized nonlinear gradient strips (pH 3–10), focused at 8,000 V within 3 hours, and separated on 10% polyacrylamide gels (Serva, Heidelberg, Germany; Bio-Rad). find more The 2-DE gels were stained with Colloidal Coomassie Blue (Invitrogen, Carlsbad, CA, USA) Capmatinib datasheet for 24 hours and then

destained with deionized water. Proteins showing abnormal expression were subjected to matrix-associated laser desorption/ionization–mass spectroscopy (MALDI-MS) analysis for identification. After preincubation of LoVo cells (1×106 cells/mL) for 18 hours, G-Rp1 (0–60μM) was added to the cell suspensions and incubated for 24 hours. The cytotoxic effect of G-Rp1 was then evaluated using a conventional MTT assay, as previously reported [11] and [12]. Three hours prior to culture termination, 10 mL MTT solution (10 mg/mL in phosphate-buffered saline, pH 7.4) was added, and the cells were continuously cultured until termination of the experiment. Incubation was halted by addition of 15% sodium dodecyl sulfate (SDS) into each well, solubilizing the formazan [13]. The absorbance at 570 nm (OD570–630) was measured using a Spectramax 250 microplate reader (BioTex, Bad Friedrichshall, Urease Germany). Flow-cytometric analysis for PI staining was performed as described previously [14] and [15]. LoVo (106) cells were washed with PBS, fixed in ethanol, suspended in PI solution (1 mg/mL

RNase A, 50 micro g/mL PI, and 0.1% Triton X-100 in 3.8mM sodium citrate) and incubated on ice for 30 minutes in the dark. After washing three times with fluorescence activated cell sorting (FACS) buffer, PI fluorescent intensity was analyzed on a FACScan (Becton Dickinson, Franklin Lakes, NJ, USA). LoVo cells incubated with G-Rp1 were harvested and suspended in 0.5 mL sample buffer consisting of 40mM Tris, 5M urea (Merck, Darmstadt, Germany), 2M thiourea (Sigma–Aldrich), 4% 3-[(3-cholamidopropyl)dimethylammonio]-1-propanesulfonate (Sigma–Aldrich), 10mM dithiothreitol (Merck), 1mM EDTA (Merck), and a mixture of protease inhibitors (Roche Diagnostics, Basel, Switzerland) for 45 minutes at room temperature.

This approach is consistent with advice from Australia’s premier

This approach is consistent with advice from Australia’s premier research organisation CSIRO (Commonwealth Scientific and Industrial Research Organisation) that state: “The SQG (Sediment Quality Guidelines) are trigger values that if exceeded are the prompt for further investigations to determine

whether there is indeed an environmental risk associated with the exceedance” ( Simpson et al., 2005, p. 2). The assessment was limited to the <2 mm sediment fraction for the additional following reasons: (i) The floodplain sediments were comprised of fine-grained alluvium, with no significant or discernible difference in grain size. (ii) Assessment of the potential risk to the cattle is based on exposure. Given that the livestock are check details exposed to the bulk sediment and not a specific size fraction, size-partitioning would not assist in determining if floodplain alluvium or channel deposits were a potential source of contamination. Sampling the bulk fraction is also consistent with the

potential for sand-sized materials in mine-contaminated waste materials to contain trace metals ( Moore et al., 1989). The National Measurement Institute (NMI) in Pymble, NSW analysed Dabrafenib nmr the samples for total extractable metals using an aqua regia digest (HNO3 + HCl) at 100 °C for 2 h (Supplementary Material S1). Following dilution, a Perkin Elmer Elan DRC II, Inductively Coupled Plasma-Mass Spectrometer, and Varian Vista Pro, Inductively Coupled Plasma-Atomic Emission Spectrometry analysed aliquots for Al, Sb, As, Cr, Co, Cu, Pb and Ni. Four field samples were split and analysed to provide Anidulafungin (LY303366) a measure of analytical repeatability. These samples returned relative percent deviations (RPD) for all elements of <30% except for Cu with two samples (RPD of 40% and 57.9%; Supplementary Material S2). Adopting a site-specific approach, these elevations can be attributed to the naturally heterogeneous nature of surface sediments at the sample sites and/or limitations with

the field splitting method utilised. The sample site rendering the highest RPD generally displayed higher RPDs in other metals compared to other duplicate sites. Therefore, either the heterogeneous surface sediments at this particular site or the splitting method utilised has probably led to these elevated RPDs. Data have been evaluated bearing in mind this limitation, with a focus on the broader results and spatial patterns returned for the creek systems. Laboratory blanks, duplicates, matrix spikes and certified reference materials were also used to ensure accuracy. Blanks were all under the limit of reporting (LOR). Matrix spike rates, which measure recovery rates, were 82–101%. The analytical recovery of sample metal concentrations was determined using certified reference material AGAL-10 (river sediment) and AGAL-12 (biosoil), which returned between 85 and 114% of the listed values for the elements of interest (Al, Sb, As, Cr, Co, Cu, Pb and Ni).

In the case of Polynesia, the Caribbean, and the Channel Islands,

In the case of Polynesia, the Caribbean, and the Channel Islands, human transformation of island ecosystems began at initial colonization and often accelerated

through time as populations grew and human activities intensified. The maritime agriculturalists that occupied Polynesia and the Caribbean often had a similar pattern of occupation with early records documenting significant anthropogenic burning and landscape clearance, a new suite of intentionally and accidentally introduced plants and animals that were part of transported landscapes, followed by soil erosion and later highly Ruxolitinib managed anthropogenic landscapes. The pattern identified in these two island regions is similar to the records of islands in the North Atlantic occupied by Neolithic and Viking Age peoples (McGovern et al., 2007 and Perdikaris and McGovern, 2008) and Mediterranean islands (Patton, 1996; Zeder, 2009). Island archeology also reveals important differences in the scale and magnitude

of human environmental impacts. On the Channel Islands and some Caribbean islands, initial human occupations were by maritime hunter-gatherers. The environmental impacts of these early peoples check details is often not as rapid, easy to discern, or as clear as those of pastoralists or agriculturalists. Without domesticated plants and animals (except dogs) or the need to clear land for horticulture, for example, early records of human occupation from California’s Channel Islands generally lack the initial burning, landscape clearing, and soil erosion typical of many Polynesian sequences. Anthropogenic burning is evident on the Channel Islands in the past, but these events are not easy to differentiate from natural fires (Anderson et al., 2010b). Still hunter-gatherers transformed their island ecosystems in major ways, including the translocation of animals, direct and indirect influences on the extinction of mammals and birds, fire and burning, and significant impacts on marine resources. On the Channel Islands, these include translocation of island deer mice, island foxes, and perhaps other organisms

(Rick, 2013), and strong influences on island marine ecosystems and organisms (Erlandson and Rick, 2010). The early record of some Caribbean islands also documents extinction of island sloths and other vertebrates, and translocation of plant resources by hunter-gatherer SPTLC1 populations (Newsom and Wing, 2004:128; Steadman et al., 2005). These data suggest that there was no single, overarching human influence or impact on island ecosystems in the past—the patterns and processes on islands were complex and related to the subsistence strategies of people occupying the island (i.e., agriculturalists, hunter-gatherers), the population densities of those people, their sociocultural systems and technologies, differences in island physical characteristics (size, age, nutrients, etc.), and the collective decisions made by individual societies.

The third and fourth cells did not fire in block 1 and formed dis

The third and fourth cells did not fire in block 1 and formed distinct timing patterns in block PLX4032 ic50 2. Finally, the fifth cell was active both early and late in the delay in block 1, and its response to lengthening the delay was to maintain both times, one relative to beginning and the other relative to the end of the delay. Note that retiming typically did not occur immediately when the delay was increased. Comparisons of firing rates within the “time-fields”

across trials after the delay was increased showed that retiming did not happen immediately but occurred after a variable number of trials, either suddenly or gradually, in different cells (Figure S4). Neurons that showed absolute and relative timing, as well as retiming, were observed in simultaneously recorded ensembles, ranging 29%–54% for absolute and relative timing versus 45%–71% for retiming, suggesting that each neuron coded moments in the delay independently of the others. In addition, two

rats were returned to their standard delay during block 3, allowing us to assess whether neurons that retimed returned to the pattern of activity that was observed when the standard delay was reintroduced. selleck inhibitor The cross-correlation analysis indicated that most neurons (90%, 46/51) that retimed in block 2 maintained the altered pattern through block 3, similar to the hysteresis reported for partial remapping of place cells (Leutgeb et al., 2005a). The remaining five neurons appeared to return to a firing pattern in block 3 that resembled that in block 1. Examples of both types

of responses in block 3 are presented Cepharanthine in Figure 6B. One possible explanation for retiming is that the performance of the rat deteriorated when the delay was lengthened. For two rats, changing the delay had no apparent effect on performance, and this was confirmed by comparing performances in each block (two-sample t tests, all p values >0.17). A third rat did show a transient decrease in performance from block 1 to the first third of block 2 trials (two-sample t test; t58 = 3.25; p = 0.002). However, its performance recovered during the last two-thirds of block 2 (two-sample t test; t71 = 2.07; p = 0.04) and was otherwise stable throughout the recording session (for all remaining comparisons: two-sample t tests, all p values >0.18). Note also that, whereas performance for all rats was equally strong in blocks 1 and 3, when the lengths of the delays were equal, retiming that occurred in block 2 often persisted into block 3. Thus, retiming appears unrelated to changes in task performance. It is also possible that retiming might be secondary to changes in the locations the rat occupied during sequential time segments when the delay was lengthened. To address this possibility we compared second-to-second spatial firing rate maps for the early part of the delay across all trial blocks.

Because O2 and CO2 fluctuations occur in different environments (

Because O2 and CO2 fluctuations occur in different environments (mountain tops, under the sea, in the ground) at different times (diurnal rhythms, seasonal variation), as well as under different conditions (respiration, photosynthesis), it is remarkable that animals can glean useful information by monitoring external concentrations. The ability to interpret these signals in the context of a variety of other sensory cues is essential to determine whether the appropriate

behavior is attraction, avoidance, or indifference. How animals evaluate O2, CO2, and other environmental cues is an important problem in neural integration and an exciting avenue of investigation. The author thanks Dr. Henk Roelink for generating the figures for this review and Dr. John Ngai for careful reading of the manuscript. This work was in part supported by a grant from the Z-VAD-FMK mw National Institute of Deafness and Communication Disorders 1R01DC006252 (KS). K.S. is an Early Career

Scientist of the Howard Hughes Medical Institute. “
“Effective therapy for Alzheimer’s disease (AD) is a major unmet medical need. The major demographic risk for development of AD is age with risk doubling approximately every 5 years after age 65 such that by the age of 85, one’s chances of having dementia due to AD ranges from 25%–40%. Therefore, the prevalence of AD is expected to double every 20 years, largely because Enzalutamide mouse of an anticipated increase in the average expected life span. Based on estimates that ∼35 million people worldwide have AD today, it is predicted that well over 100 million individuals will have AD in 2050 (Alzheimer’s Association, 2010 and Wimo et al., 2010). If nothing is done, the personal, economic, and societal toll of the ongoing and growing AD epidemic will be immense. Although key aspects of AD pathogenesis remain enigmatic, scientific advances over the

last 25 years have provided sound rationale for the development of potentially disease-modifying AD therapies (Golde, 2005 and Selkoe, 2001). These therapies primarily target the suspected trigger(s) of the disease. Therapies that have advanced the farthest have primarily been developed based on the proposed initiating role of amyloid β-protein (Aβ) aggregates (Golde et al., 2010). These therapeutic advances, coupled Quisqualic acid with advances in early detection of AD-related pathology in nondemented individuals, suggest that concerted translational research efforts focusing on prevention or early intervention could dramatically reduce the incidence and prevalence of AD. However, current trial design involves treatment of symptomatic patients, a setting where failure to show efficacy may be even more likely given the disease progression. Misalignments of the rationale for the therapy, its preclinical testing, and the actual testing of the therapy in human AD clinical trials have resulted in barriers to effective drug development that we must recognize and that will be very challenging to solve.

The observed response properties of V3A are compatible with singl

The observed response properties of V3A are compatible with single-unit responses to “real motion” described previously for the macaque (Galletti et al., 1990), as well as with gaze-modulated responses in about half of V3A’s neurons that encode spatial locations in a head-centered frame of reference (Galletti and Battaglini, 1989 and Nakamura and Colby, 2002). Interestingly, macaque V3A contains relatively few motion-responsive neurons in comparison to macaque areas V5/MT, MST, and VIP (Orban et al., 2003 and Tootell et al., 1997). Consequently, neural response properties, but also multimodal integration of visual motion signals with nonvisual signals, such as pursuit-related or vestibular input, have

been studied far more extensively in regions other than V3A, both in humans and macaques (Goossens et al., 2006, Gu et al., 2008, Ilg et al., 2004 and Zhang et al., 2004). However,

in contrast Galunisertib molecular weight to macaque physiology and macaque fMRI signals, human imaging has revealed a strong involvement of V3A in motion processing, comparable to that of human V5/MT and MST (Bartels et al., 2008b, McKeefry et al., 2008, Orban et al., 2003, Tootell et al., 1997 and Wall and Smith, 2008). This points to a functional difference INCB024360 between macaque and human V3A with respect to motion processing (Orban et al., 2003). The present study emphasizes that further by demonstrating motion responses entirely driven by objective, but not retinal, motion in human V3A. V3A has strong connections with areas V6 and V6A and has been associated with pathways serving visual control of grasping rather than control of pursuit and estimation of self-motion found in MST (Galletti et al., 2003 and Nakamura et al., 2001). For grasping and associated object vision, head- or body-centered representations would be crucial for successful execution. In contrast, visual control of pursuit would require cAMP both, retinal as well as head-centered representations, such as found

in the V5+/MT+ complex (Chukoskie and Movshon, 2009 and Ilg et al., 2004). The observed presence of both retinal as well as head-centered responses in V5/MT and MST and the preference for retinal responses in V5/MT agree with the distribution of units in both areas responsive to motion in the two reference frames (Arnoldussen et al., 2011, Chukoskie and Movshon, 2009 and Ilg et al., 2004). Similarly, task-dependent spatiotopic responses found in human V5/MT and MST (that take fixed eye position into account) are compatible with the present results (Crespi et al., 2011 and d’Avossa et al., 2007). Human V6 has been shown to respond to large-field motion (Pitzalis et al., 2006 and Pitzalis et al., 2010), to have the highest response bias among motion-responsive regions toward stimuli simulating egomotion in depth (expansion flow) (Cardin and Smith, 2010), and to achieve the highest integration between stereo-depth with 3D motion flow among flow-responsive regions (Cardin and Smith, 2011).