Conscious Brain-to-Brain Communication in Humans Using Non-Invasive Technologies

Human sensory and motor systems provide the natural means for the exchange of information between individuals, and, hence, the basis for human civilization. The recent development of brain-computer interfaces (BCI) has provided an important element for the creation of brain-to-brain communication systems, and precise brain stimulation techniques are now available for the realization of non-invasive computer-brain interfaces (CBI). These technologies, BCI and CBI, can be combined to realize the vision of non-invasive, computer-mediated brain-to-brain (B2B) communication between subjects (hyperinteraction). Here we demonstrate the conscious transmission of information between human brains through the intact scalp and without intervention of motor or peripheral sensory systems. Pseudo-random binary streams encoding words were transmitted between the minds of emitter and receiver subjects separated by great distances, representing the realization of the first human brain-to-brain interface. In a series of experiments, we established internet-mediated B2B communication by combining a BCI based on voluntary motor imagery-controlled electroencephalographic (EEG) changes with a CBI inducing the conscious perception of phosphenes (light flashes) through neuronavigated, robotized transcranial magnetic stimulation (TMS), with special care taken to block sensory (tactile, visual or auditory) cues. Our results provide a critical proof-of-principle demonstration for the development of conscious B2B communication technologies. More fully developed, related implementations will open new research venues in cognitive, social and clinical neuroscience and the scientific study of consciousness. We envision that hyperinteraction technologies will eventually have a profound impact on the social structure of our civilization and raise important ethical issues.     

Hormone directed sucrose transport during fruit set induced by gibberellins in Pisum sativum

A new system has been developed to study hormone-directed transport in intact plants during parthenocarpic fruit set induced by gibberellins. Gibberellic acid (GA₃) and gibberellin A₁ (GA₁) applied to unpollinated ovaries of pea ( Pisum sativum L. cv. Alaska) promoted sucrose transport from the leaf to the site of hormone application. In vivo experiments showed an early (30 min) accumulation of [¹⁴C]-sucrose in ovaries of pea stimulated by gibberellins. This activation of sucrose transport appears to be mediated by gibberellins (GA₁, GA₃), increasing both loading of phloem with sucrose in the leaf (source) and sucrose unloading in the ovary (sink). The ability of pea tissue segments to take up sucrose in vitro was not affected by the hormonal treatment.     

The Pleistocene lake deposits of the NE Baza Basin (Spain): salinity variations and ostracod succession

The Guadix-Baza Basin in Spain covers an area of approximately 3000 km² and yields a sedimentary sequence ranging from Lower Miocene to Pleistocene. Twenty five meters of Lower Pleistocene lacustrine sediments have been located in the NE part of the Basin at about 1000 meters in altitude. This sequence which overlies dolomitic mud flat deposits consists of limestones, calcareous and dolomitic mudstones, dolostones, silty clays, sands and gravels. Salinity fluctuations and short dry episodes, related to lake level oscillations, have been recorded by textural, mineralogical and faunal changes throughout the sequence. Ostracods, which are the most commonly encountered fossils, permit to detect recurrent changes in water salinity and regime, and solute composition. The faunal changes indicate an alternation of slightly saline and bicarbonate-rich water (when ostracods and gastropods occur) with a saline NaCl-dominant water (in which ostracods, Cerastoderma bivalves and non-marine foraminifers are found).The frequent and recurrent hydrochemical changes in the Baza Basin in the Early Pleistocene point to a climate of high contrast like in the Mediterranean region today but with a greater availability of water within the system compared to the present situation in the area.     

Proton NMR studies of [N-MeCys3,N-MeCys7]TANDEM binding to DNA oligonucleotides: sequence-specific binding at the TpA site.

[N-MeCys3,N-MeCys7]TANDEM, an undermethylated analogue of Triostin A, contains two N-methyl groups on the cysteine residues only. Footprinting results showed that [N-MeCys3,N-MeCys7]TANDEM binds strongly to DNA rich in A.T residues [Low, C. M. L., Fox, K. R., Olsen, R. K., & Waring, M. J. (1986) Nucleic Acids Res. 14, 2015-2033]. However, it was not known whether specific binding of [N-MeCys3,N-MeCys7]TANDEM requires a TpA step or an ApT step. In 1:1 saturated complexes with the octamers [d(GGATATCC)]2 and [d(GGTTAACC)]2, [N-MeCys3,N-MeCys7]TANDEM binds to each octamer as a bis-intercalator bracketing the TpA step. The octadepsipeptide ring binds in the minor groove of the DNA. Analysis of sugar coupling constants from the phase-sensitive COSY data indicates that the sugar of the thymine in the TpA binding site adopts predominantly an N-type sugar conformation, while the remaining sugars on the DNA adopt an S-type conformation, as has been observed in other Triostin A and echinomycin complexes. The drug does not bind to the octamer [d(GGAATTCC)]2 as a bis-intercalator. Only weak nonintercalative binding is observed to this DNA octamer. These results show unambiguously that [N-MeCys3,N-MeCys7]TANDEM binds sequence specifically at TpA sites in DNA. The factors underlying the sequence specificity of [N-MeCys3,N-MeCys7]TANDEM binding to DNA are discussed.     

Genome-wide RAD sequencing data suggest predominant role of vicariance in Sino-Japanese disjunction of the monotypic genus Conandron (Gesneriaceae)

Disjunct distribution is a key issue in biogeography and ecology, but it is often difficult to determine the relative roles of dispersal vs. vicariance in disjunctions. We studied the phylogeographic pattern of the monotypic Conandron ramondioides (Gesneriaceae), which shows Sino-Japanese disjunctions, with ddRAD sequencing based on a comprehensive sampling of 11 populations from mainland China, Taiwan Island, and Japan. We found a very high degree of genetic differentiation among these three regions, with very limited gene flow and a clear Isolation by Distance pattern. Mainland China and Japan clades diverged first from a widespread ancestral population in the middle Miocene, followed by a later divergence between mainland China and Taiwan Island clades in the early Pliocene. Three current groups have survived in various glacial refugia during the Last Glacial Maximum, and experienced contraction and/or bottlenecks since their divergence during Quaternary glacial cycles, with strong niche divergence between mainland China + Japan and Taiwan Island ranges. Thus, we verified a predominant role of vicariance in the current disjunction of the monotypic genus Conandron. The sharp phylogenetic separation, ecological niche divergence among these three groups, and the great number of private alleles in all populations sampled indicated a considerable time of independent evolution, and suggests the need for a taxonomic survey to detect potentially overlooked taxa.     

Expression, Purification, and Initial Characterization of the Recombinant Storage Protein Precursor ofTheobroma cacao

The gene encoding the 67-kDa cocoa storage protein precursor has been cloned fromTheobroma cacaoand expressed inEscherichia coliusing the pET expression system. The recombinant storage protein has been renatured from inclusion bodies at 30°C using 20 m glycine–NaOH buffer, pH 10.0, containing 1 m oxidized glutathione and 0.1% Brij. The renatured protein was purified and demonstrated to adopt a stable native conformation by optical spectroscopy. Secondary structure analysis from circular dichroism indicated the protein to be 23% α-helix and 38% β-sheet, in close agreement with values obtained using a secondary structure prediction program.     

The DNA sequence at echinomycin binding sites determines the structural changes induced by drug binding: NMR studies of echinomycin binding to [d(ACGTACGT)]2 and [d(TCGATCGA)]2

The complexes formed between the cyclic octadepsipeptide antibiotic echinomycin and the two DNA octamers [d(ACGTACGT)]2 and [d(TCGATCGA)]2 have been investigated by using one- and two-dimensional proton NMR spectroscopy techniques. The results obtained for the two complexes are compared to each other, to the crystal structures of related DNA-echinomycin complexes, and to enzymatic and chemical footprinting results. In the saturated complexes, two echinomycin molecules bind to each octamer by bisintercalation of the quinoxaline moieties on either side of each CpG step. Binding of echinomycin to the octamer [d(ACGTACGT)]2 is cooperative so that only the two-drug complex is observed at lower drug-DNA ratios, but binding to [d(TCGATCGA)]2 is not cooperative. At low temperatures, both the internal and terminal A.T base pairs adjacent to the binding site in the [d(ACGTACGT)]2-2 echinomycin complex are Hoogsteen base paired (Gilbert et al., 1989) as observed in related crystal structures. However, as the temperature is raised, the internal A.T Hoogsteen base pairs are destabilized and are observed to be exchanging between the Hoogsteen base-paired and an open (or Watson-Crick base-paired) state. In contrast, in the [d(TCGATCGA)]2-2 echinomycin complex, no A.T Hoogsteen base pairs are observed, the internal A.T base pairs appear to be stabilized by drug binding, and the structure of the complex does not change significantly from 0 to 45 degrees C. Thus, the structure and stability of the DNA in echinomycin-DNA complexes depends on the sequence at and adjacent to the binding site. While we conclude that no single structural change in the DNA can explain all of the footprinting results, unwinding of the DNA helix in the drug-DNA complexes appears to be an important factor while Hoogsteen base pair formation does not.     

Hydrogeochemistry of Lake Gallocanta (Aragón,NE Spain)

Lake Gallocanta has undergone drastic changes during the last thirteen years. Water level changed from a high level (Z_max = 2 m) to total dryness in 1985. From 1986 to 1988 slow refilling occurred. The water volume fluctuations have been studied in relation to climatic variations recorded for that period. Variations in the major dissolved ions were related to water volume fluctuations from data at two different stages, one corresponding to the drying phase and another to the refilling phase. Mineralogical composition of the salts precipitated at different stages was examined by X-ray diffraction. Interstitial water and mineralogical composition of recent sediments were also studied along a transect through the lake.The water column decrease from 1977 to 1985 is related to decreasing annual rainfall (500-250 mm respectively). The refilling in 1986–1988 is due to high annual rainfall (537 mm). In addition to these fluctuations, seasonal changes of the water level between 20 and 50 cm occurred every year.Gallocanta is a Na-Mg-Cl-(SO₄) type lake. During the drying period a typical salt enrichment occurs with linear relationships between TDS, Cl, Na and K. Alkalinity is linearly correlated with Ca at relatively low salinities. As salinity increases a linear relationship between Ca and SO₄ is observed. Minerals formed from the brine are halite, bischofite, epsomite, hexahydrite, mirabilite, gypsum, aragonite, calcite and dolomite. The molar ratio Mg/Ca of the interstitial water changes from 1.5 along the shorelines, where calcite and aragonite precipitate, to 40 in the center of the lake. Sediment cores from the central part of the lake show aragonite in the top layers, magnesian calcite and low proportions of quartz and illite, while at 20 cm depth a high proportion of gypsum is present. In contrast, cores from the shore of the lake are mainly composed of low magnesium calcite in the top layers and low magnesium calcite together high magnesium calcite and dolomite between 30 and 70 cm depth. Gypsum deposits only occur in significant proportions at 80–100 cm depth.The refilling process showed relationships between volume and salt concentration following the Langbein model. The salt mass in solution decreased about 50% from the drying to the refilling phase. However, Mg content decreased about 70 % for the same period, suggesting a contribution of this element to the dolomite formation.