http://www.nytimes.com/2000/05/09/science/q-a-yellow-tomatoes.html Both colors have vitamin C, though a red tomato has about three times as much. Minerals are similar, though a yellow tomato is higher in sodium. Yellow tomatoes have more niacin and folate; red tomatoes have more vitamin B6 and pantothenic acid, and so on.
http://www.pnas.org/content/35/6/284.full.pdf Lycopene formation is particularly sensitive to temperature.Thus, the fact that some twenty pure lines of yellow tomatoes studied here (differing greatly in pigment con- tent and inother respects) invariably contained small quantities of lyco- pene, does not invalidate the
Lycopene-rich tomatoes linked to lower stroke risk http://www.health.harvard.edu/blog/lycopene-rich-tomatoes-linked-to-lower-stroke-risk-201210105400 Lycopene is a carotenoid?a family of pigments that give fruits and vegetables their brilliant red, orange, and yellow coloring. Lycopene is also a powerful antioxidant that eliminates dangerous free radicals that can damage DNA and other fragile cell structures
Lycopene in tomatoes: chemical and physical properties affected by food processing. http://www.ncbi.nlm.nih.gov/pubmed/11192026 Although it has no provitamin A activity, lycopene does exhibit a physical quenching rate constant with singlet oxygen almost twice as high as that of beta-carotene.
Eggplant-LXM 2002 The map is based on 58 F2 plants from an interspecific cross between S. linnaeanum (MM195) and S. melongena (MM738) Eggplant-COSII This map is based on 58 F2 individuals from an interspecific cross between S. linnaeanum Hepper & Jaeger MM195 and S. melongena L. MM738, which was produced by Dr. M. C. Daunay at the Institut National de la Recherche Agronomique, France. A map of 232 tomato-derived markers based on the same population was reported in SGN (Eggplant-LXM 2002). However, the current map has an additional set of 110 COSII markers and 5 tomato-derived markers Tomato EXPEN 2000 This map is based on 80 F2 individuals from the cross L. esculentum LA925 x L. pennellii LA716. Potato-TXB 1992 This is a map based on a S. tuberosum x S. berthaultii BC S. tuberosum population reported in Tanksley et al (1992).
http://www.guardian.co.uk/film/video/2013/may/09/village-at-the-end-of-the-world-video-review Village At The End Of The World Production year: 2012 In this excerpt from the Guardian Film Show, Xan Brooks, Peter Bradshaw and Andrew Pulver review Village at the End of the World, a documentary by Sarah Gavron. Niaqornat in Greenland has a population of 59 and one source of employment: the local fish factory. When it seems the factory might be shut down permanently, the community must rally round to try to take it over Length: 4min 47sec 最後の歌と犬は必見
http://www.guardian.co.uk/environment/video/2012/sep/24/ice-melt-life-greenlanders-video How record sea ice melt is changing life for Greenlanders ? video Sea ice in the Arctic has shrunk to its smallest extent ever recorded, smashing the previous record minimum and prompting warnings of accelerated climate change. Klaus Thyman from Project Pressure speaks to two Greenlanders about how the extreme shift is impacting on their everyday lives
A mid-Holocene shift in Arctic sea-ice variability on the East Greenland Shelf. The Holocene January 2002 vol. 12 no. 1 49-58 http://hol.sagepub.com/content/12/1/49.short Records of iceberg-rafting and palaeohydrography from two East Greenland shelf cores (JM96-1206/1-GC and JM96-1207/1-GC) are reported. Benthic foraminifera, stable isotopes and IRD fluxes indicate a shift toward colder, lower-salinity ‘polar’ conditions c. 5 cal. ka. A new proxy of iceberg-rafting on the East Greenland Shelf is the flux of calcium carbonate (TIC) thought to be derived from glacial erosion of Cretaceous calcareous mudstones. A change in the regularity and spacing of carbonate flux peaks at c. 4.7 cal. ka in JM96-1207 coincides with the onset of Neoglacial cooling in the Renland ice core δ18O record. We propose that the carbonate flux peaks between 4.7 and 0.4 cal. ka are related to sea-surface coolings associated with increased flux of polar water and sea ice in the East Greenland Current. These peaks are synchronous with sea-surface coolings interpreted from North Atlantic deep-sea cores, but additional peaks centred around 2.4 and 3.8 cal. ka in JM96-1207 suggest that the shelf site captures higher-frequency events. The data indicate that severe Arctic sea-ice events began in the Neoglacial interval, and that earlier-Holocene cool events in deep-sea records are associated with other processes, such as release of meltwater from residual glacier ice and glacial lakes.
Reconstruction of the late-Holocene changes in the Sub-Arctic Front position at the Reykjanes Ridge, north Atlantic. The Holocene August 2012 vol. 22 no. 8 877-886 http://hol.sagepub.com/content/22/8/877.abstract
Climate-driven fluctuations in freshwater flux to Sermilik Fjord, East Greenland, during the last 4000 years. The Holocene February 2012 vol. 22 no. 2 155-164 http://hol.sagepub.com/content/22/2/155.abstract
ジルコン化合物は水とある種の化学反応を起こすときに同位体分別が起こることが知られており オーストラリア西部で見つかったジルコン粒子は約44億年前に水の関与した反応があったことを示している 地球の歴史のごく初期の時代から、少なくとも一部では海があったことを これ↓ Oxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4,300 Myr ago. Nature. 2001 Jan 11;409(6817):178-81. http://isotope.colorado.edu/~mojzsis/2001_Mojzsis_Nature.pdf Granitoid gneisses and supracrustal rocks that are 3,800-4,000 Myr old are the oldest recognized exposures of continental crust. To obtain insight into conditions at the Earth's surface more than 4 Gyr ago requires the analysis of yet older rocks or their mineral remnants. Such an opportunity is presented by detrital zircons more than 4 Gyr old found within 3-Gyr-old quartzitic rocks in the Murchison District of Western Australia. Here we report in situ U-Pb and oxygen isotope results for such zircons that place constraints on the age and composition of their sources and may therefore provide information about the nature of the Earth's early surface. We find that 3,910-4,280 Myr old zircons have oxygen isotope (delta18O) values ranging from 5.4+/-0.6% to 15.0+/-0.4%. On the basis of these results, we postulate that the approximately 4,300-Myr-old zircons formed from magmas containing a significant component of re-worked continental crust that formed in the presence of water near the Earth's surface. These data are therefore consistent with the presence of a hydrosphere interacting with the crust by 4,300 Myr ago.
アクアマリン福島より MORPHOLOGICAL COMPARISON OF THE INDONESIAN COELACANTH, Latimeria menadoensis AND AFRICAN COELACANTH, Latimeria chalumnae The Coelacanth, Fathom the Mystery 2007 http://www.marine.fks.ed.jp/images/coela/sympo/p1-2.pdf