User talk:Kero

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Hello, Kero, and welcome to Wikipedia! Thank you for your contributions, especially what you did for User talk:Waithamai. I hope you like the place and decide to stay. Here are some pages that you might find helpful: I hope you enjoy editing here and being a Wikipedian! Please sign your messages on discussion pages using four tildes ( ~ ); this will automatically insert your username and the date. If you need help, check out Questions, ask me on my talk page, or ask your question on this page and then place  before the question. Again, welcome! Wai tha Mai 16:40, 18 October 2011 (UTC)
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Hi Kero, this "kerolite (which is also discredited)", in 2nd line of Pimelite, IMHO borders to personal attack. What are we going to do about it? By the way, if you are versed in Polish, you might try to get a permission for this image, in order to have more proof for your existence. --Túrelio (talk) 08:05, 1 April 2012 (UTC)
 * Looool, sehr geil. Habe die Mail komischerweise erst jetzt bekommen und kurz Panik vor der Lolcat bekommen :D:D:D --Kero (talk) 09:08, 4 April 2012 (UTC)
 * No, Kero, this is not a personal attack, it is a verifiable scientific truth. The vein mineralogy in ultrabasic rocks changes gradually from discredited kerolith to discredited pimelith. Veins of Kerolith penetrating only almost fresh or juvenile rocks. In daylight Kerolithe aging very quickly and lose their original beauty. This is very sad, but not to change. Sry, Kero. Everyting is going to be alright. Greetings from Nina — Preceding unsigned comment added by 178.1.236.115 (talk) 10:27, 4 April 2012 (UTC)
 * Hi Nina, everything is fine, we are just kidding ;). Best regards --Kero (talk) 10:40, 4 April 2012 (UTC)

Hero Kero.... Congratulations, big hero of Aachen;). Everything will be fine ... Nina. — Preceding unsigned comment added by 178.1.236.115 (talk) 22:00, 17 April 2012 (UTC)