\documentclass[11pt,a4paper]{article}
\usepackage[latin1]{inputenc}
\usepackage[english]{babel}
\usepackage{textcomp}
\usepackage{amsmath}
\usepackage{amssymb}
\usepackage{graphicx}
\usepackage{textcomp}
\usepackage{color}               % farbe
\usepackage{wrapfig}
\usepackage{listings} % listing
\usepackage{attachfile} % files anhängen
\usepackage[hdivide={*,15cm,*}, vdivide={*,22.7cm,*}, marginparsep=0.5cm, marginparwidth=1.5cm, twoside]{geometry} % 

\newcommand{\abs}[1]{\lvert#1\rvert}
\newcommand{\titelname}{Maya and Climate\\{\small Climate and the Collapse of Maya Civilization}}

%\attachfilesetup{icon=Paperclip, color=1 0 0, author=Thomas Kuster, description=Quellcode, subject=Quellcode, mimetype=text/plain}

%\usepackage[pdftex]{hyperref,graphicx,color} % pdflinks
%\pdfoutput=1

\hypersetup
{%
pdftitle = {\titelname},%
pdfsubject = {Maya and Climate; Climate and the Collapse of Maya Civilization},%
pdfauthor = {Peter Barmet, Thomas Kuster, André Welti (MSc, D-UWIS)},%
pdfkeywords = {Presentation, Übung},%
colorlinks = {true},%
linkcolor = {blue}
}

\setlength{\parindent}{0pt} %kein einzug links nach einem abschnitt

\date{Climate History and Paleoclimatology, 24.11.2006}
\author{Peter Barmet, Thomas Kuster, André Welti\\ {\small \hyperref{http://fam-kuster.ch/index.php?navigation=ETH&main=http://n.ethz.ch/student/kusterth/eth/html/}{}{}{http://fam-kuster.ch $\rightarrow$ ETH $\rightarrow$ 7. Semester $\rightarrow$ climate\dots}}}
\title{\titelname}

\begin{document}
\markright{\titelname}
\pagestyle{myheadings}
\maketitle

\section{Maya}
\subsection{Periods}
\begin{itemize}
 \item Preclassic: 2000\,BC\footnote{Before Christ} -- 250\,AD\footnote{Anno Domini, latin for "in the year of the lord"}
 \item Classic: 250 -- 900\,AD
 \item Postclassic Period: 900 -- 1511\,AD
\end{itemize}

\subsection{Collapse}
Between classic an postclassic period, in 3 phases
\begin{itemize}
 \item 760 to 810\,AD
 \item to 860\,AD
 \item to 910\,AD
\end{itemize}
 
\section{Climate}
In the inter tropic conversion (ITC)

\section{Geology\,/\,Hydrology}
The Yucatán Peninsula consists of limestones rocks and mountains $\rightarrow$ caves (as in the jura mountains)

% \begin{wrapfigure}{r}{0.35\linewidth}
%  \includegraphics[page=4, viewport=215 20 570 480, clip, width=0.5\linewidth]{./password/peterson2005}
%  \caption{Titanium content in sediments from the cariaco basin}
%  \label{abb:ti}
% \end{wrapfigure}
%\begin{minipage}[t]{0.6\linewidth}
\section{Methods}
\begin{itemize}
 \item gypsum (CaSO$_4$) deposition in lake chichancanab (fallout of CaSO$_4$ if saturation is reached)
 \item oxygen isotops ($\delta^{18}$O) in sediments from lake chichancanab (enrichment of $^{18}$O during droughts, because $^{16}$O evaporates easier)
 \item titanium content in sediments from the cariaco basin (less titanium $\rightarrow$ less precipitation)%, see figure~\ref{abb:ti}
\end{itemize}
%\end{minipage}

\section{Results}
\begin{tabular}{rcrl}
5500\,BC & -- &  500\,BC & \textcolor{blue}{relative wet}\\
 475\,BC & -- &  250\,BC & \textcolor{red}{drought period} (before the rise of Maya civiliation)\\
 250\,BC & -- &  150\,BC & \textcolor{blue}{wet}\\
 150\,BC & -- &  250\,AD & \textcolor{red}{drier period}\\
 250\,AD & -- &  600\,AD & \textcolor{blue}{good climate conditions}\\
 600\,AD &    &          & begin of a long dry period\\
 760\,AD & -- &  850\,AD & \textcolor{red}{begin of the TCD\footnotemark}, worst drought since the last 7\,000 years\\
 800\,AD &    &          & \textcolor{red}{zenith of the drought} and collapse of the civilization\\
 910\,AD & -- &  990\,AD & second \textcolor{red}{drought period}\\
1060\,AD & -- & 1100\,AD & third \textcolor{red}{drought period}
\end{tabular}
\footnotetext{Terminal Classic Drought}

\begin{thebibliography}{10}
  \bibitem[Haug, 2003]{haug2003}
    G.~H.~Haug et.\,al.
    \newblock Climate and the Collapse of Maya Civilization.
    \newblock {\em Science}, 299:1731--1735, 2003.
      
  \bibitem[Hodell, 2005]{hodell2005}
    D.~A.~Hodell et.\,al.
    \newblock Terminal Classic drought in the northern Maya lowlands inferred from multiple sediment cores in Lake Chichancanab (Mexico).
    \newblock {\em Quanternary Science Reviews}, 24:1413--1427, 2005.

  \bibitem[Hodell, 2001]{hodell2001}
    D.~A.~Hodell et.\,al.
    \newblock Solar Forcing of Drought Frequency in the Maya Lowlands.
    \newblock {\em Science}, 292:1367--1370, 2001.

  \bibitem[Peterson, 2006]{peterson2006}
   L.~C.~Peterson and G.~H.~Haug.
   \newblock 150 Jahre Trockenheit.
   \newblock {\em Spektrum der Wissenschaft}, Januar 2006.

  \bibitem[Wiki: Cultura maya]{wiki:culturamaya}
   Wikipedia in Spanish
   \newblock Cultura maya
   \newblock {\em\url{http://es.wikipedia.org/wiki/Antiguos_mayas}}

  \bibitem[Wiki: Maya]{wiki:maya}
   Wikipedia in German
   \newblock Cultura maya
   \newblock {\em\url{http://de.wikipedia.org/wiki/Maya}}
   
  \bibitem[Wiki: Maya Civilization]{wiki:mayacivilization}
   Wikipedia in English
   \newblock Cultura maya
   \newblock {\em\url{http://en.wikipedia.org/wiki/Maya_civilization}}
  
\end{thebibliography}

\end{document}