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<DIV jQuery1372544188525="4"><CITE><SPAN 
class="slug-metadata-note ahead-of-print">Published Online <SPAN 
class=slug-ahead-of-print-date>June 6 2013</SPAN><BR></SPAN><ABBR 
class=slug-jnl-abbrev title=Science>Science</ABBR><SPAN class=slug-pub-date 
itemprop="datePublished"> 28 June 2013: </SPAN><BR><SPAN class=slug-vol>Vol. 340 
</SPAN><SPAN class=slug-issue>no. 6140 </SPAN><SPAN class=slug-pages>pp. 
1564-1566 </SPAN><BR>DOI: <SPAN class=slug-doi 
title=10.1126/science.1233797>10.1126/science.1233797 </SPAN></CITE></DIV>
<DIV jQuery1372544188525="4"><CITE><SPAN class=slug-doi 
title=10.1126/science.1233797><A 
href="http://www.sciencemag.org/content/340/6140/1564.abstract">http://www.sciencemag.org/content/340/6140/1564.abstract</A></SPAN></CITE></DIV>
<DIV> </DIV>
<DIV class="article abstract-view " jQuery1372544188525="6" 
itemprop="articleBody" sizset="0" sizcache="1"><SPAN 
class=highwire-journal-article-marker-start></SPAN> </DIV>
<DIV id=article-title-1 itemprop="headline"><FONT size=4>Varied Response of 
Western Pacific Hydrology to Climate Forcings over the Last Glacial 
Period</FONT></DIV>
<DIV id=contrib-1 class=contributor jQuery1372544188525="6" 
itemscope="itemscope" itemtype="http://schema.org/Person" itemprop="author" 
sizset="0" sizcache="0"><SPAN class=name itemprop="name"><A class=name-search 
href="http://www.sciencemag.org/search?author1=Stacy+A.+Carolin&sortspec=date&submit=Submit">Stacy 
A. Carolin</A></SPAN><A id=xref-aff-1-1 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-1" 
jQuery1372544188525="20"><SUP>1</SUP></A><SPAN class=xref-sep>,</SPAN><A 
id=xref-corresp-1-1 class=xref-corresp 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#corresp-1">*</A>, 
<SPAN class=name itemprop="name"><A class=name-search 
href="http://www.sciencemag.org/search?author1=Kim+M.+Cobb&sortspec=date&submit=Submit">Kim 
M. Cobb</A></SPAN><A id=xref-aff-1-2 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-1" 
jQuery1372544188525="21"><SUP>1</SUP></A>, <SPAN class=name itemprop="name"><A 
class=name-search 
href="http://www.sciencemag.org/search?author1=Jess+F.+Adkins&sortspec=date&submit=Submit">Jess 
F. Adkins</A></SPAN><A id=xref-aff-2-1 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-2" 
jQuery1372544188525="22"><SUP>2</SUP></A>, <SPAN class=name itemprop="name"><A 
class=name-search 
href="http://www.sciencemag.org/search?author1=Brian+Clark&sortspec=date&submit=Submit">Brian 
Clark</A></SPAN><A id=xref-aff-3-1 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-3" 
jQuery1372544188525="23"><SUP>3</SUP></A>, <SPAN class=name itemprop="name"><A 
class=name-search 
href="http://www.sciencemag.org/search?author1=Jessica+L.+Conroy&sortspec=date&submit=Submit">Jessica 
L. Conroy</A></SPAN><A id=xref-aff-1-3 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-1" 
jQuery1372544188525="24"><SUP>1</SUP></A>, <SPAN class=name itemprop="name"><A 
class=name-search 
href="http://www.sciencemag.org/search?author1=Syria+Lejau&sortspec=date&submit=Submit">Syria 
Lejau</A></SPAN><A id=xref-aff-3-2 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-3" 
jQuery1372544188525="25"><SUP>3</SUP></A>, <SPAN class=name itemprop="name"><A 
class=name-search 
href="http://www.sciencemag.org/search?author1=Jenny+Malang&sortspec=date&submit=Submit">Jenny 
Malang</A></SPAN><A id=xref-aff-3-3 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-3" 
jQuery1372544188525="26"><SUP>3</SUP></A>, <SPAN class=name><A class=name-search 
href="http://www.sciencemag.org/search?author1=Andrew+A.+Tuen&sortspec=date&submit=Submit">Andrew 
A. Tuen</A></SPAN><A id=xref-aff-4-1 class=xref-aff 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#aff-4" 
jQuery1372544188525="27"><SUP>4</SUP></A><SUP></SUP></DIV>
<DIV class=contributor jQuery1372544188525="6" itemscope="itemscope" 
itemtype="http://schema.org/Person" itemprop="author" sizset="0" 
sizcache="0"><SUP>1</SUP>School of Earth and Atmospheric Sciences, Georgia 
Institute of Technology, Atlanta, GA 30332, USA. <SUP>2</SUP>Division of 
Geological and Planetary Sciences, California Institute of Technology, Pasadena, 
CA 91125, USA. <SUP>3</SUP>Gunung Mulu National Park, Sarawak, Malaysia. 
<SUP>4</SUP>Institute of Biodiversity and Environmental Conservation, Universiti 
Malaysia Sarawak, Sarawak, Malaysia. <A class=rev-xref 
href="http://www.sciencemag.org/content/340/6140/1564.abstract#xref-corresp-1-1">↵</A><SPAN 
class=corresp-label>*</SPAN>Corresponding author. E-mail: <A 
href="mailto:stacy.carolin@gatech.edu">stacy.carolin@gatech.edu</A></DIV>
<DIV class="article abstract-view " jQuery1372544188525="45" 
itemprop="articleBody" sizset="0" sizcache="1"> </DIV>
<DIV class="article abstract-view " jQuery1372544188525="45" 
itemprop="articleBody" sizset="0" sizcache="1"><A class=current 
href="http://www.sciencemag.org/content/340/6140/tab-abstract" 
jQuery1372544188525="36"><FONT 
color=#000000><STRONG>Abstract</STRONG></FONT></A></DIV>
<DIV class="article abstract-view " jQuery1372544188525="45" 
itemprop="articleBody" sizset="0" sizcache="1"> </DIV>
<DIV jQuery1372544188525="46">Atmospheric deep convection in the west Pacific 
plays a key role in the global heat and moisture budgets, yet its response to 
orbital and abrupt climate change events is poorly resolved. Here, we present 
four absolutely dated, overlapping stalagmite oxygen isotopic records from 
northern Borneo that span most of the last glacial cycle. The records suggest 
that northern Borneo’s hydroclimate shifted in phase with precessional forcing 
but was only weakly affected by glacial-interglacial changes in global climate 
boundary conditions. Regional convection likely decreased during Heinrich 
events, but other Northern Hemisphere abrupt climate change events are notably 
absent. The new records suggest that the deep tropical Pacific hydroclimate 
variability may have played an important role in shaping the global response to 
the largest abrupt climate change events. </DIV></FONT></BODY></HTML>