[From nobody Fri Nov 6 11:57:58 2009 Return-Path: <owner-quaternary@CLIFFY.UCS.MUN.CA> Received: from mailrelay.williams.edu (EHLO mailrelay.williams.edu) ([137.165.4.207]) by miram5000a.williams.edu (MOS 3.10.4-GA FastPath queued) with ESMTP id AHF92968; Thu, 05 Nov 2009 13:09:37 -0500 (EST) X-IronPort-Anti-Spam-Filtered: true X-IronPort-Anti-Spam-Result: AoUBAF+j8kqGmegqmWdsb2JhbACCJC2ZFgEBAQEBCAsKBxPERYIugg8E X-IronPort-AV: E=Sophos; i="4.44,687,1249272000"; d="scan'208,217"; a="11184472" Received: from cliffy.ucs.mun.ca ([134.153.232.42]) by mailgate.williams.edu with ESMTP; 05 Nov 2009 13:09:36 -0500 Received: from cliffy.ucs.mun.ca (cliffy.ucs.mun.ca [134.153.232.42]) by cliffy.ucs.mun.ca (8.12.11.20060308/8.12.11) with ESMTP id nA45Luep000573; Thu, 5 Nov 2009 14:33:37 -0330 Received: by CLIFFY.UCS.MUN.CA (LISTSERV-TCP/IP release 14.3) with spool id 28468367 for QUATERNARY@CLIFFY.UCS.MUN.CA; Thu, 5 Nov 2009 14:33:25 -0330 Received: from fitzgerald.ucs.mun.ca (fitzgerald.ucs.mun.ca [134.153.232.57]) by cliffy.ucs.mun.ca (8.12.11.20060308/8.12.11) with ESMTP id nA5I3Pmc009157 for <quaternary@cliffy.ucs.mun.ca>; Thu, 5 Nov 2009 14:33:25 -0330 Received: from peterson.ucs.mun.ca (peterson.ucs.mun.ca [134.153.232.35]) by fitzgerald.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id nA5I3L41025448 for <quaternary@cliffy.ucs.mun.ca>; Thu, 5 Nov 2009 14:33:21 -0330 Received: from ellington.ucs.mun.ca (ellington.ucs.mun.ca [134.153.232.51]) by peterson.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id nA5I3LVA029064 for <quaternary@morgan.ucs.mun.ca>; Thu, 5 Nov 2009 14:33:21 -0330 Received: from gse-mta-17.emailfiltering.com (ixe-mta-17-tx.emailfiltering.com [194.116.198.149]) by ellington.ucs.mun.ca (8.13.1/8.13.1) with ESMTP id nA5I3FSm007623 for <quaternary@morgan.ucs.mun.ca>; Thu, 5 Nov 2009 14:33:16 -0330 Received: from exch-relay.rhul.ac.uk ([134.219.205.9]) by gse-mta-17.emailfiltering.com with emfmta (version 4.1.0.193.1.rd-3.2.3-libc2.3.2) vanilla id 1652937320 for quaternary@morgan.ucs.mun.ca; Thu, 05 Nov 2009 18:03:09 +0000 Received: from exch-db-05.cc.rhul.local ([134.219.205.5]) by EXCH-RELAY-02.rhul.ac.uk with Microsoft SMTPSVC(6.0.3790.3959); Thu, 5 Nov 2009 18:03:09 +0000 X-MimeOLE: Produced By Microsoft Exchange V6.5 Content-class: urn:content-classes:message MIME-Version: 1.0 Content-Type: multipart/alternative; boundary="----_=_NextPart_001_01CA5E42.3B6C2E28" X-MS-Has-Attach: X-MS-TNEF-Correlator: Thread-Topic: Geomorphic response to environmental change: Coupling climate and landscape records Thread-Index: AcpeQjq1XEWY4QUDTlq/QxZrC+nu7A== X-OriginalArrivalTime: 05 Nov 2009 18:03:09.0380 (UTC) FILETIME=[3B92A840:01CA5E42] X-Spam-Flag: NO X-Spam-Checker-Version: SpamAssassin 3.002004 (2008-01-01) X-Spam-Status: No, hits=0.1 required=4.0 tests=HTML_MESSAGE,RECVMORGAN version=3.2.4 X-Spam-Report: 0.1 RECVMORGAN Forged received site * 0.0 HTML_MESSAGE BODY: HTML included in message X-Scanned-By: MIMEDefang 2.67 on 134.153.232.57 X-Scanned-By: MIMEDefang 2.67 on 134.153.232.51 Message-ID: <570A1E8C2E229F4B96A70E010278604001BACA35@exch-db-05.cc.rhul.local> Date: Thu, 5 Nov 2009 18:03:09 -0000 Reply-To: Armitage Simon <Simon.Armitage@RHUL.AC.UK> Sender: Research in Quaternary Science <QUATERNARY@CLIFFY.UCS.MUN.CA> From: Armitage Simon <Simon.Armitage@RHUL.AC.UK> Subject: Geomorphic response to environmental change: Coupling climate and landscape records To: QUATERNARY@CLIFFY.UCS.MUN.CA Precedence: list This is a multi-part message in MIME format. ------_=_NextPart_001_01CA5E42.3B6C2E28 Content-Type: text/plain; charset="US-ASCII" Content-Transfer-Encoding: quoted-printable Geomorphic response to environmental change: Coupling climate and landscape records =20 EGU General Assembly 2010: Session GM4.1 =20 Dear Colleagues, =20 We are pleased to announce a session entitled "Geomorphic response to environmental change: Coupling climate and landscape records" at the EGU General Assembly in May 2010. =20 Session description: Environmental changes during the Quaternary can act as an important model for understanding the nature and impact of future global change. The oscillation of climates and environments during this period can be long-term (i.e. interglacial/glacial cycles) or short-term (i.e. sub-Milankovitch events such as Dansgaard-Oeschgar cycles, the Younger Dryas or the Little Ice Age). With respect to understanding the impacts of future climate change, establishing the magnitude of temperature and precipitation fluctuations during these events is only part of the issue, just as significant is understanding how Earth surface processes will respond to these events. An important step in Quaternary geomorphology is, therefore, being able to relate the shifts in climate records (i.e. marine, ice-core, speleothem and pollen signals) to changes in the activity of Earth surface processes (i.e. rivers, slopes, glaciers, Aeolian and soils). =20 The aim of this session is to provide a forum for researchers who are working on geomorphic response to palaeoenvironmental change to present their latest findings and discuss future directions. It is hoped that, as well as providing case studies of coupled records, the session will address some of the following key themes: 1) techniques for correlation (geochronology, stratigraphy etc); 2) the identification and use of suitable climate records; 3) quantifying the magnitude and timescales of change in different geomorphic settings (e.g. fluvial, glacial, aeolian etc); and 4) distinguishing climate driven response from other forcing factors (tectonics, complex response, intrinsic forcing). The session will have a very broad temporal and spatial scope, with submissions from authors working on Pleistocene and Holocene time frames, long-term and short-term climate forcing, in high through to low latitude environments and covering the full scope of geomorphic processes. =20 Abstracts must be submitted by the 18th of January 2010 using the EGU General Assembly website: =20 http://meetingorganizer.copernicus.org/EGU2010/session/3057 =20 =20 We look forward to seeing you in May. =20 Best wishes, Varyl Thorndycraft (varyl.thorndycraft@rhul.ac.uk) Ian Candy (ian.candy@rhul.ac.uk) <mailto:>=20 Simon Armitage (simon.armitage@rhul.ac.uk) =20 ------_=_NextPart_001_01CA5E42.3B6C2E28 Content-Type: text/html; charset="US-ASCII" Content-Transfer-Encoding: quoted-printable <html xmlns:o=3D"urn:schemas-microsoft-com:office:office" = xmlns:w=3D"urn:schemas-microsoft-com:office:word" = xmlns=3D"http://www.w3.org/TR/REC-html40"> <head> <META HTTP-EQUIV=3D"Content-Type" CONTENT=3D"text/html; = charset=3Dus-ascii"> <meta name=3DGenerator content=3D"Microsoft Word 11 (filtered medium)"> <style> <!-- /* Style Definitions */ p.MsoNormal, li.MsoNormal, div.MsoNormal {margin:0cm; margin-bottom:.0001pt; font-size:12.0pt; font-family:"Times New Roman";} a:link, span.MsoHyperlink {color:blue; text-decoration:underline;} a:visited, span.MsoHyperlinkFollowed {color:purple; text-decoration:underline;} span.EmailStyle17 {mso-style-type:personal-compose; font-family:Arial; color:windowtext;} @page Section1 {size:595.3pt 841.9pt; margin:72.0pt 90.0pt 72.0pt 90.0pt;} div.Section1 {page:Section1;} --> </style> </head> <body lang=3DEN-GB link=3Dblue vlink=3Dpurple> <div class=3DSection1> <p class=3DMsoNormal style=3D'text-align:justify'><b><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial;font-weight:bold'>Geomorphic = response to environmental change: Coupling climate and landscape = records<o:p></o:p></span></font></b></p> <p class=3DMsoNormal style=3D'text-align:justify'><b><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial;font-weight:bold'><o:p>&nbsp;= </o:p></span></font></b></p> <p class=3DMsoNormal style=3D'text-align:justify'><b><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial;font-weight:bold'>EGU = General Assembly 2010: Session GM4.1<o:p></o:p></span></font></b></p> <p class=3DMsoNormal style=3D'text-align:justify'><b><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial;font-weight:bold'><o:p>&nbsp;= </o:p></span></font></b></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Dear = Colleagues,<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>We are pleased to announce = a session entitled &#8220;Geomorphic response to environmental change: Coupling = climate and landscape records&#8221; at the EGU General Assembly in May = 2010.<i><span style=3D'font-style:italic'><o:p></o:p></span></i></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><i><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial;font-style:italic'><o:p>&nbsp= ;</o:p></span></font></i></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Session = description:<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Environmental changes = during the Quaternary can act as an important model for understanding the nature = and impact of future global change. The oscillation of climates and = environments during this period can be long-term (i.e. interglacial/glacial cycles) = or short-term (i.e. sub-Milankovitch events such as Dansgaard-Oeschgar = cycles, the Younger Dryas or the Little Ice Age). With respect to understanding the = impacts of future climate change, establishing the magnitude of temperature and precipitation fluctuations during these events is only part of the = issue, just as significant is understanding how Earth surface processes will respond = to these events. An important step in Quaternary geomorphology is, = therefore, being able to relate the shifts in climate records (i.e. marine, = ice-core, speleothem and pollen signals) to changes in the activity of Earth = surface processes (i.e. rivers, slopes, glaciers, Aeolian and = soils).<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>The aim of this session is = to provide a forum for researchers who are working on geomorphic response = to palaeoenvironmental change to present their latest findings and discuss = future directions. It is hoped that, as well as providing case studies of = coupled records, the session will address some of the following key themes: 1) techniques for correlation (geochronology, stratigraphy etc); 2) the identification and use of suitable climate records; 3) quantifying the magnitude and timescales of change in different geomorphic settings = (e.g. fluvial, glacial, aeolian etc); and 4) distinguishing climate driven = response from other forcing factors (tectonics, complex response, intrinsic = forcing). The session will have a very broad temporal and spatial scope, with = submissions from authors working on Pleistocene and Holocene time frames, long-term = and short-term climate forcing, in high through to low latitude environments = and covering the full scope of geomorphic = processes.<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Abstracts must be submitted = by the <b><span style=3D'font-weight:bold'>18<sup>th</sup> of January 2010 = </span></b>using the EGU General Assembly website:<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><a href=3D"http://meetingorganizer.copernicus.org/EGU2010/session/3057">http= ://meetingorganizer.copernicus.org/EGU2010/session/3057</a><o:p></o:p></s= pan></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>We look forward to seeing = you in May.<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Best = wishes,<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Varyl Thorndycraft (<font color=3Dblue><span style=3D'color:blue'><a href=3D"mailto:varyl.thorndycraft@rhul.ac.uk">varyl.thorndycraft@rhul.ac.= uk</a></span></font>)<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Ian Candy (<a href=3D"mailto:ian.candy@rhul.ac.uk">ian.candy@rhul.ac.uk</a>)<font = color=3Dblue><span style=3D'color:blue'><a = href=3D"mailto:"></a></span></font><o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>Simon Armitage (<a href=3D"mailto:simon.armitage@rhul.ac.uk">simon.armitage@rhul.ac.uk</a>)<= o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'text-align:justify'><font size=3D3 = face=3DArial><span style=3D'font-size:12.0pt;font-family:Arial'><o:p>&nbsp;</o:p></span></fo= nt></p> </div> </body> </html> ------_=_NextPart_001_01CA5E42.3B6C2E28-- ]