Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

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== GEOCHEMICAL PROXIES IN FORAMINIFERA ==
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== DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES ==
  
[[Image:JFR_cover.gif|left|80px| ]]<font size="3">We review the geochemical proxies that utilize foraminiferal carbonate tests, including potential uses of the proxies for reconstructions through time: 18O, 13C, trace elements (Mg, Cd, Ba, Zn, B, U), 87Sr/86Sr, 26Mg, 11B, and Nd. Both planktic and benthic foraminifera are included.
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[[Image:Deep-Sea_Research_II_front.gif|left|80px| ]]<font size="3">Trends in the abundance, diversity and taxonomic composition of ‘live’ (rose Bengal stained) foraminiferal assemblages (0-1 cm layer, >63-µm fraction) were analysed in replicate multiple corer samples collected at the Porcupine Abyssal Plain (48˚ 50’ N, 16˚ 30’ W, 4850 m water depth) over a 13-yr period (1989-2002). Overall, the abyssal time-series revealed decadal-scale changes among shallow-infaunal foraminifera, more or less coincident with changes in the megafauna, as well as indications of shorter-term events related to seasonally-pulsed phytodetrital inputs.
<font size="2">(from [http://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 ABSTRACT]).
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<font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VGC-4YCFYYD-3&_user=5813503&_coverDate=08/01/2010&_rdoc=10&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236035%232010%23999429984%232116751%23FLA%23display%23Volume)&_cdi=6035&_sort=d&_docanchor=&_ct=14&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=7bce5606386a5d7b29a0d519979c1e4d&searchtype=a ABSTRACT]).
 
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<font size="2">Katz, M.E., Cramer, B.S., Franzese, A., Hönisch, B., Miller, K.G., Rosenthal, Y., Wright, J.D., 2010. [http://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 Traditional and emerging geochemical proxies in foraminifera]. Journal of Foraminiferal Research 40 (2): 165–192.
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<font size="2">Gooday, A.J., Malzone, M.G., Bett, B.J., Lamont, P.A., 2010. [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VGC-4YCFYYD-3&_user=5813503&_coverDate=08/01/2010&_rdoc=10&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236035%232010%23999429984%232116751%23FLA%23display%23Volume)&_cdi=6035&_sort=d&_docanchor=&_ct=14&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=7bce5606386a5d7b29a0d519979c1e4d&searchtype=a Decadal-scale changes in shallow-infaunal foraminiferal assemblages at the Porcupine Abyssal Plain, NE Atlantic]. Deep-Sea Research II 57, 1362-1382.
  
  
 
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<font size="4">
  
== DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES ==
+
== GEOCHEMICAL PROXIES IN FORAMINIFERA ==
  
[[Image:JFR_cover.gif|left|80px| ]]<font size="3">Trends in the abundance, diversity and taxonomic composition of ‘live’ (rose Bengal stained) foraminiferal assemblages (0-1 cm layer, >63-µm fraction) were analysed in replicate multiple corer samples collected at the Porcupine Abyssal Plain (48˚ 50’ N, 16˚ 30’ W, 4850 m water depth) over a 13-yr period (1989-2002). Overall, the abyssal time-series revealed decadal-scale changes among shallow-infaunal foraminifera, more or less coincident with changes in the megafauna, as well as indications of shorter-term events related to seasonally-pulsed phytodetrital inputs.
+
[[Image:JFR_cover.gif|left|80px| ]]<font size="3">We review the geochemical proxies that utilize foraminiferal carbonate tests, including potential uses of the proxies for reconstructions through time: 18O, 13C, trace elements (Mg, Cd, Ba, Zn, B, U), 87Sr/86Sr, 26Mg, 11B, and Nd. Both planktic and benthic foraminifera are included.
<font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VGC-4YCFYYD-3&_user=5813503&_coverDate=08/01/2010&_rdoc=10&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236035%232010%23999429984%232116751%23FLA%23display%23Volume)&_cdi=6035&_sort=d&_docanchor=&_ct=14&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=7bce5606386a5d7b29a0d519979c1e4d&searchtype=a ABSTRACT]).
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<font size="2">(from [http://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 ABSTRACT]).
 
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<font size="2">Gooday, A.J., Malzone, M.G., Bett, B.J., Lamont, P.A., 2010. [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VGC-4YCFYYD-3&_user=5813503&_coverDate=08/01/2010&_rdoc=10&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236035%232010%23999429984%232116751%23FLA%23display%23Volume)&_cdi=6035&_sort=d&_docanchor=&_ct=14&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=7bce5606386a5d7b29a0d519979c1e4d&searchtype=a Decadal-scale changes in shallow-infaunal foraminiferal assemblages at the Porcupine Abyssal Plain, NE Atlantic]. Deep-Sea Research II 57, 1362-1382.
+
<font size="2">Katz, M.E., Cramer, B.S., Franzese, A., Hönisch, B., Miller, K.G., Rosenthal, Y., Wright, J.D., 2010. [http://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 Traditional and emerging geochemical proxies in foraminifera]. Journal of Foraminiferal Research 40 (2): 165–192.
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Revision as of 17:09, 7 October 2010