Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

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Line 9:

== TIMOR TRIASSIC AGGLUTINATED FORAMINIFERA ==

−

[[Image:JFR_cover.gif|left|80px| ]]Forty-nine species of organic-cemented siliceous agglutinated foraminifera are described from 11 different facies associations representing basinal deposits of the Triassic in Timor Leste. The facies associations containing the foraminifera range from those influenced by sediment derived from nearby carbonate banks to prodelta and delta-front associations. A survey of equivalent faunas from selected shallow-marine basins ranging from the Carboniferous to the mid-Cretaceous illustrates the conservative development through time of the siliceous agglutinated foraminifera.

+

[[Image:JFR_cover.gif|left|80px| ]]Forty-nine species of organic-cemented siliceous agglutinated foraminifera are described from 11 different facies associations representing basinal deposits of the Triassic in Timor Leste. The facies associations containing the foraminifera range from those influenced by sediment derived from nearby carbonate banks to prodelta and delta-front associations. A survey of equivalent faunas from selected shallow-marine basins ranging from the Carboniferous to the mid-Cretaceous illustrates the conservative development through time of the siliceous agglutinated foraminifera.

(from [http://jfr.geoscienceworld.org/cgi/content/abstract/40/4/366 ABSTRACT])

Line 20:

== LIVE FAUNAS ALONG A BATHYMETRICAL TRANSECT ==

−

[[Image:RevueDeMicropaleontologie_front.gif|left|80px| ]]In a 10-stations bathymetrical transect in the Bay of Biscay, we observed important changes in the density, composition and microhabitats of live foraminiferal faunas from the outer continental shelf to the abyssal plain.....The foraminiferal data together with the pore water data in the sediment give evidence of the presence of a trophic gradient from very eutrophic settings at the upper continental shelf towards oligotrophic settings at the abyssal area.

+

[[Image:RevueDeMicropaleontologie_front.gif|left|80px| ]]In a 10-stations bathymetrical transect in the Bay of Biscay, we observed important changes in the density, composition and microhabitats of live foraminiferal faunas from the outer continental shelf to the abyssal plain.....The foraminiferal data together with the pore water data in the sediment give evidence of the presence of a trophic gradient from very eutrophic settings at the upper continental shelf towards oligotrophic settings at the abyssal area.

(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7587-4YH4985-1&_user=10&_coverDate=09%2F30%2F2010&_rdoc=4&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%2312919%232010%23999469996%232292764%23FLA%23display%23Volume)&_cdi=12919&_sort=d&_docanchor=&_ct=7&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=f732cbbbee4fcbb261c7d6add99e8cd4&searchtype=a ABSTRACT])

Line 33:

== FORAMINIFERAL RESPONSES TO ABSENCE OF FRESH PHYTODETRITUS==

−

[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]The study illustrates that the quality of organic material has an important impact on the composition and maintenance of some benthic foraminiferal communities, that the faunal response to reduction, or even a halt, in the supply of fresh phytodetritus, is not necessarily immediate or dramatic, and that the response depends on the trophic conditions prevailing in the area when the halt occurs.

+

[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]The study illustrates that the quality of organic material has an important impact on the composition and maintenance of some benthic foraminiferal communities, that the faunal response to reduction, or even a halt, in the supply of fresh phytodetritus, is not necessarily immediate or dramatic, and that the response depends on the trophic conditions prevailing in the area when the halt occurs.

(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VCV-508CVFK-1&_user=5813503&_coverDate=09/30/2010&_rdoc=3&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%235964%232010%23999239996%232310755%23FLA%23display%23Volume)&_cdi=5964&_sort=d&_docanchor=&_ct=7&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=45ce28609d96829e489912b00c00dc34&searchtype=a ABSTRACT])

Line 45:

== ONTOGNETIC EFFECTS ON δ¹³C and δ18O ==

−

[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]We determined the stable oxygen and carbon isotopic composition of live (Rose Bengal stained) tests belonging to different size classes of two benthic foraminiferal species from the Pakistan continental margin. Our data underline the necessity to base longer δ18O and δ13C isotope records derived from benthic foraminifera on size windows of 100 μm or less. This is already common practice in down-core isotopic studies of planktonic foraminifera.

+

[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]We determined the stable oxygen and carbon isotopic composition of live (Rose Bengal stained) tests belonging to different size classes of two benthic foraminiferal species from the Pakistan continental margin. Our data underline the necessity to base longer δ18O and δ13C isotope records derived from benthic foraminifera on size windows of 100 μm or less. This is already common practice in down-core isotopic studies of planktonic foraminifera.

(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VCV-50CVR13-1&_user=5813503&_coverDate=09/30/2010&_rdoc=5&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%235964%232010%23999239996%232310755%23FLA%23display%23Volume)&_cdi=5964&_sort=d&_docanchor=&_ct=7&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=649bd3abfa34d3a55ee38aa460b0c4c4&searchtype=a ABSTRACT])

Line 58:

== PHANEROZOIC DIVERSITY OF AGGLUTINATED FORAMINIFERA ==

−

[[Image:App-cov.jpg|left|80px| ]]New diversity curves for agglutinated foraminiferal genera are presented based on the stratigraphic ranges of 764 genera distributed over the 91 Phanerozoic chronostratigraphic subdivisions given in the ICS timescale.

+

[[Image:App-cov.jpg|left|80px| ]]New diversity curves for agglutinated foraminiferal genera are presented based on the stratigraphic ranges of 764 genera distributed over the 91 Phanerozoic chronostratigraphic subdivisions given in the ICS timescale.

(from [http://www.app.pan.pl/article/item/app20090090.html ABSTRACT])

Line 70:

== [[FORAMINIFERA IN SOIL]] ==

−

[[Image:Soilforams.jpg|left|80px| ]]Environmental SSU rDNA-based surveys show that Foraminifera are a widespread and diverse component of soil microbial communities. Phylogenetic analysis clusters them in four groups branching among the radiation of early foraminiferal lineages. Identification of terrestrial foraminiferal species and understanding of their ecological role represent an exciting challenge for future research.

+

[[Image:Soilforams.jpg|left|80px| ]]Environmental SSU rDNA-based surveys show that Foraminifera are a widespread and diverse component of soil microbial communities. Phylogenetic analysis clusters them in four groups branching among the radiation of early foraminiferal lineages. Identification of terrestrial foraminiferal species and understanding of their ecological role represent an exciting challenge for future research.

(from [http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2010.02225.x/abstract ABSTRACT])

Line 83:

== JURASSIC VENT FORAMINIFERA ==

−

[[Image:App-cov.jpg|left|80px| ]]''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a black claystone overlying the manganese deposits in the Western Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow−water exhalative submarine hydrothermal vent that was active in the early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents (from [http://www.app.pan.pl/article/item/app20090082.html ABSTRACT]).

+

[[Image:App-cov.jpg|left|80px| ]]''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a black claystone overlying the manganese deposits in the Western Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow−water exhalative submarine hydrothermal vent that was active in the early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents (from [http://www.app.pan.pl/article/item/app20090082.html ABSTRACT]).

----

Line 94:

== DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES ==

−

[[Image:Deep-Sea_Research_II_front.gif|left|80px| ]]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:Deep-Sea_Research_II_front.gif|left|80px| ]]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.

(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]).

----

Line 104:

== GEOCHEMICAL PROXIES IN FORAMINIFERA ==

−

[[Image:JFR_cover.gif|left|80px| ]]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.

+

[[Image:JFR_cover.gif|left|80px| ]]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.

(from [http://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 ABSTRACT]).

----

Line 114:

== SURVIVAL OF BENTHIC FORAMINIFERAL PROPAGULES ==

−

[[Image:J_Sea_Research_Front.gif|left|80px| ]]New data support our previously published propagule dispersal hypothesis and show that propagules of some benthic foraminiferal species can survive for two years before growth commences. Our results indicate substantial inter-specific differences in dispersal potential and support previous suggestions that among free-living species, some serial forms have the potential for long-distance dispersal.

+

[[Image:J_Sea_Research_Front.gif|left|80px| ]]New data support our previously published propagule dispersal hypothesis and show that propagules of some benthic foraminiferal species can survive for two years before growth commences. Our results indicate substantial inter-specific differences in dispersal potential and support previous suggestions that among free-living species, some serial forms have the potential for long-distance dispersal.

(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VHH-4XCYJJ8-1&_user=5813503&_coverDate=01/31/2010&_rdoc=5&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236067%232010%23999369998%231577514%23FLA%23display%23Volume)&_cdi=6067&_sort=d&_docanchor=&_ct=9&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=59e9aea6614eab0d6728f9ad08c56349&searchtype=a ABSTRACT]).

----

Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA"

Revision as of 11:44, 14 October 2010

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@@ Line 9: / Line 9: @@
 == TIMOR TRIASSIC AGGLUTINATED FORAMINIFERA ==
-[[Image:JFR_cover.gif|left|80px| ]]<font size="3">Forty-nine species of organic-cemented siliceous agglutinated foraminifera are described from 11 different facies associations representing basinal deposits of the Triassic in Timor Leste. The facies associations containing the foraminifera range from those influenced by sediment derived from nearby carbonate banks to prodelta and delta-front associations. A survey of equivalent faunas from selected shallow-marine basins ranging from the Carboniferous to the mid-Cretaceous illustrates the conservative development through time of the siliceous agglutinated foraminifera.
+[[Image:JFR_cover.gif|left|80px| ]]<font size="2">Forty-nine species of organic-cemented siliceous agglutinated foraminifera are described from 11 different facies associations representing basinal deposits of the Triassic in Timor Leste. The facies associations containing the foraminifera range from those influenced by sediment derived from nearby carbonate banks to prodelta and delta-front associations. A survey of equivalent faunas from selected shallow-marine basins ranging from the Carboniferous to the mid-Cretaceous illustrates the conservative development through time of the siliceous agglutinated foraminifera.
 <font size="2">(from [http://jfr.geoscienceworld.org/cgi/content/abstract/40/4/366 ABSTRACT])
@@ Line 20: / Line 20: @@
 == LIVE FAUNAS ALONG A BATHYMETRICAL TRANSECT ==
-[[Image:RevueDeMicropaleontologie_front.gif|left|80px| ]]<font size="3">In a 10-stations bathymetrical transect in the Bay of Biscay, we observed important changes in the density, composition and microhabitats of live foraminiferal faunas from the outer continental shelf to the abyssal plain.....The foraminiferal data together with the pore water data in the sediment give evidence of the presence of a trophic gradient from very eutrophic settings at the upper continental shelf towards oligotrophic settings at the abyssal area.
+[[Image:RevueDeMicropaleontologie_front.gif|left|80px| ]]<font size="2">In a 10-stations bathymetrical transect in the Bay of Biscay, we observed important changes in the density, composition and microhabitats of live foraminiferal faunas from the outer continental shelf to the abyssal plain.....The foraminiferal data together with the pore water data in the sediment give evidence of the presence of a trophic gradient from very eutrophic settings at the upper continental shelf towards oligotrophic settings at the abyssal area.
 <font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B7587-4YH4985-1&_user=10&_coverDate=09%2F30%2F2010&_rdoc=4&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%2312919%232010%23999469996%232292764%23FLA%23display%23Volume)&_cdi=12919&_sort=d&_docanchor=&_ct=7&_acct=C000050221&_version=1&_urlVersion=0&_userid=10&md5=f732cbbbee4fcbb261c7d6add99e8cd4&searchtype=a ABSTRACT])
@@ Line 33: / Line 33: @@
 == FORAMINIFERAL RESPONSES TO ABSENCE OF FRESH PHYTODETRITUS==
-[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]<font size="3">The study illustrates that the quality of organic material has an important impact on the composition and maintenance of some benthic foraminiferal communities, that the faunal response to reduction, or even a halt, in the supply of fresh phytodetritus, is not necessarily immediate or dramatic, and that the response depends on the trophic conditions prevailing in the area when the halt occurs.
+[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]<font size="2">The study illustrates that the quality of organic material has an important impact on the composition and maintenance of some benthic foraminiferal communities, that the faunal response to reduction, or even a halt, in the supply of fresh phytodetritus, is not necessarily immediate or dramatic, and that the response depends on the trophic conditions prevailing in the area when the halt occurs.
 <font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VCV-508CVFK-1&_user=5813503&_coverDate=09/30/2010&_rdoc=3&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%235964%232010%23999239996%232310755%23FLA%23display%23Volume)&_cdi=5964&_sort=d&_docanchor=&_ct=7&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=45ce28609d96829e489912b00c00dc34&searchtype=a ABSTRACT])
@@ Line 45: / Line 45: @@
 == ONTOGNETIC EFFECTS ON δ&sup1;&sup3;C and δ18O ==
-[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]<font size="3">We determined the stable oxygen and carbon isotopic composition of live (Rose Bengal stained) tests belonging to different size classes of two benthic foraminiferal species from the Pakistan continental margin. Our data underline the necessity to base longer δ18O and δ13C isotope records derived from benthic foraminifera on size windows of 100 μm or less. This is already common practice in down-core isotopic studies of planktonic foraminifera.
+[[Image:Marine_Micropaleontology_Front.gif|left|80px| ]]<font size="2">We determined the stable oxygen and carbon isotopic composition of live (Rose Bengal stained) tests belonging to different size classes of two benthic foraminiferal species from the Pakistan continental margin. Our data underline the necessity to base longer δ18O and δ13C isotope records derived from benthic foraminifera on size windows of 100 μm or less. This is already common practice in down-core isotopic studies of planktonic foraminifera.
 <font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VCV-50CVR13-1&_user=5813503&_coverDate=09/30/2010&_rdoc=5&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%235964%232010%23999239996%232310755%23FLA%23display%23Volume)&_cdi=5964&_sort=d&_docanchor=&_ct=7&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=649bd3abfa34d3a55ee38aa460b0c4c4&searchtype=a ABSTRACT])
@@ Line 58: / Line 58: @@
 == PHANEROZOIC DIVERSITY OF AGGLUTINATED FORAMINIFERA ==
-[[Image:App-cov.jpg|left|80px| ]]<font size="3">New diversity curves for agglutinated foraminiferal genera are presented based on the stratigraphic ranges of 764 genera distributed over the 91 Phanerozoic chronostratigraphic subdivisions given in the ICS timescale.
+[[Image:App-cov.jpg|left|80px| ]]<font size="2">New diversity curves for agglutinated foraminiferal genera are presented based on the stratigraphic ranges of 764 genera distributed over the 91 Phanerozoic chronostratigraphic subdivisions given in the ICS timescale.
 <font size="2">(from [http://www.app.pan.pl/article/item/app20090090.html ABSTRACT])
@@ Line 70: / Line 70: @@
 == [[FORAMINIFERA IN SOIL]] ==
-[[Image:Soilforams.jpg|left|80px| ]]<font size="3">Environmental SSU rDNA-based surveys show that Foraminifera are a widespread and diverse component of soil microbial communities. Phylogenetic analysis clusters them in four groups branching among the radiation of early foraminiferal lineages. Identification of terrestrial foraminiferal species and understanding of their ecological role represent an exciting challenge for future research.
+[[Image:Soilforams.jpg|left|80px| ]]<font size="2">Environmental SSU rDNA-based surveys show that Foraminifera are a widespread and diverse component of soil microbial communities. Phylogenetic analysis clusters them in four groups branching among the radiation of early foraminiferal lineages. Identification of terrestrial foraminiferal species and understanding of their ecological role represent an exciting challenge for future research.
 <font size="2">(from [http://onlinelibrary.wiley.com/doi/10.1111/j.1462-2920.2010.02225.x/abstract ABSTRACT])
@@ Line 83: / Line 83: @@
 == JURASSIC VENT FORAMINIFERA ==
-[[Image:App-cov.jpg|left|80px| ]]<font size="3">''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a black claystone overlying the manganese deposits in the Western Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow−water exhalative submarine hydrothermal vent that was active in the early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents <font size="2">(from [http://www.app.pan.pl/article/item/app20090082.html ABSTRACT]).
+[[Image:App-cov.jpg|left|80px| ]]<font size="2">''Recurvoides infernus'' sp. nov., one of the oldest representatives of the superfamily Recurvoidacea (Foraminifera), is described from a black claystone overlying the manganese deposits in the Western Tatra Mountains (Poland). These manganese carbonates/silicates were laid down around a shallow−water exhalative submarine hydrothermal vent that was active in the early Toarcian. The microfossils are possibly the first described Jurassic foraminifera associated with hydrothermal vents <font size="2">(from [http://www.app.pan.pl/article/item/app20090082.html ABSTRACT]).
 ----
@@ Line 94: / Line 94: @@
 == DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES ==
-[[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.
+[[Image:Deep-Sea_Research_II_front.gif|left|80px| ]]<font size="2">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://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]).
 ----
@@ Line 104: / Line 104: @@
 == GEOCHEMICAL PROXIES IN FORAMINIFERA ==
-[[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.
+[[Image:JFR_cover.gif|left|80px| ]]<font size="2">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://jfr.geoscienceworld.org/cgi/content/abstract/40/2/165 ABSTRACT]).
 ----
@@ Line 114: / Line 114: @@
 == SURVIVAL OF BENTHIC FORAMINIFERAL PROPAGULES ==
-[[Image:J_Sea_Research_Front.gif|left|80px| ]]<font size="3">New data support our previously published propagule dispersal hypothesis and show that propagules of some benthic foraminiferal species can survive for two years before growth commences. Our results indicate substantial inter-specific differences in dispersal potential and support previous suggestions that among free-living species, some serial forms have the potential for long-distance dispersal.
+[[Image:J_Sea_Research_Front.gif|left|80px| ]]<font size="2">New data support our previously published propagule dispersal hypothesis and show that propagules of some benthic foraminiferal species can survive for two years before growth commences. Our results indicate substantial inter-specific differences in dispersal potential and support previous suggestions that among free-living species, some serial forms have the potential for long-distance dispersal.
 <font size="2">(from [http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6VHH-4XCYJJ8-1&_user=5813503&_coverDate=01/31/2010&_rdoc=5&_fmt=high&_orig=browse&_origin=browse&_zone=rslt_list_item&_srch=doc-info(%23toc%236067%232010%23999369998%231577514%23FLA%23display%23Volume)&_cdi=6067&_sort=d&_docanchor=&_ct=9&_acct=C000068454&_version=1&_urlVersion=0&_userid=5813503&md5=59e9aea6614eab0d6728f9ad08c56349&searchtype=a ABSTRACT]).
 ----