Difference between revisions of "RECENT PUBLICATIONS ON FORAMINIFERA 2010"
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== BENTHIC FORAMINIFERA IN TEMPERATE CORALS == | == BENTHIC FORAMINIFERA IN TEMPERATE CORALS == | ||
| − | + | [[Image:JFR_cover.gif|left|80px| ]]<font size="2"> Foraminiferal and sedimentary analyses were performed on upper Pliocene exposures in the Almería-Níjar basin (SE) to determine its depositional history. The composite stratigraphic section reveals that, during the late Pliocene, a restricted coastal bay with coral banks was being filled with the siliciclastic sediments of prograding fan deltas. In the lower part of the Rambla Quebrada section, fine-grained sediments with ''Cibicides refulgens'', ''Cibicidoides'' spp., ''Asterigerinata'' spp., ''Rosalina globularis'', ''Lenticulina calcar'', and carinate elphidiids indicate deposition in a distal part of the bay where the marine influence was greatest. Epiphytic species dominate in the lower part of the section and suggest that the distal substrate was densely vegetated. In contrast, the upper part of the section is dominated by taxa characteristic of very shallow brackish environments, notably ''Ammonia'' spp. and noncarinate elphidiids. Mud-dwellers inhabiting soft bottoms dominate in the middle-to-upper part of the studied sections. Here, ''Cancris auriculus'', ''Nonion asterizans'', and ''Cassidulina neocarinata'' are also locally abundant. These species are usually abundant on substrata with high contents of organic matter, which in this study could be attributed to the increased nutrient flow from the fan deltas prograding into the basin. Higher in the section, varve-like laminae that include species known to be tolerant of disoxia indicate that geomorphic restriction of the bay weakened the mixing of marine and fresh water, which allowed its water column to stratify and develop low-oxygen bottom conditions.<font size="2"> (from [http://www.jfr.geoscienceworld.org/cgi/content/abstract/40/1/61 ABSTRACT]) | |
| − | [[Image:JFR_cover.gif|left|80px| ]]<font size="2"> Foraminiferal and sedimentary analyses were performed on upper Pliocene exposures in the Almería-Níjar basin | ||
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| − | Pérez-Asensio, J. N. | + | Pérez-Asensio, J. N., Aguirre, J. (2010). [http://www.jfr.geoscienceworld.org/cgi/content/abstract/40/1/61 Benthic foraminiferal assemblages in temperate coral-bearing deposits from the late Pliocene]. Journal of Foraminiferal Research 40 (1), 61-78. |
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== FORAMINIFERA-BASED TRANSFER FUNCTION == | == FORAMINIFERA-BASED TRANSFER FUNCTION == | ||
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== EVOLUTIONARY CLASSIFICATION OF WHITEINELLIDS == | == EVOLUTIONARY CLASSIFICATION OF WHITEINELLIDS == | ||
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== HOLOTYPES IN THE TAXONOMY OF FORAMINIFERAL MORPHOSPECIES == | == HOLOTYPES IN THE TAXONOMY OF FORAMINIFERAL MORPHOSPECIES == | ||
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== LIVE BENTHIC FORAMINIFERA IN A CANYON == | == LIVE BENTHIC FORAMINIFERA IN A CANYON == | ||
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== CHLOROPLAST HUSBANDARY AND KLEPTOPLASTIDY IN FORAMINIFERA == | == CHLOROPLAST HUSBANDARY AND KLEPTOPLASTIDY IN FORAMINIFERA == | ||
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== THE FIDELITY OF SHELL-DERIVED δ<SUP>18</SUP>O<SUB>seawater</SUB> ESTIMATES == | == THE FIDELITY OF SHELL-DERIVED δ<SUP>18</SUP>O<SUB>seawater</SUB> ESTIMATES == | ||
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== Mg/Ca IN <i>Globorotalia inflata</i> AND <i>Globigerinoides bulloides</i> == | == Mg/Ca IN <i>Globorotalia inflata</i> AND <i>Globigerinoides bulloides</i> == | ||
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== Mg/Ca, δ<sup>18</sup>O AND SALINITY IN ''Ammonia beccarii'' == | == Mg/Ca, δ<sup>18</sup>O AND SALINITY IN ''Ammonia beccarii'' == | ||
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== SANTONIAN-CAMPANIAN BIOSTRATIGRAPHY AND PALAEOENVIRONMENT == | == SANTONIAN-CAMPANIAN BIOSTRATIGRAPHY AND PALAEOENVIRONMENT == | ||
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== PALAEOZOIC FORAMINIFERA == | == PALAEOZOIC FORAMINIFERA == | ||
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== [[MODERN FORAMINIFERAL DISTRIBUTION AND DIVERSITY IN ATOLLS]] == | == [[MODERN FORAMINIFERAL DISTRIBUTION AND DIVERSITY IN ATOLLS]] == | ||
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== CENOZOIC TROPICAL PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHY == | == CENOZOIC TROPICAL PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHY == | ||
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== ENVIRONMENTAL CONTROLS ON A RIVER-DOMINATED SHELF == | == ENVIRONMENTAL CONTROLS ON A RIVER-DOMINATED SHELF == | ||
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== THE RATE OF 20TH CENTURY SEA LEVEL RISE == | == THE RATE OF 20TH CENTURY SEA LEVEL RISE == | ||
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== WHAT HAPPENS WHEN THE OCEAN IS OVERHEATED? == | == WHAT HAPPENS WHEN THE OCEAN IS OVERHEATED? == | ||
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== TIMOR TRIASSIC AGGLUTINATED FORAMINIFERA == | == TIMOR TRIASSIC AGGLUTINATED FORAMINIFERA == | ||
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== LIVE FAUNAS ALONG A BATHYMETRICAL TRANSECT == | == LIVE FAUNAS ALONG A BATHYMETRICAL TRANSECT == | ||
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== FORAMINIFERAL RESPONSES TO ABSENCE OF FRESH PHYTODETRITUS== | == FORAMINIFERAL RESPONSES TO ABSENCE OF FRESH PHYTODETRITUS== | ||
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== ONTOGENETIC EFFECTS ON δ¹³C and δ<sup>18</sup>O == | == ONTOGENETIC EFFECTS ON δ¹³C and δ<sup>18</sup>O == | ||
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== PHANEROZOIC DIVERSITY OF AGGLUTINATED FORAMINIFERA == | == PHANEROZOIC DIVERSITY OF AGGLUTINATED FORAMINIFERA == | ||
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== [[FORAMINIFERA IN SOIL]] == | == [[FORAMINIFERA IN SOIL]] == | ||
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== JURASSIC VENT FORAMINIFERA == | == JURASSIC VENT FORAMINIFERA == | ||
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==DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES == | ==DECADAL-SCALE CHANGES IN ABYSSAL FORAMINIFERAL ASSEMBLAGES == | ||
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== DAN-C2 HYPERTHERMAL EVENT AT GUBBIO == | == DAN-C2 HYPERTHERMAL EVENT AT GUBBIO == | ||
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== ECOLOGICAL AND EVOLUTIONARY RESPONSE TO MECO == | == ECOLOGICAL AND EVOLUTIONARY RESPONSE TO MECO == | ||
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== [[GEOCHEMICAL PROXIES IN FORAMINIFERA]] == | == [[GEOCHEMICAL PROXIES IN FORAMINIFERA]] == | ||
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== NITRATE STORAGE AND DENITRIFICATION == | == NITRATE STORAGE AND DENITRIFICATION == | ||
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== SURVIVAL OF BENTHIC FORAMINIFERAL PROPAGULES == | == SURVIVAL OF BENTHIC FORAMINIFERAL PROPAGULES == | ||
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<font size="2">Alve, E., Goldstein, S.T., 2010. [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 Dispersal, survival and delayed growth of benthic foraminiferal propagules]. Journal of Sea Research 63 (1): 36-51. | <font size="2">Alve, E., Goldstein, S.T., 2010. [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 Dispersal, survival and delayed growth of benthic foraminiferal propagules]. Journal of Sea Research 63 (1): 36-51. | ||
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<font size="4"> | <font size="4"> | ||
| − | + | {{Recent Publications on Foraminifera Navigation}}<font size="2"> | |
[[category:recent publications]] | [[category:recent publications]] | ||
