| BENTHIC FORAMINIFERA IN HYPERSALINE SALWA BAY (SAUDI ARABIA): AN INSIGHT INTO FUTURE CLIMATE CHANGE IN THE GULF REGION? |
5 |
| MORPHOLOGICAL DISTINCTION OF THREE AMMONIA PHYLOTYPES OCCURRING ALONG EUROPEAN COASTS |
5 |
| RECENT BENTHIC FORAMINIFERS FROM THE SOUTH ATLANTIC SHELF OF ARGENTINA |
5 |
| IN SITU OBSERVATIONS OF FORAMINIFERAL BLEACHING IN THE MALDIVES, INDIAN OCEAN |
4 |
| IMPERFORATE LARGER BENTHIC FORAMINIFERA FROM SHALLOW-WATER CARBONATE FACIES (MIDDLE AND LATE EOCENE), ZAGROS MOUNTAINS, IRAN |
4 |
| UPPER HAUTERIVIAN-UPPER BARREMIAN PLANKTONIC FORAMINIFERAL ASSEMBLAGES FROM THE ARROYO GILICO SECTION (SOUTHERN SPAIN) |
3 |
| ASSESSMENT OF THE EFFECT OF INCREASING TEMPERATURE ON THE ECOLOGY AND ASSEMBLAGE STRUCTURE OF MODERN PLANKTIC FORAMINIFERS IN THE CARIBBEAN AND SURROUNDING SEAS |
3 |
| THE EFFECT OF TEMPERATURE AND FOOD CONCENTRATION ON INGESTION RATES OF QUINQUELOCULINA SEMINULA ON THE DIATOM NITZSCHIA CLOSTERIUM |
3 |
| COMBINED MOLECULAR AND MORPHOLOGICAL TAXONOMY OF THE BECCARII/T3 GROUP OF THE FORAMINIFERAL GENUS AMMONIA |
2 |
| ZOOGLIDER-BASED MEASUREMENTS OF PLANKTONIC FORAMINIFERA IN THE CALIFORNIA CURRENT SYSTEM |
2 |
| BENTHIC FORAMINIFERA AND GEOCHEMISTRY ACROSS THE PALEOCENE-EOCENE THERMAL MAXIMUM INTERVAL IN JORDAN |
2 |
| LATE QUATERNARY PALEOENVIRONMENTAL RECONSTRUCTION, USING BENTHIC FORAMINIFERA AND OSTRACODA, OF MARINE SEDIMENTARY BEDS ON THE SOUTHERN COAST OF LAIZHOU BAY, BOHAI SEA, CHINA |
2 |
| DISTRIBUTION OF MODERN SALT-MARSH FORAMINIFERA FROM THE EASTERN MISSISSIPPI SOUND, USA |
2 |
| SHALLOW-WATER BENTHIC FORAMINIFERA OF THE GALAPAGOS ARCHIPELAGO: ECOLOGICALLY SENSITIVE CARBONATE PRODUCERS IN AN ATYPICAL TROPICAL OCEANOGRAPHIC SETTING |
2 |
| INNER SHELF BENTHIC FORAMINIFERA OF THE SOUTH CHINA SEA, EAST COAST PENINSULAR MALAYSIA |
2 |
| STRATIGRAPHIC REVISION OF THE MIOCENE TREALLA LIMESTONE (CAPE RANGE, WESTERN AUSTRALIA): IMPLICATIONS FOR AUSTRALASIAN FORAMINIFERAL BIOSTRATIGRAPHY |
2 |
| WHAT, IF ANYTHING, IS A NUMMULITE BANK? |
2 |
| FORAMINIFERAL SOLUBILITY RANKINGS: A CONTRIBUTION TO THE SEARCH FOR CONSENSUS |
2 |
| SYMBIONT-BEARING FORAMINIFERA FROM REEFAL AREAS: A CASE STUDY FROM RIO GRANDE DO NORTE (RN, BRAZIL) |
2 |
| MOSCOVIAN-ASSELIAN (MIDDLE PENNSYLVANIAN-EARLIEST CISURALIAN) SMALLER FORAMINIFERS FROM THE ASAD-ABAD SECTION (SANANDAJ-SIRJAN ZONE, CENTRAL IRAN) |
2 |
| NEW FINDINGS ON AN ORBITOLINID FORAMINIFER COSKINOLINELLA BARIENSIS (LUPERTO-SINNI & REINA, 1992) FROM THE ALBIAN SHALLOW-WATER CARBONATE SEQUENCE OF THE BEY DAGLARI (S TURKEY) |
2 |
| ILERDIAN-CUISIAN ALVEOLINIDS FROM THE WESTERN ALBORZ AND EASTERN IRAN ZONES: SYSTEMATIC AND BIOSTRATIGRAPHIC IMPLICATIONS |
1 |
| RECENT ARBORESCENT DENDROPHRYID FORAMINIFERA FOUND ON UPPER PLEISTOCENE COLD-WATER CORALS FROM THE INNER SEA OF THE MALDIVES |
1 |
| CALIBRATION OF TEST DIAMETER AND AREA AS PROXIES FOR BODY SIZE IN THE PLANKTONIC FORAMINIFER GLOBOCONELLA PUNCTICULATA |
1 |
| THE EFFECTS OF SELECTED HEAVY METAL ELEMENTS (ARSENIC, CADMIUM, NICKEL, ZINC) ON EXPERIMENTALLY GROWN FORAMINIFERAL ASSEMBLAGES FROM SAPELO ISLAND, GEORGIA AND LITTLE DUCK KEY, FLORIDA, USA |
1 |
| TWO RARE PUSTULOSE/SPINOSE MORPHOTYPES OF BENTHIC FORAMINIFERA FROM EASTERN ROSS SEA, ANTARCTICA |
1 |
| PRECISION IN BIOSTRATIGRAPHY: EVIDENCE FOR A TEMPORARY FLOW REVERSAL IN THE CENTRAL AMERICAN SEAWAY DURING OR AFTER THE OLIGOCENE-MIOCENE TRANSITION |
1 |
| A SHIP'S BALLASTING HISTORY AS AN INDICATOR OF FORAMINIFERAL INVASION POTENTIAL - AN EXAMPLE FROM PRINCE WILLIAM SOUND, ALASKA, USA |
1 |
| MICRO- AND NANOSTRUCTURES OF CALCAREOUS FORAMINIFERAL TESTS: INSIGHT FROM REPRESENTATIVES OF MILIOLIDA, ROTALIIDA AND LAGENIDA |
1 |
| A STUDY OF CO-OCCURRENCES OF FORAMINIFERA AND MUSSELS IN A POLLUTED NOVA SCOTIAN WETLAND, ATLANTIC CANADA |
0 |
| COLOMINELLA PIRINIAE N. SP.: A NEW TEXTULARIID FROM THE PLIOCENE MEDITERRANEAN RECORD |
0 |
| ORGANIC-WALLED FOSSIL TESTATE AMOEBAE RECORDS (LATE CRETACEOUS-HOLOCENE) FROM THE NEOTETHYAN-MEDITERRANEAN REGION |
0 |
| CYREA SZYMBORSKA GEN. ET SP NOV., A NEW TEXTULARIID FORAMINIFER FROM THE MEDITERRANEAN SEA |
0 |
| BACULOGYPSINA SULAIMANENSIS N. SP. (CALCARINIDAE) FROM THE PRIABONIAN OF SULAIMAN RANGE, PAKISTAN: A POSSIBLE ANCESTOR FOR THE RECENT BACULOGYPSINA SPHAERULATA |
0 |
| DISTRIBUTION OF ENCRUSTING FORAMINIFERA AT SAN SALVADOR, BAHAMAS: A COMPARISON BY REEF TYPES AND ONSHORE-OFFSHORE ZONATION |
0 |
| NEOGENE BENTHIC FORAMINIFERAL BIOFACIES, PALEOBATHYMETRY, AND PALEOENVIRONMENTS OF A GULF OF MEXICO TRANSECT |
0 |
| GLOBOCONELLA PSEUDOSPINOSA, N. SP.: A NEW EARLY PLIOCENE PLANKTONIC FORAMINIFERA FROM THE SOUTHWEST PACIFIC |
0 |
| FORAMINIFERAL BIOCHRONOLOGY OF THE TRIASSIC HOANG MAI FORMATION, CENTRAL VIETNAM |
0 |
| LARGER BENTHIC FORAMINIFERA FROM THE PANNA AND MUKTA FIELDS OFFSHORE INDIA: PALEOBIOGEOGRAPHICAL IMPLICATIONS |
0 |
| MESOCOSM AND MICROCOSM EXPERIMENTS ON THE FEEDING OF TEMPERATE SALT MARSH FORAMINIFERA |
0 |
| TWO NEW SPECIES OF RECENT AND UPPER HOLOCENE COCCOLITH-AGGLUTINATED FORAMINIFERA FROM THE NORTH ICELANDIC SHELF, NORTH ATLANTIC |
0 |
| THE FORAMINIFERA OF CHINCOTEAGUE BAY, ASSATEAGUE ISLAND, AND THE SURROUNDING AREAS: A REGIONAL DISTRIBUTION STUDY |
0 |
| MOLECULAR STUDIES ON FORAMINIFERS: PAST, PRESENT, AND FUTURE |
0 |
| COMPARISON OF DIFFERENT DNA PRESERVATION METHODS ON QUINQUELOCULINA SPP. (FORAMINIFERA, MILIOLIDA) |
0 |
| RECOGNITION OF TRUNCOROTALIA CRASSAFORMIS AS A MODERN PLANKTONIC FORAMINIFERAL MORPHOSPECIES IN THE CARIBBEAN AND EQUATORIAL ATLANTIC OCEAN AND PROPOSAL OF A NEOTYPE |
0 |
| INTERACTIONS OF GLOBOBULIMINA AURICULATA WITH NEMATODES: PREDATOR OR PREY? |
0 |
| TAXONOMIC AND NOMENCLATURAL JUSTIFICATION FOR THE TRIASSIC MEANDROSPIRAL FORAMINIFERAL GENUS CITAELLA PREMOLI SILVA, 1964 |
0 |
| RAPID CHANGE OF FORAMINIFERAL COMMUNITIES AND ASSEMBLAGES IN THE SETIU ESTUARY, TERENGGANU, MALAYSIA: ANTHROPOGENIC DRIVERS |
0 |
| DEFINITION OF FORAMINIFERAL ZONES IN THE FAMENNIAN STAGE (UPPER DEVONIAN) OF TAJIKISTAN |
0 |
| LATE SERPUKHOVIAN FORAMINIFERS NEAR THE MISSISSIPPIAN-PENNSYLVANIAN BOUNDARY AT SOUTH SYNCLINE RIDGE, SOUTHERN NEVADA, USA: IMPLICATIONS FOR CORRELATION |
0 |
