Comparing radiolarian and diatom diversity and abundance from the northeast Pacific

Particle trap samples (VERTEX) from 4 locations in the northeast Pacific were used to compare centric and pennate diatoms with nassellarian and spumellarian radiolarians. The proportion of pennates and nassellarians were highest at VERTEX 3 from the northeast tropical oceans, off the west coast of Mexico. Colonial radiolarians were characteristic of warm, high saline waters from the southern edge of the north Pacific central gyre, north of Hawaii (VERTEX 4), while pennate diatoms were abundant. The subtropic oceanic Pacific (VERTEX 5A) had more pennate diatoms, while VERTEX (5C), in a coastal cyclonic eddy located west of California, had an even proportion of centric and pennate diatoms. Comparison of major faunas and flora at various oceanic sites of present siliceous sedimentation in conjunction with atmospheric, hydrographic and chemical data, can be helpful in reconstructing paleoceanographic and paleoenvironmental conditions of the past oceans throughout the Phanerozoic.     

First evidence of Late Carnian radiolarians from the Izmir-Ankara suture complex, central Sakarya, Turkey: implications for the opening age of the Izmir-Ankara branch of Neo-Tethys

Within the Late Cretaceous mélange complex of the Izmir-Ankara suture zone in central Sakarya area, north-western Turkey, a megablock with radiolarian cherts associated with basaltic pillow lavas has been dated by radiolarians. The studied radiolarian assemblage and conodonts yielded an early Late Carnian age. This age is the oldest obtained from the chert blocks all along the suture belt and has important implications for the rifting/opening age of the Izmir-Ankara branch of the Tethys ocean in north-western Turkey. Based on this new data, it is concluded that during the Late Triassic the Izmir-Ankara seaway was connected to the other Tethyan oceanic branches and deep enough to provide chert sedimentation and exchange radiolarians with the main open oceans. It is further suggested that the long-lasting misinterpretation of a Liassic rifting/opening of the Izmir-Ankara ocean should be revised.     

Hollow structures in radiolarian skeletons

Spines are the major element of radiolarian skeletons; they are usually solid or, rarely, hollow. Subcylindrical hollow spines and other hollow structures of radiolarian skeletons appeared in the Middle Cambrian. Later, hollow skeletal structures repeatedly developed in the evolution of all radiolarian classes of the subphylum Polycystina throughout the Phanerozoic to the Recent. The analysis of appearance and distribuion in the Phanerozoic of morphotypes with hollow spines has shown that the formation of hollow skeletal structures allowed better adaptation for the planktonic mode of life and could become a key adaptation in struggle for life under stressful conditions.     

Permian and Triassic Radiolaria from Northwest Thailand: paleogeographical implications

Well-preserved radiolarians were recovered from seven sections in the Mae Hong Son-Mae Sariang area, northwestern Thailand. 51 species assigned to 34 genera are identified, including 1 new species (Triassospongosphaera erici Feng sp. nov.) and 19 unidentified species. They are divided into the Late Permian, late Ladinian and middle Carnian radiolarian assemblages. Newly identified radiolarian assemblages, together with the published radiolarian biostratigraphic data from this region, indicate that there was a pelagic basin during the Late Paleozoic and Triassic. This basin was joined to the Chiang Dao and Changning-Menglian oceanic basins, and they represent the main oceanic basin of the Paleotethyan Archipelago Ocean. This main oceanic basin was situated in the traditional “Shan-Thai Block”. Therefore, “the Shan-Thai Block” was not a single block during that stage, but composed of the Paleotethyan Ocean and two continental terranes that were affiliated with the Gondwana and Cathaysian domains, respectively.     

Cenozoic radiolarian paleobiogeography: Implications concerning plate tectonics and climatic cycles

A preliminary study of the paleobiogeographic patterns of radiolarian facies during the Paleogene and subsequent time shows that:(1) Through time radiolarian assemblages display distinct faunal provincialism reminiscent of modern faunal distributions correlated with planetary temperature gradients and surface oceanic conditions. The equatorial—tropical radiolarian fauna extended apparently unrestricted across the Pacific Ocean, the Caribbean Sea and the Atlantic Ocean through Early Miocene time. In the Caribbean Sea and the Atlantic Ocean, radiolarians reached their maximum abundance in the Eocene and Oligocene. Subsequently, they gradually declined to virtual disappearance in these areas in the early Miocene. Their Pacific counterparts remained practically undisturbed, except that post early Miocene assemblages there showed a marked trend toward decreasing test thickness. This trend has since been a worldwide characteristic of Neogene radiolarian assemblages and their modern equivalents. It is postulated that the disappearance of radiolarians in the Carribean Sea and the Atlantic Ocean at the end of the Paleogene is related to the onset of the emergence of the isthmus of Panama which interrupted the preexisting oceanic circulation between the Pacific and Atlantic Oceans.(2) Throughout the Paleogene there have been marked sequential fluctuations in the radiolarian assemblages of the Caribbean Sea which indicate intermittent incursions of higher-latitude fauna in this area. Associated with the faunal fluctuations are cyclic variations in the total carbonate of the sediment with patterns also comparable in duration to Pleistocene carbonate cycles in the equatorial Pacific known to have been induced by climatic changes. Based on similarities with Pleistocene climatic cycles in the equatorial Pacific and elsewhere, it is surmised that the faunal and lithologic fluctuations observed in Paleogene radiolarian sediments were also induced by the biologic and physico-chemical processes associated with worldwide changes in the climatic conditions of that time.     

Lower Darriwilian radiolarians from the Argentine Precordillera

The first radiolarians discovered in the Ordovician of the Argentinian Precordillera are reported. The material is associated with conodonts indicating the upper part of the Lenodus variabilis Biozone (Lower Darriwilian, Da1-2). The low diversity radiolarian fauna shows similarities with Middle Ordovician radiolarians from the Akzhal Mountains of Kazakhstan. However, a close comparison is difficult due to the poor preservation of the material, in which internal structures of the radiolarian tests are not preserved.     

Oceanic oxygenation events in the anoxic Ediacaran ocean

The ocean‐atmosphere system is typically envisioned to have gone through a unidirectional oxygenation with significant oxygen increases in the earliest (ca. 635 Ma), middle (ca. 580 Ma), or late (ca. 560 Ma) Ediacaran Period. However, temporally discontinuous geochemical data and the patchy metazoan fossil record have been inadequate to chart the details of Ediacaran ocean oxygenation, raising fundamental debates about the timing of ocean oxygenation, its purported unidirectional rise, and its causal relationship, if any, with the evolution of early animal life. To better understand the Ediacaran ocean redox evolution, we have conducted a multi‐proxy paleoredox study of a relatively continuous, deep‐water section in South China that was paleogeographically connected with the open ocean. Iron speciation and pyrite morphology indicate locally euxinic (anoxic and sulfidic) environments throughout the Ediacaran in this section. In the same rocks, redox sensitive element enrichments and sulfur isotope data provide evidence for multiple oceanic oxygenation events (OOEs) in a predominantly anoxic global Ediacaran–early Cambrian ocean. This dynamic redox landscape contrasts with a recent view of a redox‐static Ediacaran ocean without significant change in oxygen content. The duration of the Ediacaran OOEs may be comparable to those of the oceanic anoxic events (OAEs) in otherwise well‐oxygenated Phanerozoic oceans. Anoxic events caused mass extinctions followed by fast recovery in biologically diversified Phanerozoic oceans. In contrast, oxygenation events in otherwise ecologically monotonous anoxic Ediacaran–early Cambrian oceans may have stimulated biotic innovations followed by prolonged evolutionary stasis.     

Mesozoic Radiolaria of Bosnia and Serbia: New data

Jurassic and Cretaceous radiolarian faunas were discovered in bedded chert of the Dinaric and Vardar tectonic zones of Bosnia and Herzegovina. Only Triassic radiolarians have previously been described in Bosnia and Herzegovina, while the finds of Bajocian, Bathonian-Callovian, Oxfordian-Kimmeridgian, Tithonian-Berriasian, and Campanian are new. Additional localities of Triassic and Jurassic radiolarians were investigated in Serbia. By correlation with radiolarians from the previous studies within Serbia, the Late Aalenian-Bajocian and Bathonian-Callovian Serbian radiolarian beds are newly dated. The first find of Cretaceous radiolarians in Serbia is reported. The oldest Mesozoic Radiolaria-bearing formations outcropping in the Western Belt of the Vardar Zone are dated Mid-Upper Triassic. The youngest radiolarians come from the Upper Cretaceous (Campanian) of the northern part of this belt of the Vardar Zone, where they co-occur with planktonic foraminifers. The distribution of 70 radiolarian samples within sections is shown. The taxonomic composition of 39 samples is analyzed. Radiolarian species extracted from 13 samples are described and figured. The list of 72 taxa and 3 plates of Jurassic radiolarians of Bosnia and Herzegovina, 3 plates of Triassic, 1 plate of Middle Jurassic, and 1 plate of Upper Cretaceous radiolarians of Serbia are presented.     

Early Cambrian radiolarians and sponge spicules from the Niujiaohe Formation in South China

Most of the reported Cambrian radiolarians are from middle Cambrian (Miaolingian Series, Wuliuan Stage) and onward, the radiolarians from lower Cambrian (Terreneuvian and Cambrian Series 2), on the other hand, are poorly documented, thus their morphological characteristics have not been well understood. In this study, we extracted spherical radiolarians and sponge spicules from the chert of the Cambrian Series 2 Niujiaohe Formation in southern Jiangxi Province, China. The well-preserved radiolarian fossils, identified as Paraantygopora porosa, consist of perforate plate shells pierced by dense pores with elevated rims, and display similarities to those from Lower Ordovician. Seven forms of sponge spicules are recognized, including monaxons, diaxons, tetractines, hexactines, triaxon tetractines, triaxon pentactines and irregular tetraxon tetractines, which are similar to those from the Qiongzhusian Stage in South China. Our results, combined with previously reported early Cambrian radiolarians from South China, indicate that the early Cambrian radiolarians developed advanced spherical skeletons.     

Distribution of living polycystine radiolarians in the Gulf of Mexico and Caribbean Sea,and comparison with the sedimentary record

Plankton tows and bottom samples from the Gulf of Mexico and Caribbean Sea were examined to study the distribution, ecology, and preservation of modern radiolarians. Abundances of radiolarians from this region, an area of low primary productivity, are low. Diversities are variable in the surface waters; diversity indices decrease with increasing water depth, indicating that fewer niches are occupied by radiolarians in deep water. Living radiolarians are confined to specific water masses, some species ranging between two masses, and can be used as indicators of these water masses in ecologic or paleo-oceanographic studies.The record of radiolarian tests present in the sediment is dissimilar to the record of living radiolarians in the water column, but is similar to the record of empty tests falling through the water column. This indicates that a considerable length of time is involved in the settling of radiolarian tests. It also confirms the validity of ecologic interpretations based on a study of sediments only.     

Host-symbiont associations of polycystine Radiolaria: epifluorescence microscopic observation of living Radiolaria

In all 29 polycystine radiolarian species were obtained from surface seawater on May 28, 1999, using a plankton-net at one station (Site 990528; 26°37′18″N, 127°47′35″E) approximately 5 km northwest of Okinawa Island, Japan. In most polycystine radiolarians of the orders Nassellarida and Spumellarida symbiotic algae were observed under light microscopy. The light microscopic (LM) images of the symbionts, however, varied in clarity among individuals because of the variations in microanatomy of the host radiolarian cells. On the other hand, epifluorescence microscopic (EFM) observation easily detected and confirmed the existence of the algal symbionts within the host cytoplasm even in radiolarians such as Dictyocoryne truncatum (Ehrenberg) that include algal symbionts in the depth of the cytoplasm. The chloroplasts of the algal symbionts emitted autofluorescence in ultraviolet irradiation and they appeared red. That is, the autofluorescence images of the chloroplasts can be used to recognize the existence of the algal symbionts within the host radiolarians. Moreover, staining of the symbiont cells with 4′,6-diamido-2-phenylindle permitted visualization of the nucleus in the center of the symbiont cell, confirming the existence of living endosymbiotic algae within the polycystine radiolarians. Both the LM and EFM observations of eight polycystine radiolarian species revealed the specific patterns of various host-symbiont associations. (1) The investigated polycystine radiolarians all possess algal symbionts, except for one species, i.e. Dictyocoryne profunda Ehrenberg. (2) The size of the algal symbionts depends on the radiolarian species. The symbionts are largely classified into two types based on the size of their diameters, i.e. about 8–10 μm for the larger group and about 5 μm for the smaller one. (3) The algal symbionts show a variety of locations within the host radiolarian cytoplasm. The types of distribution of algal symbionts may be a useful characteristic for radiolarian taxonomy.     

南海断面春季放射虫残骸的空间分布及其与表层沉积记录对比

放射虫是揭示古海洋环境信息的重要载体。本文采用虎红染色方法,首次揭示了南海典型断面现代放射虫残骸群的空间分布特征,并比较分析现代水体中放射虫残骸群与海底表层沉积物中放射虫化石群的相互关系。结果表明:南海春季放射虫残骸群比较丰富,其丰度一般呈现出随深度增加而增高的趋势,最高值主要出现在75—300m深即位于叶绿素最大值层和活体高峰深度之下;分析发现研究区放射虫残骸丰度的深度分布受到海流的横向输运影响;春季水体和表层沉积物中放射虫属种组成和丰度分布的差异表明,除了现代放射虫具有季节性变化之外,海流的横向传输也是一个很重要的原因。在150—300m水体中除了Cornutella profunda和Cyrtopera laguncula,还发现了Cycladophora davisiana的残骸,推测典型冷水种C.davisiana由于受到径向翻转流的作用,从中深层水被带到了中上层水体中。     

陕西富平金粟山组放射虫动物群及其时代

安太庠等(1985)把金粟山组分成4段,其中2-4段产有较丰富的牙形类化石Tasmanognathus动物群,当时定其时代为Caradocian期。后来,崔智林等(2000)在该组的第二段硅质岩和灰岩中发现放射虫也认为是Caradocian期的。这次,我们在第4段中找到了一个以Secuicollacta ornata为主的放射虫动物群,Noble和Aitchison(2000)在讨论早古生代放射虫动物群时提出把Secuicollacta的首现作为凯迪期的开始,并把其归属到他们建立的大门孔同心状球形放射虫带1中。因此,金粟山组有可能是凯迪期的。同时,我们对崔智林等(2000)发现的放射虫动物群进一步研究后发现,这个动物群是以Secuicollacta,Kalimnasphaera,Protoceratoikiscum,Palaeoephippium和Haplotaeniatum等属为特征,其时代也是凯迪期的。根据王志浩等(2011)最新研究,金粟山组的2个牙形类化石带,即上部的Tasmanognathus gracilis-T.multidentatus带和下部的T.shichuanhe...     

Paleobiogeographical radiolarian provinces in the Devonian

Geographical distribution of Devonian radiolarians is analyzed and four radiolarian provinces and six subprovinces are recognized for the first time: Euramerican (North American, European, Ural, and Northern subprovinces), Siberian, Paleoasiatic (South China and Japan subprovinces), and Australian. The provinces differ in morphological characters of skeletons, number of genera and species, and frequencies of particular taxa. The term “aboriginal” species is proposed to designate species that constantly dwell in a province or subprovince during certain period.     

Radiolaria associated with large diversity of marine alveolates

We have isolated cells of unculturable radiolarians from marine coastal waters. Individual cells were subjected to single cell whole genome amplification (SCWGA) and gene-targeted PCR. Using this approach we recover a surprisingly large diversity of sequences related to the enigmatic marine alveolate groups 1 and 2 (MALV I and MALV II) that most likely represent intracellular symbionts or parasites of the radiolarian cells. 18S rDNA phylogeny of the MALV sequences reveals 4 distinct clades of radiolarian associates here named Radiolarian Associated Sequences (RAS) 1-4. One clade of both phaeodarian and radiolarian associates and one clade of only phaeodarian associates are also identified. The MALV sequences cluster according to host type, i.e. sequences from associates identified in radiolarians, fish, copepods, ciliates or dinoflagellates are not intermixed but separated into distinct clades. This implies several independent colonizations of host lineages and links a large diversity of MALV to radiolarian-associated species. This demonstrates that radiolarians may be an important reservoir for MALV, making them a key group for understanding the impact of intracellular symbionts on the marine ecosystem. This study shows that applying SCWGA on unculturable cells is a promising approach to study the vast diversity and interactions of intracellular eukaryote organisms.     

江苏仑山地区上奥陶统五峰组放射虫动物群及其地质意义

五峰组以盛产笔石动物群著称,时代为凯迪晚期(相当于英国的阿什极尔期),其中也发现了放射虫.该时期的放射虫在全球并不多见.本文首次描述江苏句容仑山地区五峰组的放射虫动物群,该动物群以不具刺的球形放射虫最为发育,并出现少量Inaniguttidae科的分子,化石保存较差,属种单调,分异度很低,这些特点与大西洋沿岸地区陆表海...     

Upper Devonian Radiolarians from the Zeravshan-Gissar Mountainous Area,Uzbekistan

The first finds of Upper Devonian radiolarians in cherty rocks of the Akbasay Formation, Zeravshan-Gissar mountainous area, are reported. Nineteen species of spherical and spiny forms were identified and assigned to 8 genera. Finds of co-occurring conodonts and radiolarians enabled the refinement of the proposed age of radiolarian associations.     

Deviations in skeletons of radiolarians

Deviations in the skeleton structure of radiolarians are extremely rare in the fossil record. They are known from the Devonian to Recent. This is a very ancient and periodically repeated phenomenon, which should be regarded as a regularity or “lost chance” rather than exotic or accident. Emergence of deviant “mutants” in radiolarians is probably connected with two main causes, i.e., disturbance during reproduction and mutations in particular modules. From the point of view of the morphogenesis of skeletal structures, deviancy facilitates the recognition of relatively “weak” modules–blocks in the general skeleton pattern, which are subject to structural changes. Nonheritable deviant variants have been revealed in skeletons of 61 radiolarian in all of three subphyla of the phylum Radiolaria: Polycystina, Phaeodaria, and Collodaria. Three deviant types are recognized: multiplicative, posterioric and supplemental.