Anatomy of a source rock: environmental, climatic and stratigraphic signatures in the type Kimmeridge Clay

This project, under the aegis of the Rapid Global Geological Events Special Topic, aimed to develop a high-resolution stratigraphy for the Kimmeridgian Stage comparable to that already produced for the Pleistocene. The work involved the examination of three cores drilled at two locations close to the Kimmeridge Clay type section in Dorset: Swanworth Quarry and Metherhills, thereby making best use of the palaeontological, geochemical and sedimentological work already completed from outcrop studies. A programme of comprehensive micropalaeontological, sedimentary, geochemical and mineralogical analysis on the core material was undertaken to characterize the succession at all relevant scales, and to provide a data base for cyclostratigraphic (i.e astronomically based) and isotope-stratigraphic (delta13C(OM)) studies.

The data generated from the core was used to test models of climatic change and climatic forcing of the Mesozoic sedimentary record, and to evaluate the inter-relationships of these phenomena with relative sea-level change. Published data bear on the principal controls of organic-matter accumulation in a major hydrocarbon source-rock.


Programme of Research:

Background to the Proposal

This multi-disciplinary and multi-institutional (Luton, Newcastle, Open, Oxford, Reading and Southampton Universities) project aimed to understand the principal controls on a key episode of petroleum source-rock formation, namely that of the Kimmeridge Clay. This formation has long been recognized as the major source rock for North Sea oil, although at its type locality in Dorset the succession is immature, having suffered only modest burial. The relative lack of post-depositional alteration rendered the sequence particularly suitable for study by a range of analytical techniques. We investigated the stratigraphic, palaeogeographic and palaeoceanographic context of this unit at all possible scales of analysis. As such, the project encompassed stratigraphy, sedimentology, geochemistry and palaeontology. The inter-relationships between the various consortium institutions are shown as a flow diagram in Fig. 1.

The location of three boreholes drilled by the project close to the outcrop near Kimmeridge Bay in Dorset enabled the bio- and lithostratigraphy of the type section, worked out in detail over the last century, to be directly applied to the cored material. The type section is the most stratigraphically complete section through the Kimmeridgian Stage in Europe. There was no need to address the palaeontological aspects of correlation since, by siting the boreholes close to the type locality, we could use the preferable means of an extant and well-established biostratigraphy (Figs 2-3).

A key element of this project was the use of a combination of extant biostratigraphy, lithostratigraphy, newly generated cyclostratigraphy and magnetostratigraphy to place all other data within a secure and well-calibrated chronometric framework. To this end, some geochemical parameters were  determined at a sample interval of 10 cm, which allowed  recognition of the main astronomically controlled climatic variables.

Specific Objectives - All Institutions

The main questions addressed were as follows:

  • How do the principal sedimentary components of the Kimmeridge Clay (clay minerals, CaCO3, and organic matter) vary in quantity and character throughout the succession?
  • What variations in microfabric and palynofacies are found through the Kimmeridge Clay succession, and what is their palaeoceanographic and depositional significance?
  • How can molecular organic geochemistry be applied to obtain palaeoenvironmental information from bitumen and kerogen preserved in the Kimmeridge Clay?
  • Which sedimentary and geochemical parameters within the succession (clay minerals, CaCO3, major and trace elements, TOC, palaeomagnetism, etc.) have responded to Milankovitch forcing, and do different parameters reflect different astronomical periodicities (precession, obliquity, eccentricity)?
  • What is the potential for generating a highly detailed magnetostratigraphy from the type section of the Kimmeridge Clay, and hence for correlation to the Geomagnetic Polarity Time Scale?
  • How does the detailed sedimentary and geochemical record of the type Kimmeridge Clay compare with that in Yorkshire (Institut Français du Pétrole boreholes), the North Sea and northern France?
  • What is the role of relative sea-level change and palaeoclimate in the genesis of Kimmeridge Clay succession?
  • Is elevated plankton productivity or, alternatively, enhanced preservation the main control on organic richness?

Co-ordination Meetings

One-day meetings were held twice per year for all members of the consortium aimed at ensuring efficient collaboration and exchange of ideas.

Method and Approach

In order to tackle these problems we obtained an overview of the total succession by analyzing some quantities at a regular interval of 10 cm (e.g. TOC, CaCO3, major and trace elements). In addition, other studies concentrated on key intervals of particular interest.


At the outset of the project, it was decided that the most appropriate drilling program would be to attempt to obtain two continuous cores through the entire Kimmeridge Clay at a single site as close to the type section of Kimmeridge Bay cliffs as possible. The type section is cut by a number of small faults, both normal and reverse, and to avoid such structural complications it was necessary to locate the drill site on the near-horizontal part of the fold limb of the Purbeck - Isle of Wight monocline (i.e near the eastern end of the outcrop at St Alban's Head). Six sites were suggested and Swanworth Quarry [SY 9675 7823] near Worth Matravers was chosen on the basis of its logistical and environmental advantages. In addition to facilitating core-outcrop correlation at a high degree of resolution, this location also allowed recovery of intervals that are otherwise very poorly exposed (baylei-mutabilis ammonite zones) and/or located in structural settings (e.g. on the footwall of the Purbeck-Isle of Wight disturbance) different from that of the type locality.

The initial borehole drilled in Swanworth Quarry was completed in satisfactory time and yielded good results, which motivated the project to drill a second borehole nearby in the Quarry, together with a third at Metherhills [SY9112 7911], Kimmeridge. Together, these three boreholes recovered the Kimmeridge Clay in its entirety, and their offset double-coring provided an overlapping section between coring breaks which gave ample sample material. A collection of fresh samples from the boreholes was essential for meaningful geochemical work because some intervals exposed along the coast are very badly weathered (e.g. autissiodorensis, elegans and scitulus ammonite zones). Additionally, a full suite of borehole logs was run, including tools such as the formation microscanner and geochemical tool.

Programme of Research - Oxford, Open University (and others)

Plan of Research: Project Co-ordination, Correlation and Regional/Global Setting

Our programme of research was directed principally towards determining the rates of change of stratigraphically significant phenomena such as relative sea-level cycles and the chemistry of sea water. The role of coordinating the analytical efforts of different laboratories to produce an overall synthesis of the component studies was the responsibility of H.C. Jenkyns, S.P. Hesselbo, A.L. Coe, and PDRA H. Morgans-Bell based in Oxford.

Our specific aims can be described as Follows, but more technical details are available in the accompanying proposals from other institutions.

  • To construct a history of regional sea-level and climatic change based on outcrop facies- and sequence-stratigraphic studies in neighbouring regions (e.g. northern France) and using subsurface data (e.g. IFP Yorkim project, Cleveland Basin, Herbin et al., 1994; BP data, North Sea), and to use this as a template to understand large-scale sedimentary cyclicity (>0.5 Ma) within the type Kimmeridgian succession (cf. Coe, 1995; Hesselbo and Jenkyns, 1995, 1998; Gygi et al., 1998). An integrated stratigraphic correlation of the deep-water Dorset section with the coeval mixed offshore and littoral deposits of northern France was undertaken by Oxford-based post-graduate student Carolyn Williams (Williams et al., 2001).
  • To use the array of geochemical parameters determined from core material in order to identify the differing cyclic frequencies in the Milankovitch band (<0.5 Ma) and to produce a cyclostratigraphy for the type Kimmeridge Clay (see Luton proposal).
  • To use this astronomically based stratigraphy to assess the regularity and periodicity of relative sea-level cycles over time periods of millions of years (cf. Weedon and Jenkyns, 1990; see Luton proposal).
  • To assess the rate of change of climatically and oceanographically sensitive parameters such as clay-mineral compositions, C- and Sr-isotope ratios (the latter already determined through previous work in Oxford; Jones et al. 1994; see Newcastle and Reading proposals).
  • To use a carbon-isotope stratigraphy of organic matter (delta 13C(OM)) as a means to correlation with successions classified as Kimmeridgian sensu lato, Tithonian or Volgian in other parts of Europe and elsewhere (cf. Gale et al. 1994; Jenkyns et al. 1994; Jenkyns 1995).  These data are contained in Morgans-Bell et al. 2001).

Role of the PDRA

In addition to co-ordinating the project, the scope of the PDRA's research included: 1) a detailed visual core description of both holes and detailed comparative logging of the type section, extending the work of Cox and Gallois (1981), to produce a full synthesis of previous work and its integration with the new data, and 2) the description, interpretation and correlation of cores and geophysical log data from the North Sea Kimmeridgian made available to us by BP; 3) to understand the regional sedimentological, palaeoceanographic and stratigraphic context of the Kimmeridge Clay. Furthermore, the PDRA and others made a bed-scale, outcrop-based spectral gamma-ray log from the type section (cf. Myers and Wignall, 1987; Parkinson, in press) to aid in cross-correlation to the boreholes and as a basis for investigating the use of gamma-ray logs in sequence stratigraphic analysis (cf. Underhill and Partington, 1993; Tyson, in press; Hesselbo, in press).

Palaeomagnetic studies

Correlation of the Kimmeridgian magnetostratigraphy developed during this project with the Geomagnetic Polarity Time Scale (GPTS) was a desired aim of the project but most of the investigated sediments proved unsuitable for this type of study.


Programme of Research - Reading (and others)

Palaeoclimate Change, Clay Mineralogy and Chemostratigraphic Variation

Palaeoclimate modelling at Reading University, employing UGAMP GCM experiments (Valdes and Sellwood 1992; Sellwood and Price 1993; Valdes 1993; Valdes et al 1995) has thrown light on the way in which orbitally induced variations in solar energy might be translated into a Kimmeridgian climate response. In northwestern Europe the 100 Ka eccentricity signal would have been received in terms of significant temperature variation and minor changes in rainfall. Times of "minimum seasonal forcing" (equivalent to Quaternary ice age times) would have been cooler and slightly wetter whereas times of "maximum seasonal forcing" (equivalent to early Holocene deglaciation) were warmer and drier. This gives a predictable signal which can be sought, through the application of advanced Palaeobiological, mineralogical and geochemical techniques. These results give an ideas-driven basis for evaluating Milankovitch cyclicity, and the recognition of rapid global geological events.

As part of this programme it was our aim to evaluate the climatic changes in the Kimmeridge Clay depositional regime likely to have resulted from Milankovitch forcing. Subtle geochemical and clay mineralogical changes are to be expected. The "normal" pattern of eccentricity-forced changes would be for a progressive and long-term (tens of thousand of years) cooling associated with a slight increase in humidity. This should be reflected in secular changes in the weathering and soil-forming processes in adjacent areas (as recorded in expected clay mineralogical changes).

Work with Valdes (Meteorology Department, Reading University) involved the running of GCM experiments to evaluate the possible impact of precession (19-23 ka) and obliquity cycles (41 ka) on the Kimmeridgian Earth and a refinement of the current model for eccentricity cycles (100 ka).

It was the aim of our analytical programme to provide an overview of the clay mineralogical variation by performing analyses of the < 2 mm fraction every 10 m throughout the core and, by reference to the natural gamma-ray log of the nearby Encombe Borehole (Sellwood et al. 1990) to perform very detailed sampling (15 cm spacing) over a number of intervals. The interval between the Washing Ledge Stone Band and Flats Stone Band in the of the eudoxus Zone  provided a control for much of the Kimmeridge succession, through which the gamma-ray response shows small-scale rhythmicity and the overall gamma activity is moderate. Clay mineralogical analyses was determined through a set of upward-declining gamma-ray cycles in the scitulus Zone and the immediately succeeding wheatleyensis-Zone succession (approaching the Black Stone Band) through which the natural gamma signature becomes very much less regular. These features (together with the high TOC) provided a significant target unit for detailed investigation. In the hudlestoni Zone, because of the complex gamma-ray pattern, it was essential to sample in detail approaching the White Stone Band. Detailed analyses continued up into the lower pectinatus Zone, where gamma-ray intensity declines overall and where patterns become more regular. 

These are all intervals in which pronounced small-scale cyclicity is particularly well developed. The results were integrated with the data generated by the other Groups.

Method and Approach

The clays were separated by standard extraction techniques of disaggregation and sedimentation. In addition, because of the calcareous nature of some of the shale intervals, it was  necessary to obtain a control in the analytical programme by removing the carbonate from duplicate samples (without affecting the clay minerals). Selected samples were analysed using the method developed at PRIS by Cook (1992).

The separated clay fractions were analysed by standard XRD techniques and quantified using the method of Weir et al (1971). In addition, a portion of the separated < 2 mm fraction was sent to the University of Luton (Weedon) so that the rare-earth content of the clays could be analysed. Recent research completed at PRIS by Parker on North Sea Cretaceous clays has shown that the non-exchangeable rare- earth composition of clay minerals can be related to both clay type and provenance. Such an approach allowed subtle changes in mineralogy, as predicted by the palaeoclimate modelling, to be more readily discerned.

A principal, and particularly significant part of this programme was the definition of the major- and minor-element variation through the entire Kimmeridgian succession at 10 cm intervals (5,000 samples). This analysis was undertaken at PRIS using XRF and provided a geochemical base-line against which many of the other geochemical and mineralogical parameters could be evaluated.

XRF provides a means of rapid and accurate characterisation of the sediment. The 5 g samples were powdered by the dedicated technician at Southampton University at 10 cm intervals throughout the core and analysed at PRIS.

Programme of Research - Southampton (and others)

Any study of the cyclicity in a sequence such as the Kimmeridge Clay involves discussion of the mechanism causing the changes in relative abundance of depositional components. Work carried out at Southampton linked the metre-scale cyclicity, as seen in the outcrop and well section, with the individual processes acting during sedimentary deposition. This approach allowed an understanding of how variations in climate can be expressed by changes in mineral and organic sedimentation.

It is now increasingly accepted that many cyclic sedimentary sequences result from orbitally forced changes in sedimentation (see Luton proposal). Much has been made of the overall pattern of cyclicity through such sequences but even less is understood of the parameters which control the pattern of sedimentation in single cycles. A novel approach has been that adopted by Waterhouse (1995) who, from studying Jurassic sediments with cyclicity, showed how the characterization of the types and absolute abundances of the palynological organic matter within individual cycles could be used to understand the relationship between climate change and sedimentation.

A further approach to the study of organic-matter-rich sediments is that of integrated BSEM and palynofacies studies at the lamination scale within Jurassic mudstones. Research at Southampton pioneered the use of back-scattered electron imagery (BSEI) of resin-impregnated sediment and demonstrated that this technique alone gives the necessary resolution and compositional information to analyze unbioturbated pelagic and hemipelagic sediments, particularly where laminations or other fine-scale compositional changes are preserved (Kemp, 1990; Kemp, 1991; Kemp and Baldauf, 1993; Brodie and Kemp, 1994; Kemp et al., 1995; Pearce et al., 1995; Pike and Kemp, 1995, a,b; Bull and Kemp, 1995; Kemp, 1995). The studies cited above demonstrated that BSEI techniques are capable of resolving individual flux events preserved in laminated sediments as thin as 30 mm.

Building on the expertise developed at Southampton, we  used integrated BSEM and palynofacies studies at the lamination scale to characterize and interpret the processes of formation of a small number of Kimmeridge Clay cycles, thus determining the controlling factors on the different depositional environments represented during the deposition of these cycles.

In addition, selected aspects of the cycle-scale palynofacies studies as carried out by Waterhouse were continued in conjunction with the study of organic productivity and preservation by Tyson (Newcastle).

Method and Approach

Lamina-scale analysis

Following drilling, logging and initial core description, four Kimmeridge Clay cycles were selected for multi-disciplinary studies. Representative facies of each of these cycles were sampled and slabbed. For lamina-scale studies the 'part' was polished for BSEM and the 'counterpart' split or cut along individual laminae, using the Westbourne wire saw, and prepared for palynological study. The wire saw removes only 15 mm of rock with each cut and so is capable of sectioning individual laminae.

All palynological samples were Lycopodium-spiked to permit determination of abundances per gram rock and per gram total organic carbon. In addition, preparations were made in which an ultrasonic probe was used to remove the amorphous organic matter that is the dominant kerogen component. This process enables accurate quantification of  particulate organic matter and determination of the environmentally most sensitive kerogen components.

In turn, the polished slab was characterized using the SEM, including element mapping, with the construction of a photomosaic that effectively represents an extraordinarily detailed sedimentary log. This technique allowed lamina-scale sedimentary units to be recognised and depositional processes inferred (e.g. variation in input of the different categories of terrestrial and marine organic matter including calcareous microfossils). Where possible, varve laminae were identified, enabling a direct measure of sedimentation rate and estimates of particle flux. Such varves were subjected to time-series analysis which allowed quantification of sub-millenial time and cycles and provided  an essential higher frequency cycle hierarchy and time base within the decimetric Kimmeridgian cycles. The SEM observations on organic input were substantiated and quantified by lamina-scale palynofacies analysis which allowed determination of abundances of these different categories of terrestrial and marine organic matter.

Individual cycle analysis

In addition to the lamina-scale study, some further work was carried out at a coarser scale on the Kimmeridge Clay cycles in order to develop certain aspects of the work of Waterhouse (1995). The first, in conjunction with the organic geochemical and productivity studies of the Newcastle group, investigated the dinoflagellate cysts both in absolute numbers and species composition. This study  enabled some additional element of productivity within the water column to be determined. A parallel study was carried out on the foraminifera by C.D. Jenkins, who undertook a PhD project on the benthic foraminifera within the Kimmeridge Clay cycles to show how variation in species composition, abundance and diversity of foraminifera within cycles correlates with changing bottom conditions to provide a proxy record of climate change. The additional Kimmeridge Clay core material was particularly important for providing unweathered continuous cored section through individual cycles.

Plan of Research

  • Year 1. Acquisition of samples, preparation of SEM slabs and cutting (using wire saw) of lamination-scale palynofacies samples. BSEI observation, element mapping and photo-mosaic compilation and palynofacies for one selected cycle. Data interpretation and integration with the Newcastle group.
  • Year 2. Sample study from further Kimmeridge Clay cycles. Selected chemical analysis by ICPMS. Comparison of results between contrasting Kimmeridgian cycle types. Investigation of foraminifera and dinoflagellate cysts through cycles at decimetre spacing.
  • Year 3. Data integration with the Newcastle group. Data interpretation leading to a model for deposition of Kimmeridge Clay. Origin of the cyclicity and orbital forcing mechanisms. The responses of different organic particles to climate change in the marine and terrestrial environment.

Programme of Research - Luton (and others)

Spectral Analysis and Milankovitch Control

Work at Luton aimed to investigate the detailed high-resolution stratigraphic time series generated from measurements of percentage total organic carbon (%TOC), %CaCO3, and bulk-rock concentrations of the principal major and trace elements at sample intervals of 10 cm. Additionally, multi-sensor core data collected at 5cm intervals was used for cyclostratigraphic and correlation purposes.

Several earlier studies have implied orbital-climatic (Milankovitch) forcing of sedimentation during the Kimmeridgian (e.g. Dunn, 1974; Oschmann, 1988; Wignall and Hallam, 1991). However, despite recent evidence for metre- and decimetre-scale sedimentary cyclicity, spectral analyses to date have been restricted to just 20 m of the type section (Dunn, 1974; Herbin et al., 1991). The 11,000 point time series generated by the core logging are amenable to spectral analysis in order to test rigorously for the presence of the regular lithological cyclicity which has repeatedly been inferred to relate to orbital-climatic (Milankovitch) forcing. If regular cyclicity, as a function of rock thickness, is detected spectrally, then candidate orbital frequencies need to be unambiguously recognized in order for the "Milankovitch chronometer" to be applied. Successful recognition is most likely to depend upon cycle wavelength ratios as radiometric dating constraints remain too poor for the Late Jurassic. If particular orbital-climatic cycles are identified, evolutionary spectra and band-pass filtering will be used to monitor stratigraphic variations in sedimentation rates at the site of the borehole. Interval dating between approximate time planes (e.g. biostratigraphic datum levels and the coccolithic limestones) can be achieved using counts of regular cycles isolated using filtering (Weedon and Jenkyns, 1990). Where the time planes are recognised elsewhere, especially across the North Sea using geophysical log picks and palynological correlation, the interval dating can be used to determine variations in sedimentation rates across basins.

Method and Approach

It was essential that the true depths of individual sections of the two cores were known precisely and accurately, bearing in mind the possibility of minor faulting and gaps between successive core sections. On the basis of experience on Legs 117 and 154 of the Ocean Drilling Program, the best procedure was to use very closely spaced core-logging methods to generate high-resolution time series. Accordingly, magnetic susceptibility, GRAPE, p-wave velocity and colour reflectance were measured at 5-cm intervals using the Institute of Oceanographical Sciences "Multi-sensor Core Logging System" at Southampton by the consortium's technician. These parameters relate to dilution of paramagnetic clays by carbonate and organic matter; bulk density; sonic velocity and mineralogy respectively. The sample interval was designed to be the most effective given the wavelength of the lithological cyclicity (70-150 cm) at the type section. The resulting four time-series can be then compared between the two holes and used to establish cm-scale lithological correlations, estimate coring gaps and used to design a composite depth scale as the basis for sampling between the two holes (cf. procedures on ODP Leg 154).

Previous field- and laboratory-based work on the Lower Jurassic Belemnite Marls and Blue Lias in southern Britain has established that magnetic susceptibility measurements in the field using the Bartington system provides a rapid lithological logging tool (Weedon et al. 1999). In these rocks, and by analogy in the Kimmeridge Clay, early diagenetic dissolution of ferrimagnetic phases such as magnetite by H2S leaves paramagnetic clays as the predominant susceptibility carriers. Magnetic susceptibility logging thus gives an index of clay content and hence an inverse measure of calcium carbonate. Accordingly magnetic susceptibility logging in the field was used to allow direct lithological correlation with the susceptibility logging of the core material. One advantage of this procedure over natural gamma-ray measurement is that very closely spaced values can be obtained (minimum independent measurement spacing equals 2 cm). These data were used to check that the complete section was drilled and aided direct application of the micro- and macro-fossil biostratigraphy of the type section to the cores.

As described above, Reading investigated clay mineralogy using 250 samples at 10 cm intervals and an additional 50 samples at 10 m intervals throughout the section.  Work by Parker at Reading had found that variation in the concentration of rare-earth elements can reveal clay mineralogy and changes in clay provenance (see Reading section) Thus 300 ICP analyses for REE concentrations was undertaken at Luton on the same samples used for clay-mineral determination. The resulting high-resolution time-series was compared to the clay-mineralogical data in order to reveal Milankovitch-scale variations which could be related to climatic rather than purely diagenetic factors. Time series of all the major analytical data sets were  subjected to spectral analyses. Those parameters which reveal regular cyclicity were compared with the geophysical log and multi-sensor track data using cross-spectral methods. The coherency spectra were used to test which parameters are correlated at which spectral frequencies. Coherent parameters are likely to be related to the same climatic or diagenetic forcing mechanism. For the coherent pairs of parameters, phase spectra can reveal the timing of variations (i.e. which parameter changes before another).

Programme of Research - Newcastle (and others)

Palaeoproductivity and Preservational Controls on the TOC Cyclicity

The decimetre- to metre-scale cyclicity of the onshore Kimmeridge Clay Formation is primarily expressed by the variation in the biogenic component of the sediments, namely organic matter (kerogen) and carbonate (largely coccolithic). The Newcastle effort was directed towards elucidating the key mechanism responsible for the production of the organic-rich´┐Żorganic-poor cycles. Determining a Milankovitch origin did not solve this problem in itself. The questions addressed were: Are the cycles produced by variations in palaeoproductivity, palaeoxygenation, or dilution, or some combination of these, and, if the latter, how do the relative roles of these parameters vary within the formation?

The IFP Yorkim Group and associates recently addressed these issues in some detail, and have generally concluded that palaeoproductivity is the key control. The main arguments they have used to support this view are:

  • (a) That a relatively uniform non-carbonate mineralogical composition through the cycles argues against any significant variation in the terrigenous input (Belin and Brosse, 1992; Bertrand and Lallier-Verges, 1993; Tribovillard et al.,1994).
  • (b) That the predominance of sedimentary lamination through the whole of the cycles (eudoxus Zone, Yorkshire, but not in other cases) argues for continuous "anoxia", and thus no major variation in preservation that might explain the organic carbon (TOC) variation (Bertrand and Lallier-Verges, 1993; cf. Lallier-Verges et al., 1993). See also point (g).
  • (c) That the consistent dominance of marine organic matter argues against any major changes in terrestrial organic matter supply (Bertrand and Lallier-Verges, 1993). The refractory terrestrial component seems to account for a background TOC value of only 1% (Ramanampisoa and Disnar, 1994). The terrestrial structured organic fraction appears to form a relatively constant 15-20% of the kerogen assemblage throughout the studied eudoxus cycles (Belin and Brosse, 1992; Ramanampisoa et al., 1992).
  • (d) That the variations in carbonate content are too small to explain the TOC variation, and that their cycles, when studied on a cm-scale, are also out of phase with each other (Bertrand and Lallier-Verges, 1993; Tribovillard et al., 1994).
  • (e) That whole-rock sulphur contents can be used to calculate an index (the Sulphate Reduction Index, SRI) which records the amount of metabolisable organic matter consumed by sulphate reduction, and thus indirectly the original flux of organic matter, i.e. palaeoproductivity (Bertrand and Lallier-Verges, 1993; Lallier-Verges et al.,1993).
  • (f) That the association between enhanced TOC values and the proportion of a specific type of kerogen ("brown algae" sensu Pradier and Bertrand, 1992; "orange structureless organic matter" sensu Ramanampisoa et al., 1992; "nanoscopically amorphous" organic matter sensu Boussafir et al., 1994) argues for a palaeoproductivity mechanism. See also Tribovillard et al. (1994).
  • (g) That the asymptotic relationship between Hydrogen Index (HI, mg S2 HC/gTOC x 100) and certain biomarker ratios and TOC indicate preservation is no longer important once TOC exceeds 6%, and that any increase in TOC beyond this must be productivity related (Ramanampisoa and Disnar, 1994).

Although apparently compelling, these arguments are not definitive (Tyson, 1996). (a) The relative uniformity of the non-carbonate mineralogy cannot be considered surprising at the decimetre to metre scales in such comparatively distal facies. (b) The presence of lamination does not alone adequately distinguish the significant difference between suboxic and anoxic conditions (Tyson and Pearson, 1991). (c) The relatively constant proportion of the terrestrial component is not what would be expected from palaeoproductivity controlled increased fluxes of marine (AOM) material and a background stable terrestrial supply: a greater marine AOM flux ought to dilute the terrestrial component. The relatively constant terrestrial fraction implies that the variations in TOC are likely to be mostly due to changes in sediment dilution. The actual concentration of terrestrial particles (no./g) increases in the organic-rich part of the cycles (Waterhouse, 1995), which is probably due to lower sediment dilution (Tyson, in press). (e) The SRI index is probably strongly influenced by environment-related variations in "iron limitation" (Tyson, 1995). (f) The amorphous kerogen fraction that is most correlated with the peak TOC values is not the apparently most refractory ultralaminar variety (whose abundance might be expected to best reflect the original flux), but the truly nanoscopically amorphous material, whose distribution would appear to be more preservation controlled. (g) The asymptotic HI value (approx. 600-800) does not occur at a constant TOC, but can range from 6% up to 20% or more (e.g. Huc et al., 1992). Considered in the context of the other available information, such differences are likely mostly due to differences in sediment dilution rather than palaeoproductivity (Tyson, 1996).

Method and Approach

This study adopted several complementary approaches to assess the controls on the TOC cyclicity, which involved the critical testing of several models recently presented in the literature.

  • 1) Modelling of the variations in the percentage organic matter, clay, and carbonate data generated by Southampton, using the empirical approaches of Ricken (1994). Despite the problems of data closure, this approach was used to assess the relative fluxes of the three different components.
  • 2) The main approach used a combination of organic geochemistry and relative and absolute quantitative (non-taxonomic) palynofacies analyses. The absolute palynofacies approach (not utilised by the Yorkim Group) is based on determining particle concentrations as numbers per gram of sediment (using a Lycopodium-spike, following Waterhouse (1995), but with a refined counting procedure). This added a particularly valuable dimension to the study because it allowed one to use the concentration of the terrestrial particles as a proxy for terrigenous dilution. The concentration of terrestrial particles is generally correlated with terrestrial sediment supply (cf. Tyson, 1995) but in distal facies, where it reflects a refractory background, it primarily records sediment dilution. This view is supported by the fact that the concentrations increase in the most organic-rich strata (where marine organic matter is most abundant), and are associated with phytoclast and palynomorph assemblages that are clearly the most "distal" in aspect (Waterhouse 1995, Tyson, 1996).
  • 3) Based on their modern lake work, Hollander et al. (1992, 1993) suggested that there is a negative correlation between delta13C and Hydrogen Index when productivity is the dominant control, and a positive correlation when "stagnation" and enhanced preservation is the dominant control. Some supporting evidence for application of this approach to the Kimmeridge Clay has been very briefly presented (Hollander et al., 1993), but more rigorous studies are required, which include (as here) correction for variations in kerogen type, better stratigraphic context, and calibration against other methods.

Application of the approach

The first approach used 'whole sequence' data generated at Southampton, and also supplementary higher resolution TOC and carbonate data generated at Newcastle. Because of its time-intensive nature, the second approach has only been carried out on cycles from the four key intervals within the formation that have been selected because of their sequence stratigraphic or other significance (cf. Tyson, 1996). The last approach analysed particular cycles in detail. In order to enhance the interpretation, toward the end of the project the results of the above approaches were integrated with information from the palaeoclimatic modelling (Reading) in order to gain a better understanding of the hydrographic behaviour of the Late Jurassic shelf seas, and to evaluate the "seasonal anoxia" models of Oschmann (1988) and Tyson and Pearson (1991).

References (and additional publications)

  • Belin, S. and Brosse, E. 1992. Petrographical and geochemical study of a Kimmeridgian organic sequence. Revue de l'Institut Francais du Petrole, 47, 711-725.
  • Bellamy, J. 1979. Carbonates within Bituminous Shales in the British Jurassic - their Petrography and Diagenesis. Unpublished Ph.D thesis, University of Southampton, 276pp.
  • Bertrand, P. and Lallier-Verges, E. 1993. Past sedimentary organic matter accumulation and degradation controlled by productivity. Nature, 364, 786-788.
  • Boussafir, M., Lallier-Verges, E., Bertrand, P. and Badaut-Trauth, D. 1994. Structure ultrafine de la matiere organique des roches meres du Kimmeridgien du Yorkshire (UK). Bulletin de la Societe Geologique de France, 165, 353-361.
  • Brodie, I and Kemp, A.E.S. 1994. Variation in biogenic and detrital fluxes and formation of laminae in late Quaternary sediments from the Peru coastal upwelling zone. Marine Geology, 116, 385-398.
  • Brodie, I and Kemp, A.E.S. 1995. Pelletal structures in Peru upwelling sediments. Journal of the Geological Society, London, 152, 141-150.
  • Bull, D. and Kemp, A.E.S. 1995. Composition and origins of laminae in Late Quaternary and Holocene sediments from the Santa Barbara Basin. In: Proceeding of the Ocean Drilling Program, Scientific Results, 146, College Station, TX. (Ocean Drilling Program), 77-87.
  • Coe, A.L. (1995). A comparison of the Oxfordian successions of Dorset, Oxfordshire and Yorkshire. In: Taylor, P.D. (Ed.). Field Geology of the British Jurassic. Geological Society, London, 151-172.
  • Coe, A.L. 1996. Unconformities within the Portlandian Stage of the Wessex Basin and their sequence stratigraphical significance. In: Hesselbo, S.P. and Parkinson, D.N. (eds). Sequence stratigraphy and its application to British geology. Special Publication of the Geological Society, London, 103, 109-143.
  • Cook, R.J. 1992. A comparison of methods for the extraction of smectites from calcareous rocks by acid dissolution techniques. Clay Mineralogy, 27, 73-80.
  • Cox, B.M. and Gallois, R.W. 1981. The stratigraphy of the Kimmeridge Clay of the Dorset type area and its correlation with some other Kimmeridge sequences. Report of the Intitute of Geological Sciences, 80/4, 1-44.
  • Dunn, C.E. 1974. Identification of sedimentary cycles through Fourier analysis of geochemical data. Chemical Geology, 13, 217-232.
  • Farrimond, P., Comet, P., Eglington, G., Evershed, R.P., Hall, M.A., Park, D.W., and Wardropper, A.M.K. 1984. Organic geochemical study of the Upper Kimmeridge Clay of the Dorset type area. Marine and Petroleum Geology, 1, 340-354.
  • Gale, A.S., Jenkyns, H.C., Kennedy, W.J. and Corfield, R.M. 1993. Chemostratigraphy versus biostratigraphy: data from around the Cenomanian-Turonian boundary. Journal of the Geological Society, London, 150, 29-32.
  • Gallois, R.W. and Medd, A.W. 1979. Coccolith-rich marker bands in the English Kimmeridge Clay. Geological Magazine, 116, 247-334.
  • Gradstein, F.M., Agterberg, F.P., Ogg, J.G., Hardenbol, J. van Veen, P. Thierry, J. and Huang, Z. 1994. A Mesozoic time scale. Journal of Geophysical Research, 99, 24051-74
  • Gygi, R.A., Coe, A.L. and Vail, P.R. 1998. Sequence stratigraphy of the Oxfordian and Kimmeridgian in northern Switzerland. In: de Graciansky, P.C. and Hardenbol, J. (eds). Mesozoic and Cenozoic sequence stratigraphy of European basins. Special Publication of the Society of Economic Paleontologists and Mineralogists, 60, 528-544.
  • Herbin, J.P., Müller, J.G., Geyssant, J.R., Mélieres, F. & Penn, I.E. 1991. Hétérogénéite quantitative de la matiére organique dans les argiles du Kimméridgien du Val de Pickering (Yorkshire, UK), cadre sédimentologique et stratigraphique. Revue de l'Institut Français du Pétrole, 46, 675-712.
  • Herbin, J.P., Fernandez-Martinez, J. L., Geyssant, J.R, Albani, A.El., Deconinick, J.F.,Proust, J.N., Colbeaux, J.P. and Vidier, J.P. 1995. Sequence stratigraphy of source rocks applied to the study of the Kimmeridgian/Tithonian in the northwest European shelf (Dorset/UK, Yorkshire/UK and Boulonnais/France). Marine and Petroleum Geology 12, 177-194.
  • Hesselbo, S.P. 1996. Spectral gamma-ray logs in relation to clay mineralogy and sequence stratigraphy, ODP Leg 150, Cenozoic of the Atlantic Margin, offshore New Jersey. In: Mountain, G.S., Miller, K.G., Blum, P., and Twitchell, D. (eds) Proceedings of the Ocean Drilling Program, Scientific Results, 150, New Jersey continental slope and rise, 411-422.
  • Hesselbo, S.P. and Jenkyns, H.C. 1995. A comparison of the Hettangian to Bajocian successions of Dorset and Yorkshire. In:Taylor, P.D. (ed.) Field Geology of the British Jurassic. Geological Society of London. p.105-150.
  • Hesselbo, S.P. and Jenkyns, H.C. 1998. Sequence stratigraphy of the British Lower Jurassic. In: de Graciansky, P.C., Hardenbol, J., Jacquin, T., Farley, and Vail, P.R. (eds). Mesozoic and Cenozoic Sequence Stratigraphy of Western European Basins. Mesozoic and Cenozoic sequence stratigraphy of European basins. Special Publication of the Society of Economic Paleontologists and Mineralogists, 60, 561-581.
  • Hollander, D.J., McKenzie, J.A., Hsu, K.J., and Huc, A.Y. 1993. Application of a eutrophic lake model to the origin of ancient organic-carbon-rich sediments. Global Biogeochemical Cycles, 7, 157-179.
  • Hollander, D.J., McKenzie, J.A., and Ten Haven, H.L. 1992. A 200 year sedimentary record of progressive eutrophication in Lake Greifen (Switzerland): implications for the origin of organic-carbon-rich sediments. Geology, 20, 825-828.
  • Huc, A.Y., Lallier-Verges, E., Bertrand, P., Carpentier, B., and Hollander, D.J. 1992. Organic matter response to change of depositional environment in Kimmeridgian shales, Dorset, U.K. In: Whelan, J.K. and Farrrington, J.W. (eds). Productivity, Accumulation, and Preservation of Organic Matter in Recent and Ancient Sediments. Columbia University Press, New York, 469-486.
  • Jenkyns, H.C. (1995). Carbon-isotope stratigraphy and palaeoceanographic significance of the Lower Cretaceous shallow-water carbonates of Resolution Guyot, Mid-Pacific Mountains. In: Winterer, E.L., Sager, W.W., Firth, J.V. and Sinton, J.M. (eds). 1995 Proceedings of the Ocean Drilling programme, Scientific Results, 143: College Station, TX .
  • Jenkyns H.C., Gale, A.S. and Corfield, R.M. 1994. Carbon- and oxygen-isotope stratigraphy of the English Chalk and Italian Scaglia and its palaeoclimatic significance. Geological Magazine, 131, 1-34.
  • Jones, C.E., Jenkyns, H.C., Coe, A.L. and Hesselbo, S.P. (1994). Strontium isotopic variations in Jurassic and Cretaceous seawater. Geochimica Cosmochimica Acta, 58, 3061-3074.
  • Kemp, A.E.S. 1991. Silurian pelagic and hemipelagic sedimentation and palaeoceanography. In: Bassett M. G., Lane P. D. and Edwards D. (eds). Special Paper in Palaeontology, 44, 261-300.
  • Kemp, A.E.S. 1995. Laminated sediments from coastal and open ocean upwelling systems: what variability do they record? In: Summerhayes C., Emeis K.-C., Angel M.V., Smith R.L. and Zeitzschel B. (eds), Upwelling in the Ocean: modern processes and ancient records, Dahlem Workshop Report, John Wiley and Sons, Chichester, 239-257. 
  • Kemp, A.E.S. and Baldauf, J.G., 1993. Vast Neogene laminated diatom mat deposits from the eastern equatorial Pacific Ocean. Nature, 362: 141-144.
  • Kemp, A.E.S., Baldauf, J.G. and Pearce, R.B. 1995. Origins and paleoceanographic significance of laminated diatom ooze from the eastern equatorial Pacific Ocean (ODP Leg 138). In: Proceeding of the Ocean Drilling Program, Scientific Results, 138. College Station, TX. (Ocean Drilling Program), 641-645.
  • Lallier-Verges, E., Bertrand, P., Huc, A.Y., Bueckel, D., and Tremblay, P. 1993. Control of the preservation of organic matter by productivity and sulphate reduction in Kimmeridgian shales from Dorset. Marine and Petroleum Geology, 19, 600-605.
  • Lees, J.A., Bown, P.R., Young, J.R. and Riding, J.B. (2004) Evidence for annual records of phytoplankton productivity in the Kimmeridge Clay Formation coccolith stone bands (Upper Jurassic, Dorset, UK) Marine Micropaleontology, 52, 29-49.
  • Matthews, A., Morgans-Bell, H.S., Emmanuel, S., Jenkyns, H.C., Erel, Y. and Halicz, L., 2004.  Controls on iron-isotope fractionation in organic-rich sediments (Kimmeridge Clay, Upper Jurassic, southern England).  Geochim. Cosmochim. Acta, 68, 3107-3123.
  • Morgans-Bell, H.S., Coe, A.L., Hesselbo, S.P., Jenkyns, H.C., Weedon, G.P., Marshall, J.E.A., Tyson, R.V. and Williams, C.J., 2001. Integrated stratigraphy of the Kimmeridge Clay Formation (Upper Jurassic) based on exposures and boreholes in south Dorset, UK. Geological Magazine, 138, 511-539.
  • Myers, K.J. and Wignall, P.B., 1987. Understanding Jurassic organic-rich mudrocks - new concepts using gamma-ray spectrometry and palaeoecology: examples from the Kimmeridge Clay of Dorset and the Jet Rock of Yorkshire. In Leggett, J.K., and Zuffa, G.G. (eds), Marine Clastic Sedimentology : Concepts and case Studies.: London (Graham and Trotman), 172-189.
  • Oschmann, C.E. 1988. Kimmeridge Clay sedimentation - a new cyclic model. Palaeogeography, Palaeoclimatology, Palaeoecology, 65, 217-251.
  • Pancost, R.D., van Dongen, B.E., Esser, A., Morgans-Bell, H., Jenkyns, H.C. and Sinninghe Damsté, J.S., 2005. Variation in Organic Matter Composition and Its Impact on Organic-Carbon Preservation in the Kimmeridge Clay Formation (Upper Jurassic, Dorset, southern England). In: N.B. Harris , Editor, The deposition of organic-carbon-rich Sediments: Models, Mechanisms, and Consequences, Spec. Publ. Society for  Sedimentary Geology (SEPM), 82, 261-278
  • Parkinson, D.N., 1996. Gamma-ray spectrometry as a tool for stratigraphic interpretation: examples from the western European Lower Jurassic. In Hesselbo, S.P., and Parkinson D.N. (eds), Sequence Stratigraphy: Concepts and Application to British Geology. Special Publication of the Geological Society, London, 103, 231-255.
  • Pearce, R.B., Kemp, A.E.S., Baldauf, J.G. and King, S.C. 1995. High resolution sedimentology and micropaleontology of laminated diatomaceous sediment from the eastern equatorial Pacific Ocean (ODP Leg 138). In: Proceedings of the Ocean Drilling Program, Scientific Results, 138. College Station, TX. (Ocean Drilling Program), 647-663.
  • Pearson, S.J., Marshall, J.E.A. and Kemp, A.E.S. 2004. The Whitestone Band of the Kimmeridge Clay: an integrated high-resolution approach to understanding environmental change. Journal of the Geological Society, London, 161, 675-683.
  • Pike, J. and Kemp, A.E.S. 1995a. Silt aggregates in laminated marine sediments produced by agglutinating foramininfera. Journal of Sedimentary Research A, 66, 625-631.
  • Pike, J. and Kemp, A.E.S. 1995b. Peparation and analysis techniques for studies of laminated sediments. In Kemp A.E.S. (ed), Palaeoclimatology and palaeoceanography from laminated sediments. Special Publication of the Geological Society, London, 116, 37-48.
  • Pradier, B. and Bertrand, P. 1992. Etude a resolution d'un cycle du carbon organique de roche-mere du Kimmeridgien du Yorkshire (G.B.): relation entre composition petrographique du contenu organique observe in situ teneur en carbone organique et qualite petroligene. Compte Rendus Academie des Sciences Paris, series II, 315, 187-192.
  • Ramanampisoa, L. and Disnar, J.-R. 1994. Primary control of paleoproduction on organic matter preservation and accumulation in the Kimmeridge rocks of Yorkshire (UK). Organic Geochemistry, 21, 1153-1167.
  • Ramanampisoa, L., Bertrand, P., Disnar, J.-R., Lallier-Verges, E., Pradier, B., and Tribovillard, N.-P. 1992. Etude a haute resolution d'un cycle de carbone organique des argiles du Kimmeridgien du Yorkshire (Grande-Bretagne): resultats preliminaires de geochemie et de petrographie organique. Comptes Rendus Academie des Sciences Paris, series II, 314, 1493-1498.
  • Ricken, W. 1993. Sedimentation as a Three-Component System: Organic Carbon, Carbonate, Noncarbonate. Lecture Notes in Earth Sciences, 51. 211pp.
  • Sellwood, B.W. and Price G.D. 1993. Sedimentary facies as indicators of Mesozoic palaeoclimate. Philosophical Transactions of the Royal Society, London, B341, 225-233.
  • Sellwood, B.W., Wilson, R.C.L. and West, I.M. 1990. Jurassic sedimentary environments of the Wessex Basin, Field Trip A16, 13th Internat. Sedimentol. Congr. Nottingham, 87pp.
  • Tribovillard, N.-P., Desprairies, A., Lallier-Verges, E., Bertrand, P., Moureau, N., Ramdani, A., and Ramanipisoa, L. 1994. Geochemical study of organic-matter rich cycles from the Kimmeridge Clay Formation of Yorkshire (UK): productivity versus anoxia. Palaeogeography, Palaeoclimatology, Palaeoecology, 108, 165-181.
  • Tyson, R.V. 1985. Palynofacies and Sedimentology of Some Late Jurassic Sediments From the British Isles and Northern North Sea. Unpublished Ph.D thesis, The Open University, Milton Keynes, 623pp.
  • Tyson, R.V. 1989. Late Jurassic palynofacies trends, Piper and Kimmeridge Clay Formations, UK onshore and offshore. In: Batten, D.J. and Keen, M.C. (eds). Northwest European Micropalaeontology and Palynology. British Micropalaeontological Society Series, Ellis Horwood, Chichester, 135-172.
  • Tyson, R.V. 1995. Sedimentary Organic Matter: Organic Facies and Palynofacies. Chapman and Hall, London. 615pp.
  • Tyson, R.V. 1996. Sequence stratigraphical interpretation of organic facies variations in marine siliciclastic systems: general principles and application to the onshore Kimmeridge Clay Formation, UK. In: Hesselbo, S.P. and Parkinson, D.N. (eds.). Sequence stratigraphy and its application to British geology. Special Publication of the Geological Society, London, 103, 75-96.
  • Tyson, R.V. 2004. Variation of marine total organic carbon through the type Kimmeridge Clay Formation (Late Jurassic), Dorset, UK. Journal of the Geological Society, London, 161, 667-673.
  • Tyson, R.V. and Pearson, T.H. 1991. Modern and ancient continental shelf anoxia: an overview. In: TYSON, R.V. and PEARSON, T.H. (eds) Modern and Ancient Continental Shelf Anoxia, Geological Society of London Special Publication, 58, 1-24.
  • Underhill, J.R. and Partington, M.A. 1993. Jurassic thermal doming and deflation in the North Sea: implications of the sequence stratigraphic evidence. In: Parker, J.R. (ed.) Petroleum geology of North West Europe: Proceedings of the 4th Conference. The Geological Society, London, 337-345.
  • Valdes, P.J. 1993. Atmospheric circulation models of the Jurassic. Philosophical Transactions of the Royal Society, London, B341, 317-326.
  • Valdes, P.J. and Sellwood, B.W. 1992. A palaeoclimate model for the Kimmeridgian. Palaeogeography, Palaeoclimatology, Palaeoecology, 95, 47-72.
  • Valdes, P.J., Sellwood, B.W. and Price, G.D. 1995. Modelling Late Jurassic Milankovitch climate variations. In House, M.R. and Gale, A.S. (eds). Orbital forcing, timescales and cyclostratigraphy. Special Publication of the Geological Society, London, 85, 115-132.
  • van Dongen, B.E., Schouten, S. and Sinninghe Damsté, J.S. 2006. Preservation of carbohydrates through sulfurization in a Jurassic euxinic shelf sea: Examination of the Blackstone Band TOC cycle in the Kimmeridge Clay Formation, UK. Organic Geochemistry, 37, 1052-1073.
  • Waterhouse, H.K. 1995. High-resolution palynofacies investigation of Kimmeridgian sedimentary cycles. In: House, M.R. and Gale, A.S. (eds) Orbital forcing timescales and cyclostratigraphy. Special publication of the Geological Society, London, 85, 75-114.
  • Weedon, G.P. 1993. The recognition and stratigraphic implications of orbital-forcing of climate and sedimentary cycles. In: Wright, V.P. (ed.) Sedimentology Review. Blackwell, p.31-50.
  • Weedon, G.P. and Jenkyns, H.C. (1990). Regular and irregular climatic cycles and the Belemnite Marls (Pliensbachian, Lower Jurassic, Wessex Basin). Journal of the Geological Society, London, 147, 915-918.
  • Weedon, G.P and Shimmield, G.B. 1991. Late Pleistocene upwelling and productivity variations in the northwest Indian Ocean, deduced from spectral analyses of geochemical data from Sites 722 and 724. In: Prell, W.L., Niitsuma, N. et al.Proceedings of the Ocean Drillling Program, Scientific Results, 117, 431-443.
  • Weedon, G.P., Jenkyns, H.C., Coe, A.L. and Hesselbo, S.P. 1999. Astronomical calibration of the Jurassic time-scale from cyclostratigraphy in British mudrock formations. Phil. Trans R. Soc Lond., Ser. A., 357, 1787-1813.
  • Weedon, G.P., Coe, A.L., Ogg, J.G. and Gallois, R.W. 2004. Cyclostratigraphy, orbital tuning and inferred productivity for the type Kimmeridge Clay (Late Jurassic), southern England. Journal of the Geological Society, London, 161, 655-666.
  • Wignall, P.B. and Hallam, A. 1991. Biofacies, stratigraphic distribution and depositional models of British onshore Jurassic black shales. In: Tyson, R.V. and Pearson, T.H. (eds) Modern and ancient continental shelf anoxia. Special Publication of the Geological Society, London, 58, 291-310.S
  • Weir, A.H. , Ormerod, E.C. and El Mansey, I.M.I. 1971. Clay mineralogy of sediments of the Western Nile Delta. Clay Mineralogy 10, 369-386.
  • Williams, C.J., Hesselbo, S.P., Jenkyns, H.C. and Morgans-Bell, H.S. 2001. Quartz silt as a key to sequence stratigraphy (Kimmeridge Clay Formation, Late Jurassic, Wessex Basin, UK). Terra Nova, 13, 449-455.