ALBERT

Description: Two late Miocene Tridacna (giant clam) shells from East Kalimantan (Indonesia) were investigated in order to evaluate their potential as subannually resolved paleoenvironmental archives. Via a combination of X-ray diffraction (XRD), laser ablation–inductively coupled plasma–mass spectrometry (LA-ICPMS) trace element analysis, scanning electron microscopy (SEM) and cathodoluminescence (CL) imaging, pristine versus diagenetically altered domains within the shells were identified. LA-ICPMS transects targeting altered aragonite and calcite zones reveal distinct compositional differences in elemental ratios (B/Ca, Mg/Ca, Sr/Ca/ Ba/Ca, Mn/Ca, Al/Ca, La/Ca, Ce/Ca) relative to primary shell aragonite. Pristine shell domains are characterized by an intact banding pattern of alternating dark and light growth bands, with which spatially resolved LA-ICPMS element/Ca and micromilled 18 O records were aligned. Light 18 O values correspond to dark growth bands, indicating growth during warm seasons. The Mg/Ca and/or Sr/Ca ratios covary with oscillating stable oxygen isotope profiles. Progressive increase in Mg/Ca with age demonstrates that besides temperature, growth kinetics exert control over Mg incorporation. If interpreted as temperature controlled only, 18 O from both shells represents average seasonal sea-surface temperature (SST) variability of 2.7 ± 2.1 and 4.6 ± 1.7 °C, respectively. Using published temperature equations and assuming 18 O sw = –0.88, corresponding mean annual paleo–sea-surface temperatures of 27.8 ± 0.2 and 28.5 ± 0.2 °C are estimated. Although the fossil Tridacna shells were noticeably affected by alteration on their external surfaces, their internal aragonitic structure is, to a large extent, well preserved. These corresponding paleoproxy records provide detailed insight into tropical SST variability of the Indo-Pacific region during the late Miocene.

Description: The present-day global maximum for marine biodiversity has been located in Southeast Asia since at least the earliest Miocene. The history of biota in the region has been inferred from the present-day biogeography and phylogeny of extant organisms, but these analyses do not provide adequate tests of the various hypotheses proposed for the origins of the diversity hotspot. The papers in this special issue present the results of an interdisciplinary research project designed to reconstruct the history of shallow marine biota and habitats within the hotspot and help understand the ecological context responsible for the maintenance of the diverse regional biota. A series of remarkably complete and fresh exposures were studied from the Kutai Basin (East Kalimantan, Indonesia) that included thick lower to upper Miocene sections of deltaic and marine sediments including abundant and extremely well preserved fossils. New stratigraphic and environmental frameworks allowed comparison of biota from habitats ranging from shelf-edge reefs to nearshore shallow seagrass meadows and coral carpets. Diversity was overall high throughout the interval, especially when compared to diversity in similar modern turbid mixed carbonate-siliciclastic settings. This points to the previously unrecognized importance of these mesophotic habitats for the development of the diverse reef-associated communities in the modern-day hotspot.

Description: This study is a preliminary assessment of an extremely diverse Tortonian (late Miocene) mollusk assemblage from a coral carpet environment preserved at Bontang (East Kalimantan, Indonesia). Even though coral-associated aragonitic faunas are rarely well preserved, the composition of the assemblage described here can be used to address the following questions: (1) How do the mollusk assemblages in coral habitats differ from other habitats, and (2) What is the effect of sampling on estimates of taxon richness? The mollusk assemblage is dominated by predatory snails and includes typical modern coral-associated taxa such as the gastropod Coralliophila and the bivalve Tridacna . Our investigation implies that adequate documentation of Cenozoic mollusk diversity in the Indo-Pacific is even more challenging than previously expected as very large samples are required to capture species richness. Further assessments of fossil faunas from coral-dominated habitats will be required to provide insight to development of Indo-Pacific biodiversity through time.