REEFCLAM · GSnapshots of tropical Pacific climate variability during the time of Lapita ocean voyaging: giant clam fossils from Fijian shell middens as high resolution archives of climate information.
„Хоризонт 2020“ — Действия „Мария Склодовска-Кюри“
- Период
- 2021-07-01 → 2024-10-29
- Финансиране от ЕС
- 212 934 €
- Участници
- 1
- Схема
- MSCA-IF
Линиите свързват координатора с партньорите.
Накратко на български
Фосили от гигантски миди във Фиджи разкриват температурата и солеността на океана преди 3000 години. Тези данни помагат за подобряване на климатичните модели и разбирането на природната променливост преди индустриализацията.
Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.
Резултати накратко
GSnapshots of tropical Pacific climate variability during the time of Lapita ocean voyaging: giant clam fossils from Fijian shell middens as high resolution archives of climate information.
Understanding how Earth’s climate behaved before industrialisation is essential for predicting future climate change. Instrumental records extend back only ~150 years (a period already influenced by human activity) making them too short to the capture ‘background’ states of natural variability needed to test and improve climate models. These are the same models used to inform climate policy decisions and for guiding adaptation strategies in vulnerable Pacific Island communities. To look further back in time, scientists rely on past climate (paleoclimate) records based on ‘climate proxies’ such as chemical signals preserved in sediments, corals, and shells. The tropical southwest Pacific is especially important, as it hosts two major climate systems: the El Niño–Southern Oscillation (ENSO) and the South Pacific Convergence Zone (SPCZ). These influence weather patterns far beyond the Pacific, yet the region remains underrepresented in high resolution paleoclimate datasets, particularly for the late Holocene (roughly the last 4,000 years). This gap hinders model development and limits understanding of how climate variability may have shaped past societies. The REEFCLAM project aimed to address this by reconstructing seasonally resolved climate records from giant clam (Tridacnidae) shells in Fijian archaeological sites, dated to ~3,000 years before present (BP). Giant clams grow daily and annual layers that record sea surface temperature and salinity via geochemical climate proxies, such as stable oxygen isotopes. Further, giant clams were consumed and left behind in large quantities by the Lapita people, the pioneering voyagers who settled Remote Oceania ~2,500–3,200 years ago. This project used a unique collection of Lapita-aged shells from Fiji, donated/collected by the PI and staff at the Fiji Museum. By analysing physical and chemical patterns in these shells, REEFCLAM sought to address vital gaps in late Holocene paleoclimate records from the tropical SW Pacific as well as investigate the climate conditions that coincided with one of the greatest feats of human migration in history. The project had four main objectives: 1. Analyse modern giant clams from Fiji to determine how their shell chemistry and growth record environmental and climatic change. 2. Apply the same methods to Lapita-aged fossil clams to generate multi-year, seasonally resolved paleoclimate records. 3. Reconstruct sea surface temperature and salinity variability, with a focus on ENSO and SPCZ dynamics. 4. Place these results in context by comparing them with records from other parts of the Holocene and elsewhere in the Pacific and examine the mean climate state during the Lapita settlement period. The project was carried out in close collaboration with the Fiji Museum. Key conclusions All major objectives were achieved. A successful field campaign, carried out in close collaboration with the Fiji Museum, secured both modern and fossil clam specimens. Twelve fossil shells were confirmed as Lapita-aged (~2,700-3,100 BP), providing an invaluable archive of climate information. One was dated as ~5800 BP, providing an important mid-Holocene comparison. Laboratory analyses of growth patterns, isotopes, and trace elements are already producing high-resolution insights into past ocean conditions and are helping to refine how giant clams can be used as climate recorders. Some laboratory measurements are still being processed, with final interpretation expected by 2026. However, the project has already generated new results on mid-to-late Holocene Pacific climate variability, improved understanding of how giant clams archive environmental signals, and established robust methods for identifying well-preserved fossil material. In short, REEFCLAM has filled an important gap in tropical Pacific paleoclimate data, strengthened collaborations with Pacific institutions, and provided new perspectives on both climate dynamics and human history in Oceania.
Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз
Цел на проекта
Records of pre-industrial climate change are vital for accurately simulating Earth’s climate system and reducing uncertainty in 21st century climate predictions. Giant clams are particularly valuable archives of past climate as they are fast-growing, long-lived, and their dense shells have annual growth bands that can be subsampled and analysed to produce sub-annually resolved climate proxy records spanning multiple decades. Furthermore, they are common in the tropical Pacific, where paleoclimate data is particularly valued as sub-annual to decadal-scale changes in this region have been linked to dramatic global temperature and rainfall anomalies with far-reaching socioeconomic and environmental effects. Giant clams are/were a common food and tool supply in the tropical Pacific, and are abundant in Lapita-age shell middens, providing unique opportunities for paleoclimate research that have surprisingly not been exploited.In REEFCLAM, I will use giant clam shells in a ~3,000 year old shell midden to generate the first sub-annually resolved record of pre-industrial climate variability in Fiji. Specifically, trace element and stable isotope profiles across multiple shells will be generated and stitched together, and used to reconstruct patterns of variability in sea surface temperature and salinity. Fiji’s climate is highly sensitive to changes in the SPCZ and WPWP, and so these records will provide a snapshot of Mid-Late Holocene variability relating to the El Niño Southern Oscillation that will be of great value to the climate community. I will generate the first modern clam-based geochemical proxy calibrations for Fiji providing an important platform for future work. Importantly, the data will be also used to test the hypothesis that the pulse of eastward ocean voyaging by the Lapita people and their rapid colonisation of the Pacific coincided with more frequent El Niño events (more westerlies), a novel opportunity to marry the sciences and the humanities.
Оригинален текст от CORDIS (на английски).
Участници
- CARDIFF UNIVERSITY · CARDIFFКоординаторОбединеното кралство
Връзки
Данни: CORDIS, © Европейски съюз
